.^3 LIBRARY NEW YORK BOTAMCAL TRANSACTIONS "*"" OF THE ACADEMY OF SCIENCE OF ST. LOUIS. VOL. XIII. JANUARY 1903 TO DECEMBER 1903. PUBLISHED UNDER DIRECTION OF THE COUNCIL. ST. LOUIS: NIXON JONES PRINTING CO. /95 ■A ^1 CONTENTS. PAGE. Table of Contents iii List of Members. Revised to December 31, 1903 v 1. Patrons. 2. Active Members. Constitution xiii By-Laws xvii Abstract op History xxii Record. January 1 to December 31, 1903 , xxvL Papers Published. January 1 to December 31, 1903: 1. G. Hambach. — Revision of the Blastoideae, with a pro- posed new classification, and description of new species. — Plates I. -VI. — Issued November 4, 1903.. 1 2. Francis E. Nipher. — On the predetermination of the speed of the trotting horse. — Issued July 9, 1903 69 3. Julius Hurter. — Second contribution to the herpetol- ogy of Missouri. — Issued July 31, 1903 77 4. Walter L. Sheldon. — A bird's-eye view of the litera- ture of ethical science since the time of Charles Dar- win.— Issued August 21, 1903 87 5. Francis E. Nipher. — The law of contraction of gaseous nebulae. — Issued October 1, 1903 143 6. Edward H. Keiser and S. W. Forder. — A new method for the determination of free lime, and on so-called dead burnt lime. — Issued December 4, 1903 165 7. B. F. Bush. — A new genus of grasses. — Plates VII.- VIII.— Issued December 11, 1903 175 8. J. Arthur Harris. — Polygamy and certain floral ab- normalities in Solanum. — The germination of Pachira, with a note on the names of tv70 species. — Plates IX.-XI. — Issued December 12, 1903 185 9. Title-page, prefatory matter and index of Vol. XIII. — Record, January 1 to December 31, 1903. — Issued February 9, 1904. List of Authors 211 General Index 212 Index to Genera 214 CORRECTIONS.* P. 7, line 5. — For lumen is, read lamina are. P. 9, line 18. — For oval, read oral. P. 12, line 32. —For Fig. 5, read Figs. 8, 10 and 11. P. 14, line 20. — For Plate II. fig. 2, 3, 5, read Plate II. fig. 3. P. 34, line 28. — For Maccoy, read M'Coy. p. 47, line 22. — For Codastus, read Codaster. footnote. — For ralated, read related. P. 49, line 10. — For impossible, read impossible. P. 51, lines 13, 15. — For Canedayi, read Cassedayi. P. 53, line 22. — For ambulacria, read ambulacra. P. 55, line 18. — For plicable, read plicated. line 35. — For prominent, read promising. P. 59, line 18. — Omit comma. Explanation of Plate II. No. 5. — Add, enlarged four times. No. 11. — Add, in a Codaster. Explanation of Plate IV. No. 6. — For pyramidalis, read bipyra- midalis. P. 69, line 18. — The equation should read S= a-}- 6e-^'* P. 72, line 5. — For 13.5, read 19.95. P. 147, equation (12). — For (2 — n), read (2 — n)^- P. 155, line 3. —For 2C, read 2Cp. last line. — For aT, read clT. P. 156, equation (17)'. — For ilf — , read iiyr=. P. 157. — For W= 4 tt f E^ Pd R, read W= Air C R^PdR. ^ ^ R P. 160, equation (41) and preceding equation. — For Cp , read Cp. (8— 5n) (4 — 3n) G P. 163, equation (50). - Read, S = ^^g^^^^^W^^ J ' Q following equation. — Read = 0.177 y • P. 181, line 21. — For Hall, read Hale. * Some of these changes require to be made in only the latter part of the edition, from which type appears to have fallen. MEMBERS. 1. PATRONS. Eliot, Henry W 2635 Locust st. Harrison, Edwin 3747 Westminster pi. McMillan, Mrs. Eliza 25 Portland pi. McMillan, William Northrop 25 Portland pi. 2. ACTIVE MEMBERS. Adkins, James Park and Vandeventer avs. Alleman, Gellert* Swarthmore College, Swarthmore, Pa. Allen, Terry W 5061 Lindell av. Alt, Adolf 3036 Locust st. Andrews, William Edward* Taylorville, 111. Bain, Robert Elward Mather 900 Locust st. Bailey, Liberty Hyde* ...Ithaca, N. Y. Baker, Carl Fuller* Pomona College, Claremont, Calif. Barck, Carl 2715 Locust st. Bartlett, George M 215 Pine st. Baumgarten, Gustav 4900 Berlin av. Bean, Tarleton Hoffman* Administration bldg,, World's Fair. Becktold, William B 212 Pine st. Bernays, A. C 3623 Laclede av. Bixby, William Keeney 13 Portland pi. Boeckeler, William L 4441 Laclede av. Bolton, Benjamin Meade 4160 McPherson av. Brannon, Melvin A.* University, N. Dak. Brennan, Martin S 1414 O'Fallon st. Brimmer, George G 6900 Michigan av. Brookings, Robert S 5125 Lindell av. Brown, Daniel S 2212 DeKalb st. Brown, Willi 3526 Pine st. Budgett, Sidney Payne 1806 Locust st. Burg, William 1756 Missouri av. * Non-resident. vi Trans. Acad. Set. of St. Louis. Burnett, E. C University Club. Busch, Adolphus 1 Busch pi. Busch, Aug. A Busch pi. Bush, Benjamin Franklin* Courtney, Mo. Calvert, Sidney* State University, Columbia, Mo. Carpenter, George O Russell and Compton avs. Carter, Howard* Webster Groves, Mo. Carver, George Washington* Tuskegee, Ala. Chaplin, WinfieldS 3636 West Pine boul. Chappell, W. G 3810 Westminster pi. Chase, E. C Oriel bldg. Chauvenet, Louis 5501 Chamberlain av. Chouteau, Pierre 912 Security bldg. Chouteau, Mrs. Pierre 912 Security bldg. Compton, P. C 4156 Washington boul. Comstock, T. Griswold 3401 Washington av. Conklin, Harry R.* Joplin, Mo. Cramer, Gustav V,, G. Cramer Dry Plate Co. Crandall, George C .....4287 Olive st. Crunden, Frederick Morgan Public Library. Curtis, William S St. Louis Law School. Cushman, AllertonS.* Bryn Mawr, Pa. Dame, James E 2353 Albion pi. Dameron, Edward Caswell.* Ciarksville, Mo. Davis, N. H 56 Vandeventer pi. Davis, John D 421 Olive st. De Menil, Alexander N De Menil bldg., 7th and Pine sts. Diehm, Ferdinand 1834 Kennett pi. Dodd, Samuel M 415 Locust st. Douglas, Archer W % Simmons Hardware Co. Drake, George S 64 Vandeventer pi. Drosten, F. W 2011 Park av. Duenckel, Frederick William 2912 EUendale av. Duggar, B. M.* 202 Hitt st., Columbia, Mo. Eggert, Henry* 1001 CoUinsville av., E. St. Louis, 111. Eimbeck, August F.* New Haven, Mo. Eliot, Edward C 5468 Maple av. Engler, Edmund Arthur* 11 Boynton st., Worcester, Mass. Erker, AdolphP 608 Olive st. Members. vii Espenschied, Charles 3500 Washington av. Euston, Alexander 3730 Lindell boul. Evers, Edward 1861 N. Market st. Ewing, Arthur E 6024 West Cabanne pi. Eycleshymer, A. E 3650 Washington av. Favor, Ernest Howard* Box 842, Columbia, Mo. Fernald, Robert Hey wood Washington University. Fischel, Washington E 3841 Washington av. Forbes, Stephen A.* Urbana. 111. Fordyce, John R.* 2223 Louisiana st.. Little Rock, Ark. Forster, Marquard 2317 S. 13th st. Francis, David R 4421 Maryland av. French, George Hazen* ...Carbondaie, 111. Frerichs, Frederick W 4608 S. Broadway. Frick, John Henry* Warrenton, Mo. Fruth, Otto J 3066 Hawthorne boul. Fry, Frank R 3133 Finest. Funkhouser, Robert Monroe 3534 Olive st. Gazzam, James Breading 514 Security bldg. Geeks, Frank 3453 Magnolia av. Gerling, H. J 4320 Cook av. Glasgow, FrankA 3894 Washington boul. Glasgow, William C 2847 Washington av. Goetz, Victor 129 Market st. Goldstein, Max A 3858 Westminster pi. Goodman, Charles H 3329 Washington av. Graham, Benjamin B 5145 Lindell boul. Graves, William W 1943 N. llth st. Graves, Willis Nelson 2813 Lafayette av. Gray, MelvinL 3756 Lindell boul. Greeley, Arthur W Washington University. Green, John 2670 Washington av. Gregory, ElishaHall 3525 Lucas av. Gregory, Elisha H., Jr.* Medical Dept., Univ. of Pa., Philadelphia. Grindon, Joseph 3894 Washington av. Gundelach, Chas. H 3900 Westminster pi. Gundelach, W. J 3703 Finney av. Gurney, James Tower Grove and Magnolia avs. Guy, William Evans 4380 Westminster pi. viii Trans. Acad. Sci. of St. Louis. Haarstick, Henry C Third and Chestnut sts. Hambach, Gustavf 1319 Lami st. Hardaway, W. A 2922 Locust st. Harris, James Arthur Washington University. Hartmann, Rudolph. 2020 Victor st. Held, George A International Bank. Herzog, William 3644 Botanical av. Hirschberg, Francis D 3818 Lindell boul. Hitchcock, Albert Spear* ..U. S. Dept. Agriculture, Washington, D. C. Hitchcock, George C 3877 Washington av. Holman, BI. L 3744 Finney av. Holmes, Joseph A Mines Dept., La.Purch. Exposition. Homan, George 323 Odd Fellows' bidg. Hough, Warwick Circuit Court, Room 1. Hughes, Charles Hamilton 3860 West Pine boul. Huiskamp, John E 5554 Cabanne av. Hume, H. Harold* Lake City, Fla. Hunicke, Henry August 3532 Victor st. Hurter, Julius 2346 S. 10th st. Hyatt, Robert J U. S. Weather Bureau. Irish, Henry C Mo. Botanical Garden. Ives, Halsey Cooley Museum of Fine Arts. Johnson, Reno De O.* Desloge, Mo. Jones, Breckinridge 4010 Lindell boul. Kail, Richard 1370 Goodfellow av. Keiser, Edward H Washington University. Keyes, Charles R.* State School of Mines, Socorro, New Mex. Kinealy, John H.* ..1108 Pemberton bIdg., Boston, Mass. King, Goodman 78 Vandeventer pi. Kirchner, Walter C. G 1211 N. Grand av. Klem, Mary J 1808^ Lafayette av. Kodis, Theodore* Schadow, Kowno, Russia. Krall, George Warren Manual Training School. Lackland, Rufus J 1623 Locust st. Langsdorf, Alexander S Washington University. t Elected a life-member January 3, 1882. Members. ix Leavitt, Shei-man Washington University. Lefevre, George* State University, Columbia, Mo. Leighton, George Bridge 803 Garrison av. Letterman, George W.* Allenton, Mo. Licliter, John J 1740 Simpson av. Lloyd, Hiram Odd Fellows' bldg. Loeb, Hanau Wolf 3559 Olive st. Ludwig, Charles V. F 1509 Chouteau av. Luedeking, Robert 1837 Lafayette av. LumeUus, J. George 1225 St. Ange av. Lyon, Hartwell Nelles 3910 Russell av. Mack, Charles Jacob 113 N. Broadway. Mallinckrodt, Edward 26 Vandeventer pi. Mallinckrodt, Edward, Jr 26 Vandeventer pi. Markham, George Dickson 4961 Berlin av. Marx, Christian William* University of Cincinnati, Cincinnati, O. Mason, Silas C* Berea, Ky. Matthews, Leonard 300 N, 4th st. McGee, W J World's Fair. Meier, Theodore G 3938 Washington boul. Merrell, Albert 3814 Washington boul. Meyer, John F 1739 Pennsylvania av. Michel, Eugene H 2721 S. King's Highway. Miller, Charles F 1751 Missouri av. Monell, Joseph T.* ....Flat River, Mo, Monroe, Lee Ernest* Eureka, Mo. Moore, Robert 61 Vandeventer pi. Mudd, Harvey G 2604 Locust st. Mueller, Ambrose* Webster Groves, Mo. Nagel, Charles 3969 Washington boul. Nasse, Aug 209 N. 2d st. Nautze, Gustav 2868 S. 18th st. Nelson, Aven* Laramie, Wyom. Niedringhaus, George W 3745 Lindell boul. Nipher, Francis E..... Washington University. Norton, J. B. S.* College Park, Md. Oglevee, Christopher Stoner* Lincoln, III. Olshausen, Ernest P 1115 Rutger st. Olshausen, George R.* Cornell University, Ithaca, N. Y. X Trans. Acad. Sci. of St. Louis. O'Reilly, Andrew J 1507 Papin st. O'Reilly, Robert J 3411 Pine st. Outten, W. B Missouri Pacific Hospital. Overstolz, Herman 100 N. Broadway. Palmer, Ernest Jesse* 321 S. Allen st,, Webb City, Mo. Pammel, Louis Hermann* Ames, la. Pantaleoni, Guido 415 Locust st. Parker, George Ward 417 Pine st. Parsons, Charles 2804 Pine st. Pauls, Gustavus St. Louis Altenheim. Pettus, W. H. H 4373 Westminster pi. Pfeiffer, Egmont 3921a Shenandoah av. Pike, Sherman B 5881 Cates av. Pitzman, Julius 1900 S. Compton av. Poats, Thomas Gra3^&on* Clemson College, S. C. Post, Martin Hayward 5371 Waterman av. Preetorius, Emil % Westliche Post. Prewitt, Theodore F 4917 Berlin av. Prynne, Charles Martyn Lincoln Trust bldg. Pulsifer, William H* Nonquitt, Mass. Quaintance, A. L.* U. S. Department of Agriculture, Washington, D. C. Randall, JohnE 1910 Olive st. Raphael, Abraham 5164 Raymond av. Ravold, Amand 2806 Morgan st. Reverchon, Julien* R. F. D. 8, Dallas, Texas. Richter, Phil. George 2424 S. 18th st. Rieloff, F. C 3837 W. Pine boul. Rilliet, Chas. E 4719 S. 9th st. Robert, Edward Scott 1105 Missouri Trust bldg. Robertson, Charles* Carlinville, 111. Roever, William Henry* Cambridge, Mass. Rogers, Herbert F V^ Provident Chemical Works. Rolfs, Peter H.* Tropical Laboratory, Miami, Fla. Rosenwald, Lucian* Las Vegas, New Mex. Ruf, Frank A 5863 Cabanne av. Runge, Edward C Vanol bldg. Russell, Colton* 325 S. Bunker Hill av., Los Angeles, Cal. Ryan, Frank K 2725 Lawton av. Members. xi Sander, Enno 2807 Lawton av. Sargent, Charles Sprague* Jamaica Plain, Mass. Schmalz, Leopold 2824 Shenandoah av. Schneck, Jacob* Mt. Carmel, 111. Von Schrenk, Hermann Mo. Botanical Garden. Schroers, John 1730 Missouri av. Schrowang, Otto Gay bldg. Schwab, Sidney I 2602 Locust st. Schwarz, Frank 1520 Lafayette av. Schwarz, Henry 1723 Chouteau av. Schweitzer, Paul* Columbia, Mo. Scott, Henry C 64 Vandeventer pi. See, Thomas Jefferson Jackson*. .Naval Observatory, Mare Island, Cal. Selby, Augustine Dawson* Wooster, O. Senseney, E. M 2829 Washington av. Sheldon, Walter L 4065 Delmar av. Shepley, John F 60 Vandeventer pi. Shoemaker, William Alfred 4386 Westminster pi. Simmons, E. C 9th and Spruce sts. Simmons, Wallace D 9th and Spruce sts. Sluder, Greenfield 2647 Washington av. Smith, Arthur George* 422 N. Dubuque st., Iowa City, la. Smith, D. S. H 3646 Washington boul. Smith, Irwin Z 87 Vandeventer pi. Smith, Jared G.* '. .Honolulu, Hawaiian Islands. Soldan, F. Louis ...3634 Flad av. Spiegelhalter, Joseph 2166 Lafayette av. Starkloff, H. M 3623 Cleveland av. Starr, John E.* 258 Broadway, New York City. Staudinger, B 3556,Lindell boul. Stedman, John Moore* State University, Columbia, Mo. Stevens, Charles D 1749 S. Grand av. Stevens, Wyandotte James 4043 Juniata st. Stocker, George J 2833 S. King's Highway. Strauss, Julius C 3516 Franklin av. Stuart, James Lyall 5346 Maple av. Summa, Hugo 2249 St. Louis av. Taussig, Albert E 2647 Washington av. Taussig, William 3447 Lafayette av. Teichmann, William C 1141 Market st. Terry, Robert James 4105 Washington av. xii Trans. Acad. Sci. of St. Louis. Thacher, Arthur 4304 Washington boul. Thorn, Charles* 239 Hazel St., Ithaca, N. Y. Thomas, John R 420 N. 4th st. Thomson, William H., Jr 3805 Lindell boul. Thurman, John vS 416 Lincoln Trust bidg. Timmerman, Arthur H 2633 Park av. Tittmann, Harold H 3726 Washington boul. Trelease, William Mo. Botanical Garden. Tyler, Elza Edward* State University, Columbia, Mo. Tyrrell, Warren Ayres 3620a Folsom av. Updegraff, Milton* 12 Goldsborough Row, Annapolis, Md. Valle, Jules F 3303 Washington av. Van Ornum, John Lane Washington University. Vickroy, Wilhelm Rees 2901 Rauschenbach av. von Schrader, George F Wainwright bldg. von Schrader, Otto U 3749 Westminster pi. Warren, William Homer 1806 Locust st. Watts, Millard F 4362 Morgan st. Weller, Stuart* University of Chicago, Chicago, 111. Westgate, John Minton* Dept. of Agriculture, Washington, D. C. Wheeler, H. A 3124 Locust st. Whelpley, Henry Milton 2342 Albion pi. Whitaker, Edw^-ds 300 N. 4th st. Whitten, John Charles*. Columbia, Mo. Widmann, Otto 5105 Morgan st. Wilson, Edward Allen 3745 W. Pine st. Winkelmeyer, Christopher 3540 Lawton av. Wislizenus, Frederick A 3628 Cleveland av. Witt, Thomas D.* Rushville, 111. Woodward, Calvin Milton Washington University. Zahorsky, John 1460 S. Grand av. Zawodny, Joseph* Schloss Lobes, Mscheno, bei Melnik, Bohemia, Austria. CONSTITUTION. ARTICLE I. NAME. Section 1. This Association shall be called "The Acad- emy OF Science of St. Louis." ARTICLE II. object. Section 1. It shall have for its object the promotion of science. Sec. 2. As means to this end the Academy shall hold meetings for the consideration and discussion of scientific subjects ; shall take measures to procure original papers upon such subjects; and shall, as often as may be practicable, publish its transactions. It shall also establish and maintain a cabinet of objects illustrative of the several departments of science, and a library of works relating to the same. It shall also place itself in communication with other scientific institutions. article hi. members. Section 1. The Academy shall consist of Active Members, Corresponding Members, Honorary Members, and Patrons. Sec. 2. Active Me7nbers shall be persons interested in science, and they alone shall conduct the affairs of the Academy. Sec. 3. Persons not living in the City or County of St. Louis who may be disposed to further the object of the Academy by original researches, contributions of speci- mens, or otherwise, may be elected Corresponding Members. Sec. 4. Persons not living in the City or County of St. xiv Trans. Acad. Sci. of St. Louis. Louis may be elected Honorary Members by virtue of their attainments in science. Sec. 5. Any person conveying to the Academy the sum of one thousand dollars ($1,000), or its equivalent, may be elected a Patron. Sec. 6. Persons may be admitted to any of the preceding classes of membership, or dismissed therefrom, in accordance with the regulations prescribed by the By-Laws, ARTICLE IV. OFFICERS. Section 1. The officers of the Academy shall be chosen from the active members, and they shall consist of a President, 1st Vice-President, 2d Vice-President, Recording Secretary, Corresponding Secretary, Treasurer, Librarian, Three Curators, Two Directors. Said officers shall be elected at the time and in the man- ner prescribed by the By-Laws, and shall hold their offices for one year, or until their successors are elected. Sec. 2. The duties of these officers shall be such as are customary and as prescribed by the By-Laws. ARTICLE V. COUNCIL. Section 1. The President, the two Vice-Presidents, the Recording Secretary, the Treasurer, the Librarian, and the two Directors shall constitute the Council of the Academy. Sec. 2. The duties of the Council shall be to consider all plans conducive to the welfare of the Academy; to audit all bills and order payment of such as they may approve ; Constitution. XV to consider all applications for membership ; and to adminis- ter the business of the Academy, subject to the Constitution and By-Laws and to such instructions as may be given by the Academy. ARTICLE VI. MEETINGS. Section 1. The meetings of the Academy shall be held at such times and places as the By-Laws may direct. ARTICLE VII. AMENDMENTS. Section 1. Amendments to this Constitution shall be sub- mitted in writing at a regular meeting. They shall be open to discussion until at least the second ipeeting thereafter. They may then be adopted by a two-thirds vote of a letter- ballot, conducted in the manner prescribed by the Council. ARTICLE VIII. SECTIONS. Section 1. To encourage and promote special investiga- tions in any branch of science, members of the Academy may form Sections which shall be constituted as herein provided. Sec. 2. For the formation of a Section written application shall be made to the Academy, at a regular meeting, by not less than six active members. On the approval of this application by the affirmative vote of two-thirds of the members present at the next regular meeting, the Section shall be established and the names of the petitioners shall be recorded on its minutes as its founders. Sec. 3. Sections may increase the number of their mem- bers by election, but only members of the Academy shall be elected members of any of the Sections . Sec. 4. The officers of each Section shall be a Chairman and a Secretary, who shall be elected by its members at the xvi Trans. Acad. Sci. of St. Louis. first meeting of the Section, and subsequently at the first meeting in January of each year. Sec. 5. The collections and books of each Section are the common property of the Academy. Donations of books and specimens made to or for any Section shall be received as donations to the Academy for the use of the Section. Sec. 6. A report of the proceedings of each Section shall be submitted to the Academy at least once every month. Papers read before any Section with a view to publication by the Academy shall take the same course as papers read before the Academy. Sec. 7. On all points not herein provided for, each Section shall be governed by the Constitution, By-Laws, and instructions of the Academy. BY-LAWS. I. REGULAR MEETINGS. The regular meetings of the Academy shall be held on the first and third Monday evenings of every month, unless otherwise ordered by the Council. II. SPECIAL MEETINGS. Special meetings may be called by the President at his dis- cretion, and shall be called by him on the written request of three or more members. III. NOTICE OF MEETINGS. The Recording Secretary shall send a notice of each meet- ing to every active member at least two days before such meetmg. IV. QUORUM. Seven members shall constitute a quorum, but four mem- bers shall constitute a legal meeting for reading of papers. V. ORDER OF BUSINESS. The order of proceeding, at the regular meetings of the Academy, shall be as follows: — 1. Minutes of last meetmg. 2. Report of the Council. 3. Reports of Committees. 4. Report of the Corresponding Secretary. 5. Donations to the Museum and Library. 6. Written Communications. 7. Oral Communications. 8. Deferred Business. 9. New Business. 10. Elections. 11. Proposals for Membership. 12. Adjournment. xviii Trans. Acad. Set. of St. Louis. VI. CORRESPONDING SECRETARY. It shall be the duty of the Corresponding Secretary to conduct the correspondence and report to the Academy. VII. TREASURER. The Treasurer shall collect all moneys due the Academy ; be custodian of all its funds, and pay such bills against the Academy as the Council shall approve. The Treasurer shall deposit the moneys and invest the funds of the Academy in its name and by and with the advice of the Council. Besides his annual report to the Academy, the Treasurer shall make such further reports and statements concerning the financial affairs of the Academy as the Council may from time to time require. Before entering upon his duties, the Treasurer shall give bond in such sum as may be required by the Council. VIII. LIBRARIAN. The Librarian shall take charge of all books belon^ins to or deposited with the Academy, and shall be responsible for the same; he shall keep a catalogue thereof, in which the names of contributors shall be inscribed ; he shall superintend the distribution of all the publications of the Academy. IX. COUNCIL. The Council shall act as a publication committee ; shall prepare a programme for each meeting, and may make rules and regulations for their own guidance, not inconsistent with the Constitution and By-Laws. X. ELECTION OF OFFICERS. A nominating committee of three active members who are not oflacers of the Academy shall be elected at the first regu- lar meeting in December. This committee shall nominate By-Laws. xix candidates for all the offices for the ensuing year, and report the nominations at the following meeting, when other nom- inations may be made by any active member. The Recording Secretary shall mail to every active member a list of the nom- inees for office, at least ten days preceding the annual meet- ing. The polls shall be closed at 6 p. m. on the day of the annual meeting, after which the nominating committee shall count the ballots and announce the results to the Academy. A plurality of the votes cast shall suffice to elect. XI. VACANCIES. A vacancy in any office shall be filled by election conducted in the same manner as the annual election. XII. ELECTION OF MEMBERS. A candidate for admission to the Academy shall be pro- posed by not less than two members at any regular meeting. The proposal must then be referred to the Council, and if upon examination they shall find the candidate to be eligible and' worthy of membership, they shall order the question as to his admission to be submitted to the Academy by ballot. If there be five votes in the negative, the candidate shall be re- jected, and shall not be again voted upon for twelve months after such rejection. But if the number of negative votes be less than five, the candidate shall be elected, but shall not be considered a member until he shall have paid the initiation fee and the annual dues for the current year. Any failure to pay the initiation fee and annual dues within thirty days after the candidate has been notified of his election, shall work a forfeiture of all rights under said election, if the Council shall so determine. No entry shall be made on the record of the rejection of any candidate. XIII. RESIGNATION OF MEMBERS. Any member whose dues have been fully paid, may with- draw from the Academy by a written resignation. Non-pay- XX Trans. Acad. Sci. of St. Louis. ment of dues for one year or longer may be treated as equivalent to resignation ; but before any member is dropped from the rolls for delinquency, he shall be entitled to not less than four weeks' notice. XIV. EXPULSION OF MEMBERS. Upon the written request of five members, that, for cause stated, any member be expelled, the Council shall consider the matter, and if they deem it best, shall advise the member that his resignation will be accepted. He shall, however, have the right to demand and shall be given a copy of the •charges against him, and shall have a reasonable time to pre- sent a written defense. The Council may then pass finally upon the matter, and if resignation has not been tendered, or a satisfactory defense made, may by an afiirmative vote of four of their number expel the member, in which case they shall notify him and the Academy of their action, and his name shall be at once dropped from the list of members. XV. INITIATION FEE AND DUES. Resident active members shall pay an initiation fee of five dollars, and annual dues of six dollars, payable at the begin- ning of each year. Non-resident active members shall pay an initiation fee of five dollars and annual dues of one-half the dues for resident active members, payable at the begin- ning of each year. XVI. HONORARY MEMBERS AND PATRONS. Honorary members and Patrons shall be recommended by the Council, and elected by the unanimous vote of the mem- bers present at any regular meeting. XVII. PUBLICATIONS. Patrons and all active members not in arrears shall be entitled to one copy of all the publications of the Academy By-Laws. xxi issued subsequent to their election. Authors of papers shall be entitled to twenty extra copies of their individual papers. XVIII. SALE OF REAL ESTATE. The property convej^ed to The Academy of Science of St. Louis on the eighteenth day of March, 1903, by Edgar R. Hoadley and Lavinia L. Hoadley, as a gift from Mrs. Eliza McMillan and William N. McMillan, shall not be morta:as:ed or voluntarily incumbered by the Academy of Science ; and the said property shall not be sold, except with the consent of two-thirds of the members of the Academy of Science, obtained by letter ballot, in such manner as may be pre- scribed by the Council, and, when sold, the proceeds of the sale or so much thereof as may be necessary, shall be used to provide a suitable location and building for the use of The Academy of Science of St Louis. XIX. AUTHORITY. On all points of order and procedure, not provided for in the Constitution and By-Laws, Robert's Rules of Order shall be the authority. XX. AMENDMENTS. These By-Laws may be amended by a two-thirds vote of all the members present at any regular meeting, provided notice of the proposed amendment shall have been mailed to every member at least one week before the vote thereon is taken. ABSTRACT OF HISTORY. ORGANIZATION, The Academy of Science of St. Louis was organized on the 10th of March, 1856, in the hall of the Board of Public Schools. Dr. George Engelmann was the first President. CHARTER. On the 17th of January following, a charter incorporating the Academy was signed and approved, and this was accepted by vote of the Academy on the 9th of February, 1857. OBJECTS. The act of incorporation declares the object of the Academy to be the advancement of science and the establishment in St. Louis of a museum and library for the illustration and study of its various branches, and provides that the members shall acquire no individual property in the real estate, cabinets, library, or other of its effects, their interest being usufruc- tuary merely. The constitution as adopted at the organization meeting and amended at various times subsequently, provides for hold- ins meetino;s for the consideration and discussion of scientific subjects ; taking measures to procure original papers upon such subjects ; the publication of transactions ; the establishment and maintenance of a cabinet of objects illustrative of the several departments of science, and a library of works relating to the same; and the establishment of relations with other scientific institutions. To encourage and promote special in- vestigation in any branch of science, the formation of special sections under the charter is provided for. Abstract of History. xxiii MEMBERSHIP. Members are classified as active members, corresponding members, honorary members and patrons. Active member- ship is limited to persons interested in science, though they need not of necessity be engaged in scientific work, and they alone conduct the affairs of the Academy, under its constitu- tion. Persons not living in the city or county of St. Louis who are disposed to further the objects of the Academy, by original researches, contributions of specimens, or otherwise, are eligible as corresponding members. Persons not living in the city or county of St. Louis are eligible as honorary members by virtue of their attainments in science. Any person conveying to the Academy the sum of one thousand dollars or its equivalent becomes eligible as a patron. Under the by-laws, resident active members pay an initia- tion fee of five dollars and annual dues of six dollars. Non- resident active members pay the same initiation fee, but annual dues of three dollars only. Patrons, and honorary and corresponding members, are exempt from the payment of dues. Each patron and active member not in arrears is entitled to one copy of each publication of the Academy issued after his election, Since the organization of the Academy, 967 persons have been elected to active membership, of whom, at the present time, 292 are carried on the list. Four patrons, Mr. Edwin Harrison, Mrs. Eliza McMillan, Mrs. William Northrop McMillan and Mr. Henry W. Eliot, have been elected. The list of corresponding members (Vol. X., p. xii) includes 205 names, among which are the names of 102 persons known to be deceased. OFFICERS AND MANAGEMENT. The officers, who are chosen from the active members, con- sist of a President, two Vice-Presidents, Recording and Cor- responding Secretaries, Treasurer, Librarian, three Curators, and two Directors. The general business management of the XXIV Trans. Acad. Sci. of St. Louis. Academy is vested in a Council composed of the President, the two Vice-Presidents, the Recording Secretary, the Treas- urer, the Librarian and the two Directors. The office of President has been filled by the following well-known citizens of St. Louis, nearly all of whom have been eminent in some line of scientific work : George Enorel- mann, Benjamin F. Shumard, Adolphus Wislizenus, Hiram A. Prout, John B. Johnson, James B. Eads, William T. Harris, Charles V. Riley, Francis E. Nipher, Henry S. Pritchett, John Green, Melvin L. Gray, Edmund A. Engler, Robert Moore, and Henry W. Eliot. MEETINGS. The regular meetings of the Academy are held at its build- ing, 3817 Olive Street, at 8 o'clock, on the first and third Monday evenings of each month, a recess being taken between the meeting on the first Monday in June and the meeting on the third Monday in October. These meetings, to which in- terested persons are always welcome, are devoted in part to the reading of technical papers designed for publication in the Academy's Transactions, and in part to the presentation of more popular abstracts of recent investigation or progress. From time to time public lectures, calculated to interest a larger audience, are provided for in some suitable hall. The following dates for regular meetings for the year 1904 have been fixed by the Council : — Jan. 18 Feb. 1 Mar.v April. May. June. Oct. Nov. 7 4 2 6 7 15 21 18 16 17 21 Dec. 19 LIBRARY. After its organization, the Academy met in Pope's Medical College, w^here a creditable beginning had been made toward Abstract of History. xxv the formation of a museum and library, until May, 1869, when the building and museum were destroyed by fire, the library being saved. The library now contains 14,893 books and 11,663 pamphlets, and is open during certain hours of the day for consultation by members and persons engaged in scientific work. PUBLICATIONS AND EXCHANGES. Thirteen thick octavo volumes of Transactions have been published since the organization of the Academy, and widely distributed. Two quarto publications have also been issued: one from the Archaeological section, being a contribution to the archaeology of Missouri, and the other a report of the observations made by the Washington University Eclipse Party of 1889. The Academy now stands in exchange rela- tions with 576 institutions or organizations of aims similar to its own. MUSEUM. Since the loss of its first museum, in 1869, the Academy has lacked adequate room for the arrangement of a public museum, and, although small museum accessions have been received and cared for, its main effort of necessity has been concentrated on the holding of meetings, the formation of a library, the publication of worthy scientific matter, and the maintenance of relations with other scientific bodies. RECORD. From January 1, 1903, to December 31, 1903. January 5, 1903. President Eliot in the chair, twenty-two persons present. The nominating committee reported that 138 ballots had been counted, and the following officers for 1903 were declared duly elected : — President Henry W. Eliot. First Vice-President D. S. H. Smith. Second Vice-President William K. Bixby. Recording Secretary William Trelease. Corresponding Secretary... .Ernest P. Olshausen. Treasurer Enno Sander. Librarian G. Hambach. Curators G. Hambach, Julius Hurter, A. H. Timmerman. Directors F. E. Nipher, Adolf Alt. The President addressed the members present, on the con- dition of the Academy, and its work during the year 1902.* The Treasurer submitted his annual report, showing in- vested funds to the amount of $6,500.00 and a current balance of $358.09 carried forward to the year 1903. t The Librarian submitted his annual report. + The Council reported that the resignation of Mr. A. T. Primm, Jr., and Mr. G. R. Kline had been accepted, and that the followino; additions had been made to the exchange list: R. Accademia . . . degli zelanti, Acireale; Broteria, Lis- * Transactions 12:xxix. t Transactions 12 : xxxi. X Transactions 12 : xxxi. Record. xxvii bon ; The Zoological Department of the University of Cali- fornia, Berkeley; and the Museum of the Institute of Arts and Sciences, Brooklyn. On behalf of Mr. Hurter, who represented the Academy at the Fifth International Congress of Zoologists, held in Berlin in 1901, the Secretary presented to the library of the Academy a copy of the report of said Congress. Mr. Julius Hurter presented for publication a paper on the herpetology of Missouri, illustrating his remarks by speci- mens. Dr. Hermann von Schrenk presented some notes on the bitter-rot disease of apples, referring particularly to recent investigations and cultural experiments. He exhibited speci- mens of the cankers formed on apple limbs by the bitter- rot fungus (Gloeosporiiun fructigenum^ Berk.) in various orchards, and of artificial cankers produced in apple trees at the Missouri Botanical Garden by inoculating branches with spores from apples aifected with the bitter-rot disease, and spores from pure cultures of the fungus from cankers occurring naturally in the orchard. Cultures showing the perfect or ascus stage of the fungus were exhibited, and attention was called to the fact that up to date the perfect form had been found only in cultures and on several apples kept in the laboratory. He announced the discovery two weeks ago, by Mr. Perley Spaulding, of the perithecia and perfectly formed asci and ascospores of the bitter-rot fungus in several of the cankers produced on apple limbs from pure cultures of the bitter-rot fungus as well as from bitter-rot spores taken from cankers obtained in an affected orchard. This discovery is considered extremely important, as it dem- onstrates, for the first time, beyond question, that the bitter- rot fungus actually produces its perfect fruit in the cankers, and thereby strengthens the contention that the cankers on apple limbs are actually formed by the bitter-rot fungus. The asci are apparently as evanescent in the cankers as they are in cultures, and it is therefore not at all improbable that many of the supposed pycnidial spores found in both the natural and artificially produced cankers were really ascospores. xxviii Trans. Acad. Set. of St. Louis. Drawings were exhibited showing the perithecia found in the cankers with asci and ascospores. Mess. R. Kail and Th. Lange, of St. Louis, were elected to active membership. Two persons were proposed for active membership. January 19, 1903. President Eliot in the chair, twenty-seven persons present. The Council reported that the regular edition of the Acad- emy's Transactions had been increased from 1,000 to 1,100; that the resignation of Mr. F. W. Biebinsfer and Mr. Victor Goetz had been accepted ; and that exchange relations had been discontinued with the Anthropologische Gesellschaft, of Vienna. Mr. W. L. Sheldon presented a summary of the progress in the science of ethics, since the publication of Darwin's " Descent of Man," in 1871. Miss Mary J. Klem and Mr. Charles E. Rilliet, of St. Louis, were elected to active membership. One person was proposed for active membership. February 2, 1903. Professor Nipher in the chair, twenty-four persons present. The Council reported that the Academia Nacional, of Cordova, had been dropped from the exchange list, and that the Deutscher Verein Zum Schutze der Vogelwelt had been added to the list. Dr. Tarleton H. Bean delivered an interestino; illustrated address on the salmon and salmon fisheries of Alaska. Dr. R. J. Terry reported on a case of right aortic arch in man — of relatively rare occurrence — and, with the aid of lantern slides and blackboard diagrams, indicated its peculiar features and morphological significance. Dr. W. J. Gundelach, of St. Louis, was elected to active membership. One person was proposed for active membership. Record. xxix February 16, 1903. Vice-President Smith in the chair, sixteen persons present. Professor A, W. Greeley gave an account of recent experiments on the effects on protoplasm of variations in temperature and in the water content of the cells. It was shown that in the case of certain algae, protozoa, and the eggs of some marine invertebrates, a reduction of temperature gave rise to parthenogenetic spore formation or egg segmen- tation, as was also the case when, by suitable plasmolysis, water was withdrawn from the cells. Mr. CM. Prynne, of St. Louis, was elected to active membership. March 2, 1903. Dr. John Green in the chair, nine persons present. Professor F. E. Nipher gave an account of his experiments in the production of ether waves by means of explosions. He is now using a brass tube, six feet long and one and one-third inch in diameter, for the explosive, which is laid in a train from end to end. This tube is placed within a large brass tube, one and three-eighths inch in diameter, which is wound with 25,700 windings of No. 25 copper wire. This coil is connected with a delicate D'Arsonval galvanometer. The coil is placed with its axis in the magnetic meridian. When gunpowder is exploded in the inner tube, the galvano- meter gives indication of a change in permeability of the heated channel within the coil. The results were said to be as yet inconclusive, and the apparatus is to be somewhat modilied with a view to making it more sensitive. March 16, 1903. Vice-President Smith in the chair, twenty-eight persons present. Dr. H. M. Whelpley gave an account of the sacred pipe- stone quarries of the Upper Missouri, illustrating his remarks XXX Trans. Acad. Sci. of St. Loxiis. by the use of lantern slides, some of them from photographs taken by him at the quarries and others reproducing views published by Catlin and others. April 6, 1903. President Eliot in the chair, twenty persons present. The Council reported that the property now occupied by the Phillips School, on Olive Street between Spring and Vande- venter, had been purchased by Mrs. Eliza McMillan and her son, Mr. William Northrop McMillan, and deeded to the Academy as a memorial to the late William McMillian, who, at the time of his death, was a member of the Academy. The gift was referred to the Academy for appropriate action, with the recommendation on the part of the Council that Mrs. McMillan and her son be elected patrons of the Academy. The President stated that in connection with this announce- ment by the Council he wished to say that it had been thought advisable by the Council that the gift, which was made for the purpose of giving the Academy a permanent home, should be surrounded b}'^ proper restrictions as to any future sale of the propert}^ which should insure the permanent possession of a home by the Academy, and that he trusted that action would be taken which should prevent the alienation at any time of this property without the contingent acquisition of an equal or better building for the Academy's use. Professor Nipher said : — Mr. President and Qentlemen of the Academy : I cannot allow this occasion to pass without calling attention to the great significance of the announcement which has been made this evening. Ever since the Academy was organized, in March, 1856, its work has been done under the most discouraging circumstances. It has never had a home. Its meetings have been held in the meeting room of the Board of Education, at a medical college, at Washington University, and in the rooms of th« Missouri Historical Society. It has never had its own home, where it might make its valuable library and its collections of real service to the citizens of our city. During all these years of its existence the Academy has been collecting a library of scientific publications, in exchange with similar societies in all parts of the world. Our published Transactions have gone to every civilized land. We have certainly had the outward semblance of great scientific activity. There is no local Academy of Science in this Record. xxxi country which can present a more creditable record of published work. Even during the civil war, when almost every educational interest suffered, a few working investigators aided by others who gave such support as they could give, continued to produce before this body their contributions to knowledge, and to publish them to the world in the Transactions of the Academy. During all of this time these pioneers have been hoping to see this day. Year after year the President's annual report has called attention to the vital necessity of a fixed abiding place which we could own and control. Without this we could never hope to establish a public museum of Science, or to avail ourselves of our precious library. And now the first great advance has been made. This gift to the cause we have been striving to uphold, could not have been more opportune. These enlightened patrons of higher learning have seen their opportunity, and they have volunteered their aid. The manner in which they have be- stowed their bounty makes it doubly valuable and effective. They have made it impossible for us to honor them by any act within our power. They have become one with us in the cause which we have all labored to advance. May we not hope that they will permit us to enroll their names in our membership as Patrons of the Academy? And this gift brings with it new obligations for us. We should now seek to establish an endowment fund, which will enable us to make our valuable collection of books and specimens fully available to the public. During the World's Fair we shall be under examination. Learned men from this and other lands will come among us. The great public will be here. The location of our new home is such that we cannot fail to attract the attention of vast numbers of our visitors. We should not only have a museum and library which will be an honor to our city, but it should be open to all. We wish to show that we have here, among the permanent institutions of our city, an Academy of Science wiiich is dedicated to the advancement of human learning, and to the diffusion of knowledge among men. In this way we shall fittingly carry out the work which Mrs. William McMillan and her son, Mr. William Northrop McMillan, have so nobly begun. The following resolutions, introduced by Professor Nipher and seconded by Dr. Ewing, were unanimously adopted, and the Secretary Avas instructed to communicate a copy of them to Mrs. McMillan and Mr. McMillan: — Besolved, That the members of The Academy of Science of St. Louis most gratefully accept from Mrs. Eliza McMillan and Mr. William N. McMillan the gift of a permanent home for the Academy. We feel that this generous donation will infuse new life into the institution, and will insure its future usefulness. We pledge ourselves to use every effort to make it worthy of the confidence thus shown by the donors and to maintain the object of its founders, as expressed in the Act of Incorporation — "the advancement of science and the establishment in St. Louis of a museum and library for the illustration and study of its various branches." xxxii Trans. Acad. Set. of St. Louis. Besolved, by the members of The Academy of Science of St. Louis, that the property conveyed on the 18th day of March, 1903, by Edgar R. Hoad- ley and Lavinia L. Hoadley, to The Academy of Science of St. Louis, which property is the gift of Mrs. Eliza McMillan and William N. McMillan, shall not be mortgaged or incumbered so long as it remains the property of The Academy of Science. Besolved, further, that the property shall not be sold except by a two- thirds vote of the members of The Academy of Science of St. Louis by letter-ballot in the manner prescribed by the Council, and that when sold, the proceeds of the sale, or as much thereof as may be necessary, shall be used to provide a suitable location and building for the uses of The Academy of Science. Mrs. Eliza McMillan and Mr. William Northrop McMillan were elected patrons of the Academy, on nomination of the Council. Professor A. S. Chessin presented the following communi- cation on the strains and stresses in a rotating thin circular disc : — The problem of determining the strains and stresses in a rotating disc or, as it is commonly known, the problem of the fly-wheel, is still an open one so far as a general solution is considered. The present paper deals only with very thin discs but the method of obtaining a solution may be readily extended to the more general problem. Let the axis of the disc be the axis of z, and let r be the radius vector to any point drawn perpendicular to this axis, and 0 the angle between the direction of r and a fixed plane through the axis ; also let ii and w be the displacements in the direction of the radius and the axis ; finally let p be the density of the solid, &> the angular velocity of its rotation and 2h its thickness. If the disc be isotropic the stresses are (1) rr - Cll := XA + 2/U, — , 66 = u = XA + 2yLt - , zz - 9w -XA + 2/i^, dZ rz \3z c)' J Record. XXXlll 3u u 97V where A = ^;; — |- — h ^=^5 and the problem consists in inte- grating the differential equations (2 9 1 9 11^ u,\ 9hi. 9'^w 9r9z 0 ii' 9 I 9w\ 9'^w where the function (3) u, = u pco^ 8(2/x + X) ».3 has been introduced in place of w. At the same time the following surface conditions must be satisfied : I. Full disc (0 ^^i» • • • ^^e functions of r only. Substituting these expressions of u^ and ly in (2) we find that this system of differential equations may be replaced by the following jone fjt' d / dii\ 'CZW,, M, /cm,, M,,\ (8) +2(M + M(sr+r") = 0, = 0, Becord. while the surface conditions for z ^ ± h become XXXV (9) 0=h^' + ¥ j::' + dw. dr . + 2«,, + 4h\^^ + + (2it^ + X) M7o + 3(2/X + X)7i22(;^ + . . . . For very thin discs we may neglect the powers of z and h higher than the first. Then, to determine u-^^ and iv^, we have the first of the equations (7) together with the surface conditions dwn (9 bis) 0=-^'+2u,^, Xpco^ nlu. ( 10 bis) 2(2^x-) »•' = M*^ + . ) + ( 2/^ + ^) -«• from which we can eliminate u^^. The problem now is very simple and we give below only the results. I. Full disc* "-8e(1 "'^^ 1 + 0- pco"^ w — — ^^(T{1 +a-)z '3+0- _2(l + cr)^ rz 0; zz ■ 0; rr — ^^ {1 ^ pa,2(l + 2(l + <7) (3 + 0-)i?^27^,2 ^6' = pa)2(l+o-)(3 + (r) 4E 4E 5 — 60- i?,2+i^^.___^^,2 + pa>''{l+a)(3+a)B,'Ii, 4E Professor F. E. Nipher reported that he had apparently succeeded in producing a distortion of a magnetic field by means of explosions. The apparatus used was a transformer consisting of concentric coils wound upon brass tubes. The outer tube was five inches in diameter and six feet long, wound Avith over four thousand windings of No. 16 wire. This coil was traversed by a continuous current from a storage battery. Within this and separated from it by an air-space of an inch, is a secondary coil of equal length having over twenty-five thousand windings of No. 25 wire. This coil is connected to a D'Arsonval ofulvanometer. Within the tube on which this coil is wound is a smaller brass tube within which a train of black gunpowder is laid. This tube is open at both ends, and has practically no recoil when the explosion is made. When hung by a bifilar suspension on cords ten feet in length , the recoil is about an inch. When the exciting current is small compared with the capacity of the battery, the galvano- meter reading is very steady. When the train is exploded a sudden and marked throw of the galvanometer results, which Record. xxxvii could be accounted for by an increase in the permeability of the long explosion chamber. The deflection reverses when the field is reversed. The hot gases liberated in the explo- sion are all diamagnetic, and tend to decrease the observed effect. In two cases the galvanometer deflection was in the opposite direction from that stated above, and this is being further inquired into. When seven tubes between the two coils are simultaneously exploded, only slight effects could be obtained, and these deflections are wavering, or to and fro, in character. A wire was threaded through the inner com- bustion tube, through which a current of three amperes was passed. This circuit was opened and closed with no visible effect. The galvanometer circuit is shielded by tin-foil, which is also connected with the explosion tube, and grounded. Sparks an inch long to the tin-foil produce no result. When the explosion tube is removed from the transformer, and taken near the galvanometer, or the storage battery, no deflection is produced by the explosion. An explosive mixture of gases from water electrolysis under atmospheric pressure produces a much less violent explosion, and produces a correspondingly less effect. The scale reading of the galvanometer changes by over twenty divisions with the heaviest explosions, and an exciting current of 0.6 ampere. With smaller explosions or feebler current, the effect is diminished. No deflections can be produced by striking the table upon which the transformer rests, or by striking the transformer itself, even when it moves slightly under the blow. The secondary and primary coils are held rigidly in fixed position with respect to each other. Arrangements have now been made to place the explosion tube in the focal line of a parabolic cylinder of metal, the galvanometer coil being in the focal line of a similar mirror. Either or both are to be surrounded by an exciting coil. This line of research was suggested by Young's account of his observation of five solar outbursts in 1872, which were each accompanied by sharp fluctuations in the magnetic trac- ings at Kew and Stonyhurst. Since the experiments began. xxxviii Trans. Acad. Sci. of St. Louis. volcanic explosions have produced such ether waves, which have been simultaneously recorded over the continents of Europe and America. April 20, 1903. President Eliot in the chair, twenty-two persons present. Professor J. A. Holmes gave an account of some of the efforts that are being made in the United States to preserve the forests and other natural features of the country, show- ing what is being done for the preservation of some of the great scenic features and particularly what the National Gov- ernment is doing in the establishment of national parks and forest reserves, and in the protection of their forests. The lecture was illustrated by a series of lantern slides. Dr. Alexander N. De Menil was elected to active member- ship. May 4, 1903. President Eliot in the chair, thirteen persons present. Mr. H. A. Wheeler gave an account, illustrated by several lantern slides and some of the ejected material, of the active Mexican volcano Colima, in which it was shown that the material now being ejected is a trachyte or belongs to the acid series of lavas, while the basal plain of the volcano is basalt, which is basic, and resting on volcanic tufa. It was pointed out that this sequence reverses the Richtopen order, from which it was considered probable that there had been other centers of lava outflow besides the now visible vents of Mt. Colima (active) and Mt. Zapotlan (inactive). Samples of the ash from the eruption of February 28, collected at Tuxpan, some 25 miles from the crater, by Prof. Trelease, contained 62.5% silica, according to the analysis of Wm. M. Chauvenet. Mr. Trelease, who had been near the base of the mountain during its recent activity, made a few remarks in connection with the paper. The following amendments to the By-Laws, recommended Record. xxxix by the Council, and notice of which was mailed by the Secre- tary to each member on April 23, were adopted by a unani- mous vote of the members present. By-Laws 18 and 19 were changed respectively to 19, Authority, and 20, Amendments; and the following new By-Law was adopted : — XVIII. Sale of Real Estate. The property conveyed to The Academy of Science of St. Louis on the eighteenth day of March, 1903, by Edgar R. Hoadley and Lavinia L. Hoad- ley, as a gift from Mrs. Eliza McMillan and William N. McMillan, shall not be mortgaged or voluntarily incumbered by the Academy of Science; and the said property shall not be sold, except with the consent of two-thirds of the members of the Academy of Science, obtained by letter ballot, in such manner as may be prescribed by the Council, and, when sold, the proceeds of the sale or so much thereof as may be necessary, shall be used to provide a suitable location and building for the use of The Academy of Science of St. Louis. One person was proposed for active membership. May 18, 1903. President Eliot in the chair, fifty persons present. Dr. C. Barck gave a detailed account of the Grand Canon of the Colorado, with lantern illustrations, and reported the first deliberate crossing of the Canon, by Mr. James and himself, in 1901. Restated that, starting from Bass's camp, about twenty-four miles west of the Bright Angel hotel, they had reached "Point Sublime" on the northern rim on the fifth day, after some difiicult traveling, the return taking three days. Dr. Robert Luedeking, of St. Louis, was elected to active membership. One person was proposed for active membership. June 1, 1903. President Eliot in the chair, fifteen persons present. Drs. B. M. Bolton and D. L. Harris exhibited sections cut xl Trans. Acad. Sci. of St. Louis. after infiltration with agar-agar, and described the use of this material for imbedding purposes as follows : — Tissues can be readily hardened and imbedded for cutting into sections in a hot solution of agar-agar containing formalin. The proportions of the mixture which have so far yielded the best results are nine parts of a five per cent aqueous solution of agar-agar to one part formalin. This mixture can be prepared beforehand and kept indefinitely in an air-tight vessel. The agar-agar should be boiled for several hours, and after the addition of the formalin allowed to clear by sedimentation. The bits of tissue to be imbedded are placed in a wide test-tube or wide-mouth vial containins: the mixture previously melted. This is kept at 65-70° C. for an hour or longer, and the tissues are ready to be blocked. After attach- ing to blocks they are placed in strong or absolute alcohol for an hour or two and can then be cut. It is important not to use dilute alcohol. The tissues are stuck to the blocks by means of the agar-agar itself and adhere as soon as the agar becomes cold. No previous hardening of the tissues is at all necessary, fresh tissues can be placed at once into the hot agar-agar-formalin mixture — in fact, fresh tissue is more desirable than that which has been previously hardened, though this can be readily imbedded by this method. But the main advantage of the method, aside from its convenience and sim- plicity, is the fact that the cells of , the tissues are not at all con- tracted or shrunken, and the ordinary methods of hardening have this effect more or less. With sections prepared from fresh tissues by this method the cell-protoplasm fills out the membrane fully, and the granules of the protoplasm, the nuclei, and the cell contours are remarkably distinct. The whole process, hardening, imbedding and cutting, does not occupy more than three or four hours, where the tissues are not larger than about one centimeter in diameter. Professor A. W. Grreeley presented the results of an in- vestigation of the reactions of Paramecia and other protozoa to chemical and electrical stimuli.* Two persons were proposed for active membership. * Science n. s. 17:980. Record. xli October 19, 1903. President Eliot in the chair, thirty-five persons present. This was the first meeting held in the new Academy Building, 3817 Olive street. The Council reported that the following names had been dropped from the membership roll: J. H. Boogher, M. F. Engman, E. Grebe, A, Habermaas, A. A. Henske, J. Maser- ang, Jr., C. H. Stone, O. Sutter, and O. M. Wood; that the resignation of Professor A. S. Chessin had been accepted ; and that the Zoological Institute, Cagliari, had been added to the exchange list. Professor F. E. Nipher gave an abstract of the results of his paper on the " Law of Nebular Contraction," which has just been published in the Transactions. He also remarked that the molecular conditions iu nebulae of different gases were being examined, and some very interesting results are at once evident. If a series of nebulae of various gases have the same mass internal to the same radius, the average mole- cular velocities would be the same for all gases. The velocity which would enable a molecule to escape from the nebula is 2.71 times the average molecular velocity, and this ratio is constant for all parts of the nebula. If the entire solar system formed the core of such a nebula, and the mass of the solar system extended to Neptune's orbit, the density at that distance from the center of the nucleus would be less than that in a Crookes tube. This opens up some very interesting questions concerning the history of such a mass. It would appear that such a gravitating mass would lose some heat by the escape of the more rapidly moving molecules, as well as by radiation. Professor E. H. Keiser read a paper on a method of de- terminino; the amount of lime in cements. He finds that this can be done by determining the amount of water ab- sorbed. By measuring this absorption in samples containing known amounts, the precautions to be taken in manipulation have been found. The determination only requires about twenty minutes. xlii Trans. Acad. Sci. of St. Louis. Professor F. E. Nipher presented a diagram on which was drawn the curve of speed of the trotting horse. This curve represents the equation published by him twenty years ago. On the same diagram was shown a belt of observed values representing the performance of every horse who has broken the speed record since 1845. In some cases a single horse has broken the record several times in the same year. All such observations were included. The points representing these observations formed a belt within which was the curve of predicted speed. The agreement was considered very satisfactory. Mess. Edward Mallinckrodt, Jr., Gustav Nautze, and A. Kaphael, were elected to active membership. Five persons were proposed for active membership. November 2, 1903. Vice-President Smith in the chair, thirty-five persons present. The following papers were presented, accompanied by abstracts: B. F. Bush, A new genus of grasses; J. A. Harris, Polj^gamy in Solanum; and J. A. Harris, The germi- nation of Pachira, with a note on the names of two species. Mr. Trelease read an address on The Academy of Science of St. Louis — a biography.* Mess. J. A. Harris, H. C. Irish, W J McGee and Oscar Riddle, of St. Louis, and Dr. Jos. Zawodny, of Schloss Lobes, Mscheuo-Melnik, Bohemia, were elected to active membership. November 16, 1903. Vice-President Smith in the chair, twenty-two persons present. The Council reported the death of Dr. J. B. Johnson and Mr. I. W. Morton. Popular Science Monthly. 64: 117. Record. xliii Professor A. W. Greelej' presented a report on experi- ments on the nature of the contraction of muscle. These experiments were undertaken with the view of working out more fully the mechanism involved in the galvanotropic and chemotropic reactions of Paramecia in acid and alkaline media, as described in Mr. Greeley's report before the Academy last spring. In the experiments on the contraction of muscle, it was found that when the medusa, Goniomemius, was exposed to the constant current, rhythmical contraction began always on the cathodal side when the medusa was immersed in normal sea water, but that the contractions began on the anodal side in acidulated sea water. Likewise it was shown that acids induce a phase of contraction, alkalis a phase of relaxation. It was suggested that these results may throw some light on the supposed electrical nature of muscle contraction, and that they offer additional evidence toward the conclusion that the charge carried by the pro- toplasmic particles depends on certain definite chemical conditions of the surrounding medium. Two persons were proposed for active membership. December 7, 1903. Vice-President Smith in the chair, forty persons present. The Chairman stated that because of the necessity of pro- viding the new building with fuel, furniture, lighting appli- ances, etc., the expenses of moving, added insurance, the final payment on the Yandell collection, and other unusual expenses, the Council was confronted by the necessity of temporarily raising some $1,750.00, which it was hoped could be repaid in a few months, after suitable arrangements had been made for securing revenue by renting meeting accommo- dations in the Academy Building to other societies. He stated that as this was a very important matter, the Council wished action on it to be taken by the Academy. On motion, the Council was authorized, by a unanimous vote, to raise the necessary sum by borrowing on the securities representing xliv Trans. Acad. Sci. of St. Louis. invested funds, it being understood that no lien of any kind should be attached to the real property of the Academy. The Council reported the resignation of Mess. Frank Thilly, J. M. Holzinger and Arthur Winslow. Dr. Adolf Alt read an interesting paper entitled What is a cataract? — illustrated by diagrams and lantern views from specimens selected from his personal collection. Dr. H. M. Whelpley exhibited a minute particle of radium, the remarkable activity of which was beautifully shown in a special form of hand apparatus now on the market for such demonstration. In accordance Avith the By-Laws of the Academy, a com- mittee, which consisted of Mess. Krall, Barck and Wid- mann, was elected to nominate officers for the year 1904. Dr. A. E. Eycelshymer and Mr. Hiram Lloyd, of St. Louis, were elected to active membership. Four persons were proposed for active membership. December 21, 1903. Vice-President Smith in the Chair, twenty-eight persons present. The Council reported that the resignation of Mess. A. H. Muegge and Oscar Riddle had been accepted, and that, under the instructions given at the last meeting, arrangements had been made for borrowing $1,750.00 for sixty days, on in- vestment securities. The nominating committee reported the following list of candidates for the year 1904 : — President W . K. Bixby. First Vice-President William Trelease. Second Vice-President Adolf Alt. Recording Secretary Ernest P. Olshausen. Corres^ponding Secretary August Hunicke. Treasurer Enno Sander. Librarian G. Hambach, Curators G. Hambacb, Julius Hurler, Frank Schwarz. Directors F. E. Nipher, Jos. Spiegelhalter. Record. xlv Other nominations were called for, but none were made. Mr. Robert Moore presented, with diagrams, a paper entitled Vital statistics of St. Louis from 1840 to 1902. On motion, the President was authorized to sign a petition to the President of the United States for aid in preserving groves of the Calaveras big trees, which was presented by the Outdoor Art League. Mr. T. W. Allen, Mr. F. W. Drosten, Dr. H. M. Stark- loff and Dr. Hugo Summa were elected to active member- ship. Two persons were proposed for active membership. Eeports of Officers for the Year 1903, SUBMITTED JANUARY 4, 1904. The First Vice-President, Dr. D. S. H. Smith, addressed the Academy as follows : — In the absence of the President, it becomes my duty to lay before you a summary of the doings of the Academy of Science for the year 1903. Sixteen meetings were held in 1903, with average attendance of 25. Fifteen meetings were held in 1902, with average attendance of 21. Total attendance in 1903 406 Total attendance in 1902 314 Increase for 1903 92 In 1903 the unusual attendance of 50 at the second meeting in May was due to the announcement of Dr. Barck's account of his crossing of the Grand Canon of the Colorado. There has been a noticeable increase in attendance at the meetings since the removal of the Academy to its new home, the largest number (40) at the first December meeting, when Dr. Alt gave us his paper on Cataract. Membership December 31, 1903 292 Elections for the year 23 Losses " " " 24 By death 4 By resignations ^0 ■ • • Net loss for the year 1 xlvi Trans. Acad. Sci. of St. Louis. The active members are classified as follows. — Patrons 3 Resident members 221 Non-resident members 68 Total 292 No corresponding members have been elected for some years past. Nine papers were published in 1903, eight by resident members and one by a non-resident member. Ten papers were published in 1902, seven of them by non-resident members. Of the papers published in 1903, two were on mathematical subjects, one was on a chemical subject, three were on botanical subjects, one was on a zoological subject, one was on a paleontological subject, and one on a philosophical subject. The reports of the Treasurer and of the Librarian have already been submitted to you. As matter for special consideration this evening, I beg leave to invite your attention to the financial needs of the Academy. In the spring of 1903 this house and lot were conveyed to the Academy by Mrs. William McMillan and her son, Mr. William Northrop McMillan. It was the free gift of a home for the Academy, untrammeled by any condi- tions. The generous lady and her son had every confidence that the mem- bers of the organization would care for the property with a wise economy. Whatever limitations were placed on the ownership were placed by the Academy itself. As soon as the conveyance was legally completed by the proper deed, Mr. Eliot, the President of the Academy, announced to the Council that he would give $5,000.00 to be expended in necessary repairs and rehabilita- tion and furnishing of the house. Mr. Eliot's modesty has made him unwilling that anything should be said about this generous gift, but the necessities of this sketch and justice to the Academy compel me to refer to it. We are unwilling to accept so handsome a donation without being given an opportunity to express our grateful appreciation of it. Imme- diately upon Mr. Eliot's announcement, the Council appointed a committee, of which Mr. Eliot was chairman, for the disbursement of the $5,000.00 in accordance with the terms of the gift. This has now been accomplished, and proper vouchers showing the various items of expenditure have been rendered to the Council, and placed by the Council in the hands of the Treasurer. In moving to these more ambitious quarters we necessarily increase our expenses largely. The Assistant to the Librarian and the Janitor together cost us over $1,000.00 a year. Then there are the bills for lighting and heating the house and the expense of our annual publication, along with a multitude of small disbursements which amount to a considerable sum in the aggregate. The annual dues of members, the interest upon a sum of $6,500.00, and rentals to societies of a scientific character, are our only sources of revenue. What these rentals shall be we cannot determine. Miss Phillips, who occupied the building as a school until its acquisition by the Academy, paid an annual rental of about $1,000.00. Record. xlvii In frequent discussions and comparisons of ideas by members of the Council for several years past, there has been a unanimity of opinion that if the Academy ever became possessed of a home, it would be necessary to obtain an endowment fund for its support, and that that fund should not be less than $50,000.00. I am here to-night to submit a plan for securing this amount of money. The plan, if approved by you, will be carried out in its details by the Council. 1st. The Council shall appoint three members to act as an Endowment Fund Committee. This Committee shall receive and account for all dona- tions and subscriptions to the Endowment Fund, and shall invest the same in securities to be approved by the Council. 2d. Thirty members of the Academy are to be appointed as Chairmen of Soliciting Committees. Each Chairman may select five (5) Committeemen to complete his Committee. These selections need not of necessity be mem- bers of the Academy. It shall be the task of each Committee to collect $1,000.00. 3d. When $30,000.00 shall have been collected and placed in the hands of the Endowment Fund Committee, a member of the Academy will raise $10,000.00. While these are the main and definite features of the plan, it does not stop here. I may take it for granted that every member of the Academy wishes it well and is willing to do something to assist it in promoting its aims and the purposes for which it was organized. Let each member who is not selected to serve on a Soliciting Committee consider himself a com- mittee of one to raise $50.00. It is difficult for me to believe that we have in our membership anyone who has not ten friends and acquaintances who would contribute $5.00 apiece to the support of an institution with such noble and unselfish aims as this Academy. Our membership should be increased to 500. Every member who brings in a new member is practically contributing $100.00 to the Academy — for the annual dues of $6.00 are equivalent to 6 per cent per annum on $100.00. Such, gentlemen, is the plan which I submit for your consideration. This or some better scheme must be adopted without delay, for the need of money is urgent. We have had to borrow $1,750.00, and in sixty days this loan must be met. This Endowment Fund comes home to every member of the Academy as a personal matter, and I urge most earnestly upon every man to throw apathy and indifference to one side and to do his share towards securing the fund for this institution. The Treasurer reported as follows : — Balance from 1902 '. $ 358 09 Gift of Henry W.Eliot 5,000 00 Capital released 3,000 00 Interest on invested money 372 50 Rent from Academy building v 405 00 Borrowed on note 1,750 00 Membership dues 1,552 10 $12,437 69 xlviii Trans. Acad. Sci. of St. Louis. Expenditures. Rent $ 49135 Publication of Transactions 897 01 Mailing Transactions and library expense, above sales of Transactions 586 66 Sundry expenses 533 27 Payment, account Yandell collection 295 00 Capital reinvested, and premium 3,023 50 Improvements to property 5,929 47 Insurance 118 00 Balance to 1904 563 43 $12,437 69 Invested Fund. Invested on security $6,500 00 Less note covered by securities 1,750 00 Net invested fund $4,750 00 The Librarian reported that during the year exchanges had been received to the number of 402 vohimes and 646 pam- phlets, an increase of 54 numbers as compared with 1902 ; that during the year the Transactions of the Academy were distributed to 575 societies or institutions, an increase of 6 as compared with the preceding year ; and that the expense of his office for 1903 had amounted to $121.49, against which was to be credited $27.97 received from the sale of publi- cations. Transactions of The Academy of Science of St. Louis. VOL. XIII. No. 1. REVISION OF THE BLASTOIDEAE, WITH A PRO- POSED NEW CLASSIFICATION, AND DESCRIP- TION OF NEW SPECIES. G. HAMBACH. Issued November 4, 1903. REVISION OF THE BLASTOIDEAE, WITH A PRO- POSED NEW CLASSIFICATION, AND DESCRIP- TION OF NEW SPECIES.* G. Hambach. 7. 9. 12, U. 34. 47. 47. 49. 51. 53. 55. 55. 59. EKRATA. 1. 5 read for lumen is '' lumina are." " 18 '' 32 " 20 "28 "22 a (( u SI (< u IC ii oval '-oral." Fig. 5 "Figs. 8, 10 and 11." Plate II flg. 2, 3, 5 " Plate II Fig. 3." Maccoy " M'Coy." Codastus " Codaster." footnote read for ralated " related." 1. 10 read for impossible " impossible." i. 13 & 15 read for cauedayi " cassedayi." " 22 read for ambulacria "ambulacra." "18 " " plicable "plicated." "35 " " prominent "promising." " 18 omit comma Explanation to PI. II. No. 5 add " enlarged four times." " " " " 11 " " in a Codaster." " " PI. IV. " 6 read for pyramidalis "bipyramidalis " greater degree of certainty than has been the case hereto- * Presented by title to The Academy of Science of St. Louis, June 3, 1901. t So is, for example, the figure of Granatocrimis melonoides ou PI. IX., Vol. V. of the Illinois Geological Survey absolutely a false representation of this species although it was drawn by the eminent palaeontologist, Meek. (1) REVISION OF THE BLASTOIDEAE, WITH A PRO- POSED NEW CLASSIFICATION, AND DESCRIP- TION OF NEW SPECIES.* G. Hambach. Our knowledge of the morphology of the Blastoideae has made such progress during the last two decades that a revision is highly desirable ; first, because all late publications on this subject, even the newest text-books on palaeontology, repeat old and erroneous conceptions which are, to a great extent, accompanied by incorrect illustrations,! and secondly, because of the inadequacy of the present classification, which is almost an arbitrary one, not based on permanent anatomical differ- ences, nor ontogenetic peculiarities. New material which I have collected during this period, and also that which has kindly been intrusted to me for comparison with my own, of which I may mention the whole collection of Blastoideae belonging to the Smithsonian Institution, numbering 1038 specimens, also a very valuable collection of Mr. F. A. Sampson, corroborate the suppositions expressed in my first paper, on " The Anatomy of the Blastoideae," and add new facts to those alreadv known. Blastoideae are known from the following countries be- sides America : England, Belgium, Germany, Spain, France, Russia and Australia. The main bulk of the material belongs to America, however, and especially to the family Pentremidae. In no other family do we find such abun- dant and such well preserved material as we do in this family; which fact allows us to form conclusions with a greater degree of certaint}^ thau has been the case hereto- * Presented by title to The Academy of Science of St. Louis, June 3, 1901. t So is, for example, the figure of Granatocrinus melonoides ou PI. IX., Vol. V. of the Illinois Geological Survey absolutely a false representation of this species although it was drawn by the eminent palaeontologist, Meek. (1) 2 Trans. Acad. Sci. of St. Louis. fore, because sucli families as Codasteridae , Olivanidae, etc. are known to occur only in such limited quantity and in such a poor state of preservation that conclusions regarding their internal structure will stand no comparison with that of the Pentremidae and leave a large and open field for future investigation. The present revision and the anatomical descriptions herein given are based mainly on Pentremites sulcatus, florealis and conoideus, not because they are more abundantly represented than any other species (for Pentremites godoni occurs in great numbers in Pulaski Co., Kentucky, as well as at Hunts- ville, Alabama), but the preservation of Pentremites sulcatus is so excellent that we often find the most delicate and frao-ile organs preserved, especially in those specimens which were imbedded in a kind of clayey substance. I think it is not unreasonable to suppose that similar conditions in structure must have existed in other species belonging to this famil3^ Therefore, if not otherwise stated, all descriptions and illustrations are based on Pentremites sidcatus, florealis and conoideus tov the following reasons : — 1st. These species are found in the most perfect state of preservation . 2nd. They are among the largest species so far discovered. 3rd. They are among the most abundant species to be found here. I take this opportunity to express my sincere thanks to the following scientific friends for the generous and ready way in which they have facilitated my undertaking by the loan of valuable specimens: Prof. W. H. Barris, of Davenport, Iowa; Mr. R. A. Blair, of Sedalia, Mo.; Dr. J. H. Britts, of Clinton, Mo. ; Prof. G. C. Broadhead, of Columbia, Mo. ; Mr. G. K. Greene, of New Albany, Ind. ; Mr. Edwin G. Kirk, of Burlington, Iowa; Dr. Joshua Liudahl, of Springfield, 111. ; Mr. F. A. Sampson, of Sedalia, Mo. ; Mr. C. Schuchert, of the Smithsonian Institution, Washington, D. C. ; Prof. A. G. Wetherby, of Cincinnati, Ohio; Dr. W. P. Jenney, and Mess. J. and H. Hurter, of St. Louis, Mo. It is a well-known fact that all principal parts in the con- Hambach — Revision of the Blastoideae. 3 struction of Echinodermata are arranged in multiples of five around a central axis. However, deviations from the preva- lent rule occur more frequently in this class of the animal kingdom than elsewhere. Such abnormal developments have often been the cause of redescribing well-known forms as new species, especially among the Crinoideae.* For the purpose of illustrating the tendency of abnormal develop- ments I will give a few examples, which, however, I could have multiplied if time and space would permit. Similar de- formities have been observed and described by others. f In Fig. 13 and 14, Plate III., we have a specimen of Pentremites Jlorealis, with only four fork pieces and four ambulacra. In Fig. 8 and 9, same plate, Pentremites pyriformis has four ambulacra but five fork pieces, of which the fifth is not fully developed. Fig. 15 and 16, same plate, Pentremites pyriformis^ show six fork pieces but only four ambulacra are fully developed. Fig. 11 and 12, same plate, Pentremi- tes sulcatus, show five fork pieces, one of which is a longitudinal square without any sinus, and consequently no ambulacrum has been developed. In Fig. 10, same plate, Pentretnites sulcatus, we have one ambulacrum developed only to one-half the length of the others. Fia;. 6 and 7, same plate, Pentremites sulcatus, show an extra longitudinal piece inserted between two fork pieces. Fig. 18, same plate, Pen- tremites Jlorealis, has only four fork pieces but five am- bulacra, so that two ambulacra are inserted into one sinus, causing the two opposite halves of the ambulacrum to form a prominent ridge. In Fig. 17, same plate, Pentremites * See Bulletins of the Illinois State Museum of Natural History, by S. A. Miller and W. F. E. Gurley, Nos. 1-12, t Robert Etberidge, Jun., and P. Herbert Carpenter. Catalogue of the Blasloidea, Hermann von Meyer. Abweichung von der Fiinfzahl bei Echinideen. Prof. Georg Boehm. Ueber eine Anomalie im Kelche von Millericrinus mespiliformis . Zeitschrift der deutschen geologischen Gesellschafl. Band XLIII., Hefts, p. 741. H. W. Mackintosh. On a Malformed Corona of Echinus esculentus. Proceedings of the Royal Irish Academy. Vol. II., Ser. II , 1875, p. 206. Dr Philippi. Beschreibung zvveier missgebildeter See-Igel. Wiegmann's Archiv fiir Naturgeschichte. Band I., 1837, p. 241. 4 Trans. Acad. Sci. of St. Louis. bipyramidalis, Hall (Saccoblastus), we have five fork pieces but six ambulacra, of which two occupy one sinus. I think these examples are sufficient to justify the above statement. Fig. 1. Fig. 2. The body of a Pentremite is constructed of twenty pieces, (at least in the embryonic state), arranged in two circles in such a way that we have a most perfect dicyclical* body with a primary center of a pentagonal outline for each circle. Each piece of the second circle rests upon two of the first circle. These two circles may be designated as an ambulacral and an interambulacral, of which the former grows down- ward in its development, whereas the latter grows upward. Fig. 1 and 2. THE BASAL PIECES. The base or central part of the interambulacral circle (also called pelvis )t varies very much in size and in general form, from a flat disc to a more or less funnel-shaped piece. It is perforated by a fine channel in the center, and the articula- tion surface for the column is either round or triangular ac- cording to the species and consists, at least in the embryonic state, of five equal pieces, though in the course of development two of the five sutures become obliterated, so that it gener- ♦ The word dicyclical is not used in the same sense as in Crinoideae. t H. B. Geinitz. Grundriss der Versteineruugskunde, p. 558. Hamhach — Revision of the Blaxtoideae. 5 ally appears as if the base were constructed of only three pieces, of which two are equal and pentagonal and the other rhombic in form, though specimens are fre- quently found in which no anchylosis took place so that all five sutures remain open, an occurrence which is also observed in Crinoids, for example in Agassizocrmus where the base generally appears as one solid piece, though fig. 3. specimens are not uncommon where one, two or all sutures remained open and did not anchylose. Fig. 3. FORK PIECES. The fork pieces are of an oblong form, more or less wide, according to species, and the incision or sinus is also of vari- able depth and width, making them resemble a two-pronged fork, from which the name originated, or a V shape. Their solid base portion is more or less thick and has, in cross sec- tion, a more or less triangular or semi-lunar form, or, as in other genera of the family Pentremidae, it is turned in and upward so that the base portion becomes inverted and exter- nally invisible. The incision or sinus is wider externally than internally, i. e., the inner lateral margin of the sinus slopes toward the interior, causing the internal opening of the sinus to be narrower than the external. The upper points of the prongs are cut obliquely laterally making them rest against the upper and lateral spurs of the deltoid expansion. In other species they run out into sharp and acute points as in Pentremites reinwardtU, Troost. In still others they are of uniform thickness with an upper oblique and smooth margin. THE DELTOID PIECES. The deltoid pieces of the typical species, as Pentremites sidcatus, pyriformisy fiorealis^ etc., when fully developed, can be divided into two parts, which, however, are not separated from each other by sutures. First a main or base portion, the most important part of the whole calyx, 6 Trans. Acad. Sci. of St. Louis. which is never wanting ; and secondly a laterally expanded blade, not present in the young but becoming gradually more and more dev^eloped as they grow older; see Plate VI. The first or base portion, in the typical species above mentioned, has a shape resembling very much a six- sided prism; see Plate II., Fig. 9. The surface toward the center of the calyx has a semi-lunar groove which forms with the adjoining piece the central opening or mouth, and, as this basal part is placed in a slightly oblique position, it causes the external opening to be a little smaller than the internal one. The opposite side of this semi-lunar cavity is prolonged into a narrow blade, except for the posterior one, where the septum is divided into two blades for the outlet of the anus. The lower part is divided lengthwise into two blades, running down and outwards with a plicated outer margin, — Plate II., Fig. 9, — for the support of the plications of the hydrospiric tubes, whereas the upper part of this blade forms a sharp crest, and the outer one a triangular in- cision, during the juvenile state, for the reception of the upper points of the fork pieces which rest in this triangular incision. At the base of these lamellar blades we find a semi- lunar groove which forms with a similar one on the base of the lancet piece the genital opening, except in species where the deltoid pieces are perforated, as in G. norwoodi and similar forms. The outer or upper surface of the base portion is either rounded or sharp pointed, whereas the lower surface, which expands toward the center of the calyx, is grooved transversely so as to form a circular groove around the mouth on the interior side of the calyx for the reception of the central ring of a water vascular system. This central water ring underlies the basal part of the deltoids and does not penetrate the calcareous shell, sending off five straight branches, one for each ambulacrum, running between the hy- drospiric tubes and the lancet piece, but not through the latter; see Plate II., Fig. 8. The outer half of the prism is transversely perforated by a fine channel, forming in connection with the other parts a pentagonal ring for the reception of the nervous center. Hamhacli — Revision of the Blastoideae. 7 giving off five branches, one for each ambulacrum, and run- ning through the center of the lancet piece. From the foregoing we see that the whole center of this system as well as the branches run through the midst of a calcareous substance, and their lumen is so small that they are frequently found to be obliterated. It is therefore hardly possible that these fine channels could have served for anything else than the reception of the nervous system, giv- ing us an analogous arrangement to what we find in our living Asteroidea ; see Fig. 4. Fig. 4. The second part, ^. e., the lateral expansion in the typical species above mentioned, is not un- like the Greek letter delta, from which the name originated, or resembles an arrow head with a very acute surface up- wards and an obtuse one downwards, having on each side a spur, running obliquely down and inwards, so as to be ex- ternally concealed by the upper points of the fork pieces. The upper acute surface differs very much in the different species and often in one and the same species, being subject to great variations, so that we find it often very acute and bent iuwardl}^ or very broad and bent outwardly. In other species, where the calyx consists of only a very thin shell, as for example in C meJo, the laminar blade widens immediately so that the whole piece is placed more horizon- tally on the summit of the calyx, and hardly any division between base portion and lateral expansion takes place, ex- cept the incision for the construction of the genital openings, and this same condition can be observed throughout the whole juvenile state of the body. In other species again, as for instance in C. fsayi, the lateral expansion assumes such an enormous size that it occupies almost three fourths or four fifths of the entire calyx, and in others, as in G. norwoodi, the whole deltoid piece has a triangular form and the genital opening pierces directly through the center of this piece, but with only one external opening, bifurcating within the shell, 8 Trans. Acad. Sci. of St. Louu. and forming two openings on the interior side. In silicious casts of this species these little openings are often found to be filled with silicious matter, and will naturally show on the summit of such casts a little bifurcating tube, as illustrated b}'^ Meek and Worthen,* which undoubtedly gave origin to the supposition that two of the hydrospiric tubes were united near the summit into one, as figured by Billings t and Lud- wig.t By a little reflection, however, it is easily compre- hended that these bifurcating tubes have nothing to do with the hydrospiric tubes and that it is only silicious matter filling out these little channels, for they are never found on casts of other species than those which have the deltoid pieces pierced in the described manner. From the foregoing it 'will be seen that we have nearly every degree of development in form and size represented, and this gradual development of the lateral expansion as we find it in the typical specimens of Pentremites sidcatus, pyri- formis, Jiorealis and others is a sufiicient and good reason to exclude the newly rehabilitated genus Pentremitidia of D'Orbigny, whose principal distinguishing character consists in the absence of the lateral expansion, as plainly stated by him: " Calice compost de deux series de cinq pieux superpos^es."§ His types for this genus were Pentremites schrdtzii and ^9a«7/e^/ee. But the absence or non-develop- ment of the lateral expansion, as it is often found in the typical species, and alwaj^s in the young specimen of the same species, does not justify the creation of a new genus, as was well remarked bv Dr. Koemer: " Gewiss verdient es aber keine Nachahmung." |1 Otherwise the young specimens of Pentremites sidcatus, jjyriformis, etc., would belong to the genus Pentremitidia during their juvenile state, and after- wards when fully developed to Pentremites ; see Plate VI., Fig. * Illinois Geological Survey, Vol. V., plate IX., Fig. 2 c, p. 473. t Palaeozoic Fossils, Vol. II., Part I., Fig. 60, p. 102. % Morphologische Studien an Echinoderraen, Band I., p. 289, Plate 27, Fig. 36 and 37. § M. A. D'Orbigny. Prodrome de Pal^ontologie, Vol. I., p. 102. II Roemer. Monographie der fossilien Crinoidenfamilie der Blastoideen, p. 49; and Wiegmann'a Archivfiir Naturgesctiichte, Jahrg. XVII., B. 1. Hamhach — Revision of the Blastoideae. & 1—3, because Pentremites schultzii and paillettei are as typi- cal PentreTYiites as sulcatus, pyriformis and others, — that is to say, their calyx consists of the same number of pieces with the same relationship of them to each other as in the true Pentremites. Their genital openings are constructed by the junction of deltoid and lancet pieces precisely as we find in the typical species above mentioned. Other differences in the character of this genus as lately revised are of no generic value as they are due to the variability in size and shape of basal, fork and lancet pieces, and are only of specific impor- tance. That the general conception of the deltoid pieces is not a correct one is sufficiently shown by the descriptions given by various authors. They were called interscapular plates, second radials, interradials, orals, etc. The name inter- radial w^as first used by DeKoninck at a time when the Blas- toideae were regarded as a sub-order of Crinoideae. In 1879 they were regarded as homologous to the oval plates of Crinoids by Wachsmuth, which statement he corrected three or four years later when he called them true interradials.* He says : — ♦♦ The term ' oral' for the deltoid pieces was proposed by Wachsmuth and Springer in Part I. of their Eevision, and afterwards adopted by Prof. v. Zittel and by Messrs. Etheridge and Carpenter. " Since the publication of the present article, I became fully convinced that the so-called deltoid pieces are not oral plates, but true interradials, and that, as such, they form a part of the abactinal system. If the deltoids were actinal plates, and this they should be if they were orals, the actinal regions in Elaeacrimcs ohovatus would extend to over three fourths of the entire body — a proportion almost equal to that of Echini. On the contrary, in the allied Granatocrinus norwoodi, with small deltoids, and in Hetero- schisma gracile, the actinal system excluding the ambulacra, would be limited to a small area around the oral pole, and occupy scarcely more than a twentieth part. The different * Proceedings Davenport Academy of Natural Sciences, Vol. IV., p. 76. 10 Trans. Acad. Sci. of St. Louis. proportions of the actinal and abactinal regions among Ecliinoderms were looked upon by Prof. L. Agassiz as determining the different outlines of the various ' orders of this class,' and he has ranked their orders according to the greater preponderance of the one or the other of the two re- gions. In the Neocrinoidea, the oral and aboral regions are proportioned almost equally, and this is the case not only in the adult, but is to be observed already in the Pentacrinoid- larva. In the Palaeocrinoidea, the abactinal regions, as a rule, are considerably contracted, and in the lower organ- ized Blastoids they are reduced still more. Plates of such enormous dimensions as are found occasionally among the deltoids, cannot possibly form a part of the actinal system in so low a group as the Blastoids, and hence cannot be orals. That they are true interradials is proved by the relative position which they occupy to the interradials of the Palaeocrinoideae. Like those plates, they rest upon the upper sloping sides of the radials, and extend, whether consisting of a single plate as in the Cyathocrinidae, or of a series of pieces as in Actinocrinidae and Rhodocrinidae, into the ventral side, to a series of plates, which were desig- nated by W. and Sp. as central pieces and proximals." The first question which presents itself is, what is meant by interradial? The Avord undoubtedly means something between the rays of a circle. We therefore have to assume a primary circle of rays or plates between which the secondary parts can be placed, as, for example, in Crinoids those plates which are placed between the regular radial plates. The second question would be, what is the function of the inter- radials? Referring to Crinoids again we find that their function is to fill out space in order to increase the circumfer- ence of the body. They are not essential to the construction of the body or calyx as is weJl illustrated in a number of Crinoids which have no interradials. Besides, their number is variable. Therefore they may be regarded as supernu- merary pieces whose only function is to enlarge the body. In no case do they enter into the construction of the various openings unless we regard the anals as interradials, which I Hamhach — Revision of the Blastoideae. 11 think has not been done so far. But in the case under con- sideration, that is in Pentremites and allied forms, the body is dicyclical, which it could not be if the deltoids were inter- radial. In that case the apex of the deltoid, i. e., the lateral expansion, would be the base and not the apex and hence would have been developed first, which is not the case as I have shown above, — Plate VI., Fig. 1-3. However large or small the lateral expansion of the deltoid may be, the fact is that the base part of the deltoid is developed first and is the prin- cipal part of the body. It is not separated from the laterally expanded part by any suture. All principal openings are constructed by this part, or together with the lancet piece, or the openings pierce the deltoid piece. They do not rest upon the upper sloping sides of the fork pieces or radials but the fork pieces lean against the deltoid piece whether the laterally expanded part is developed or not. Therefore it is hardly possible to assume that such imi)ortant pieces as the deltoids should have been developed later than less important ones, which is sufficiently demonstrated by the foregoing pages. For these reasons they cannot be interradials. LANCET PIECES. The lancet piece varies very much according to the dimen- sions of the fork piece sinus, i. e., according to the species, from a regular lancet-shaped piece to a mere linear lamella and fits in the sinus of the fork piece in such a way as to fill the incision with the exception of a narrow fissure on each side. They are in the typical forms, as Pentreinites sulcatus, P. florealis, P. pyriformis, etc., as substantial as the other parts of the calyx and form an integral part of the calyx of the same value as the other pieces constructing it, and are in large specimens of P. sulcatus fully one eighth inch thick. They are generally of uniform width with a smooth anterior surface, whereas the posterior or inner surface is more or less concave and has a semi-lunar groove throughout its length for the reception of some duct or vessel. On the upper or base portion is a little beak-like process of a triangular form 12 Trans. Acad. Set. of St. Louis. by which it connects with the annuliis centralis or central ring of the deltoid pieces, resting thereby on two deltoid pieces ; see Fig. 2. The center of these pieces is perforated by a fine channel in its entire length, bifurcating at its base to connect with the transverse channel of the deltoid base-portion, form- ing thus a pentagonal ring around the central opening. The size of these channels is such that it seems hardly possible that they could serve for the water vascular system. It seems more probable that they contained the nervous system, giving a similar arrangement to what we find in higher forms like Asteroids; see Fig. 4. The little beak-like process where the lancet piece connects with the deltoid is laterally grooved to form with the corre- sponding groove of the deltoid, the ovarian or genital aperture except in species where the deltoid piece is perforated, as in G. noriooodi. PORAL PIECES. The triangular groove which is formed by the outer margin of the lancet piece and the inner margin of the fork piece sinus is filled with little pieces corresponding to this groove, which were called most appropriately poral pieces by Dr. Koemer. This name has been changed to side plates b}^ R. Etheridge, Jr., and P. H. Carpenter,* which term is also adopted by C. R. Eastman. t The reason given for the change of this name is not a logical one and shows that the nature of the pieces is not thoroughly comprehended. Are perhaps the poral open- ings not constructed by the poral pieces? Does not the name poral piece indicate the nature better than the new name? What benefit is to be derived from the new name? They are of a triangular form, corresponding to the groove which they occupy. They are inserted edgewise so that the thickness of these pieces forms their outer exposed surface; see Fig. 5. These pieces have on both sides of their outer lateral margin a little semi-lunar groove, which with the adjoining one forms the pore-opening, and, in no case, are these pieces ♦ Catalogue of the Blastoidea. t Text Book of Palaeontology. Hambach — Revision of the Blastoideae. 13 pierced by marginal pores, as stated by C. E. Eastman.* They are supernumerary pieces and form a kind of accessory part to the construction of the ambuhicrum. It is self-evident that there are differences in the size and shape of these pieces, depending upon the size and shape of the lancet piece as well as upon the fork piece sinus; but all have undoubtedly the same physiological function, so that such dif- ference in the size and shape can be of specific value only. THE AMBULACEAL INTEGUMENT. The outer surface of the ambulacrum, i. e., the lancet and poral pieces, is covered by an organic and elastic integument which I formerly designated as the zigzag plicated integu- ment.! It gives to the ambulacra! surface a striated appear- ance which is not, as Etheridge and Carpenter state, " merely a delicate surface ornamentation." } This integument has a different appearance in different species, and varies very much in its zigzag shape and in the distance of its windings. In most cases it is so eroded that it is almost impossible to make out its true appearance. It may be regarded as a ribbon placed obliquely on edge and running in a zigzag form forward and back so that the lower opposite edges of the returning ribbon unite and form the bottom of a little groove, while the other or upper edges form a little ridge ; see Plate II., Fig. 2 and 5. These ridges show an open surface in species like Pentremites pyriformis and Jlorealis, whereas in Pentremites sulcatus and others they are firmly united to the margin of the poral pieces. There is also a great variety in the distance between two ridges. In Pentremites pyriformis we may count nine to ^ inch, whereas in Pentremites sulcatus we have eleven to ^ inch, etc. It begins with an acute point at the center of the del- toids, surrounding two ovarian or genital openings, and does this in typical species like Pentremites sulcatus, Jlorealis , pyri- formis, etc., in such a way as to make the two openings appear as one, externally. In some species, as C . sayi, the ♦ Text Book of Palaeontology, p. 192. t Transactions St. Louis Academy of Science, Vol. IV., p. 150. t Catalogue of the Blastoidea, p. 59. 14 Trans. Acad. Sci. of St. Louis. integument does not run close to the margin of the sinus in the vicinity of the ovarian or genital openings, making them appear as little slits instead of round openings. It runs in the shape of a letter J^ inverted with the two arms extend- ing out and downward to the apex of the ambulacrum. Each arm covers one-half of the ambulacral surface, forming with the opposite one a longitudinal groove in the center (the so-called foot groove ) . This foot groove and the little transverse grooves at each side of it are covered with little scales, so that, in specimens very well' preserved, the ambulacrum does not '^^^- ^- show any transversely striated surface at all, but appears rather smooth or granulated with a little crest in the center. The whole covering is of a uniform character, except on the summit, where the scales surrounding the ova- rian or genital apertures (at least in the typical species) are fully ten times as long and placed erect on the underlying membrane, — see Fig. 5 and Plate II., Fig. 2, 3, 5, — forming in this way a part of the cone-shaped body which has been observed on the summit of many species. Their physiologi- cal function is still unknown, but probably it was to protect the finer inner ovarian tubes. Besides the scales we find on the posterior side above the anal opening, on very well preserved specimens, a small proboscis about one fourth of an inch in length, constructed of small hexago- nal pieces, as shown in Fig. 6 and 7. To my knowledge it is the first time that such a body has been observed on a Blastoid. I found this appendix on JPentre?nites conoideus and have now four speci- mens of it showing this, so far unknown, organ. All four specimens are in an excellent state of pres- ervation and show also the pinnulae preserved. I am inclined to believe hiG. 7. |.jj^^ similar organs existed Fig. (;. Hambach — Revision of the Blastoideae. 15 in all tj^pical species. At the outer margin of the ambulac- rum, where the outward running ribbon returns to the center of the field, the ribbon is twisted over so that the fold fa'cili- tating the return is the under surface of the ribbon and becomes the articuhition surf ace of thepinnulae; see Plate II., Fig. 5. These pinnulae are little filaments of various lengths extending in some species as much beyond the summit as the entire length of the calyx, or even more. They consist of a single row of calcareous particles, wedge-shaped in form and about as broad as long. As evidence to support the foregoing assertion, i. e., the flexibility and organic nature of the ambulacral integument, I give in Figures 1-7, Plate I., representations of some pathologic specimens selected from a large amount of mate- rial collected for this purpose. I have over fifty such patho- logic specimens, showing various kinds of injuries and the subsequent restoration of the injured parts, which would have been impossible had the integument been inorganic mat- ter only, as supposed by Carpenter. All specimens figured, belong to the species JPentremites sulcatus. Plate I., Fig. 6, shows an injury near the middle of the ambulacrum; Fig. 5 a similar injury on one side of the field and on the other side the loss of half the poral pieces and the subsequent restora- tion of the integument. Fig. 1 and 2 show the flexion of the transverse ridges into a sigmoid form and the partly compressed shape of the genital openings ; Fig. 7 and Plate II., Fig. 7 show the unevenness of the integument at the outer margin near the sinus. The acute points at the beginning of the ambulacral in- tegument are the only covering for the central orifice. (The surrounding genital openings are entirely out of the ques- tion.) The different descriptions and illustrations given (which all differ from each other) are erroneous representa- tions due to mistaking foreign matter for covering plates, as already expressed in my first paper.* Nothing is more natural than that some of the little scales or particles of broken pinnulae should drop into some of the summit openings and Transactions of The St. Louis Academy of Science, Vol. IV., p. 150. 16 Trans. Acad. Set. of St. Louis. remain there, which also accounts for the irregularity of these coverings as described and figured by the different authors. It is strange that every one adheres to the old idea of Shumard, and that no one has taken the pains to examine the matter more carefully in order to convince himself of the true nature of it. This irregular arrangement of the pieces covering the summit openings, as described by Eastman,* is evidence for the contradiction of his statement, because it is hard to suppose that specimens belonging to one and the same species should not have a uniform arrangement in the covering plates of their openings if such a covering existed. It is true that Wachsmuth admits, after seeing Shumard' s type specimen of Pentremites conoideus that the summit openings are not closed in the manner described by Shumard but he still believes that thev are closed. It stands to reason and is only logical to suppose that, if nature provided an opening it should remain open or that the covering is a flexible one and not formed by additional plates inserted into the openings as intimated by all authors Avho adopted the first statement of Shumard. No one explains or gives any reason why the opening should be closed. Every one disregards the fact that all casts of the interior of a calyx exhibit on the summit a cast of the summit opening, which could not be possible if the openings had been closed by ad- ditional pieces. This fact has not been observed on speci- mens of Olivanites or others where the center of the summit is closed. THE WATER VASCULAR SYSTEM. On the under side of the lancet piece and completely filling the semi-lunar groove we find a tubular vessel con- necting with a circular ring underlying the base of the deltoid and surrounding the central orifice. The thickness of this vascular rins^ and its branches varies according: to the species. The diameter of this vessel is about 1-20 of an inch in a large specimen of Pentremites sulcatus. ♦ Text Book of Palaeontology, Vol. I., p. 197. Hambach — Revision of the Blastoideae. 17 It is not often found preserved, at least not in an open condition, but oftener in a collapsed condition. In this condition it presents the so-called underlancet plate of late authors.* I can prove the existence of this vessel by a number of cross sections of an ambulacrum of which Fig. 8 and Plate II. are a correct representation. Lancet piece and poral pieces are well preserved, also the vascular duct a, which in this specimen is filled with calcspar which could enter only in a liquid state. The triangular space b at each side of the vessel is filled by a kind of clayey substance, which must also have been in a very plastic or liquid form when entering the cavity. Underneath we have the hydrospiric plications c. Had the vessel a not existed the substance in h would have undoubtedly filled the whole space if it were the first to enter the calyx. On the other hand if the liquid calcspar had entered first it would have spread over the whole space if no vessel had existed. The walls of these vessels must have been very thin, which accounts for their easy destruction and absence in most cases. In an empty state they would naturally have collapsed, but nevertheless could easily be distinguished from the underlying upper blade of the hydrospiric tube, in not showing a suture line in the center, which would be the case if the vessel had been destroyed and the upper blade of the hydrospiric tube were exposed to view. Fig. 8. a. Water vascular duct. b. Space at each side of duct filled with clayey sub- stance. c. Lobes of the hydrospiric tube. d. Upper blade of the hy- drospiric tube. e. Nervous channel. f. Tentacle. g. Ovarian tubes, h. Lancet plate, i. Poral pieces. THE HYDR08PIRES OR RESPIRATORY ORGAN. The hydrospires in the typical species like PentremUes sul- catus, florealis, pyriformis, etc., form ten isolated plicated * Eastman. Text Book of Palaeontology, VoL I., p. 19L 18 Trans. Acad. Sci. of St. Louis. membranous tubes and not bundles of tubes as stated by various authors, and accompanied by incorrect illustrations. They are located beneath the water duct and run parallel to it from near the summit of the calyx to the apex of the ambulacrum. The plications rest in little grooves of the expanded lower deltoid portion, and are not united with the adjoining one to form five bundles as described and illustrated by Billings* and Ludwig.f These plicated tubes or hydro- spires are of a peculiar construction. Each tube may be regarded as a somewhat collapsed cylinder of which the upper blade, ^. e., the one nearest to the water duct, is smooth in its whole length, whereas the underlying blade is folded into a number of plications of no regularity. They vary in number Fig. 9. Transverse sections of ambulacral fields, to show abnormal developments of the hydrospiric sacs: A, of Pentremitea pyri- formis; B, P. Jlorealis; C, P. conoideiis — about 20 times magnified and drawn with the aid of the camera lucida. a, hydrospiric sac; b, calcareous part of ambulacral field, i. e. lancet and poral pieces. in the different species and vary very often in one and the same specimen; see Fig. 9. At the outer margin where these two blades meet, that is, where the upper smooth blade connects with the lower plicated one, they run out into little thread-like filaments or tentacles, giving the compressed cylinder a fringed appearance on this side. They form the so much doubted tentacles which protrude through the poral openings and form * Palaeozoic Fossils, Vol. II., Part 1, p. 102. t H. Ludwig. Morphologische Studiea an Echinodermen, Band I., p. 289. Taf. XXVIl,, Fig. 36, 37. Hambach — Revision of the Blastoideae. 19 in their collapsed state the supplementary poral pieces of Dr. Roemer * or outer side plates of later authors. f What could be the function of these supplementary poral pieces situated as described by Dr. Roemer, within the poral opening? As I understand the term it applies to something similar to and in addition to the poral piece, that is a small piece inserted in the poral opening. According to the Doc- tor's description it served to reduce the opening, which, how- ever, is not a very plausible supposition, as the same result might have been accomplished by nature in a much simpler manner by lessening the groove in the pore piece. Therefore I deem it proper to seek for another explanation which is to be found in supposing them to be tentacles. The correctness of this supposition is easily tested, as there can be only three possible conditions : — 1st. If a supplementary poral piece existed it should be found by making a transverse sec- tion through or near the middle of a pore channel, a- j- ffj- — ^ say at the line indicated from « to & in Fig. 10. 2d. If then the supplementary poral pieces ^^^- 1^- are not preserved, we should find the poral opening vacant or filled with foreign matter. 3d. If my supposition is correct and the tentacles are pre- served, we will find them by making such a section, in either an open or collapsed condition. In a number of sections I have made I can prove the existence of the so much doubted tentacles in either condition. Fig. 1, Plate II., is a trans- verse section through a row of poral pieces of Pentremites Jlorealis, showing the preservation of the tentacles in a some what collapsed condition. Fig. 4 is a similar section of Pen- tremites ahbreviatus showing the tentacles in an open condition. I could show further evidence of their existence in pathologic specimens where mechanical injuries had been inflicted, caus- ing a hypertrophic growth of some of the tentacles into a little bundle of tubes. The plications, as already stated, vary in number and in the * Wiegmann's Archiv fur Naturgeschichte, Jahrg. XVII., Bd. I., p. 335. t Eastman. Text Book of Palaeontology, Vol. I., p. 191. 20 Trans. Acad. Sci. of St. Louis. manner of folding. They are in an end view not unlike an un- symmetrical figure 8, — see Fig. 11, — of which the upper loop is larger than the lower one. These loops, in large specimens of Pentremites sulcalus, are one fourth of an inch long. Counting five folds to each of the ten cylinders, or ten to each ambulacrum, it would give for the whole body, if stretched out, a ribbon over two feet long — an organ well adapted for respiratory function as sup- posed by Billings.* The apices of these foldings are often found to have coalesced with the calcareous base part of the fork pieces as observed in Pentremites conoideus and others, whereas the plicae of the other end rest in those plications or grooves of the deltoid expansion already described near the summit openings. The coalescing with the calcareous base portion of the fork pieces is not a peculiarity found only in certain species as indicated by Carpenter, f but it can be observed in other species, as in Pentremites Jlorealis, etc. Between the upper loops of these plications, which are kept open by resting in the little grooves near the summit, we find longitudinal tubes, protruding through the genital openings on the summit and filling them completel}^ These tubes I regard as the ovarian or genital tubes. They are found (in well preserved specimens) to be filled with little round bodies (eggs?). Fig. 6, Plate II., is a longitudinal section through the upper loop of a hydrospiric cylinder of Pentremites jlorealis, exhibiting these little round bodies at various places. The supposition that these are ovarian tubes is strengthened by the fact that the plications near the summit rest in grooves, which would be necessary to prevent any obstruction to the passage of the &^g. In Cadaster the construction of the hydrospires is quite different. Here we have from the roof of the calyx vertical lamellae one eighth to one fourth of an inch long, reaching * Billings, Loc. cit., p. 103. t Carpenter, Loc. cit. Harabach — Revision of the Blastoideae. 21 into the interior of the calyx and varying in number according to species from six to twelve or even more. These lamellae are completely surrounded by a ribbon-like membrane ; see Plate II., Fig. 11. The water is admitted to the surface of the membrane by longitudinal slits in the calcareous substance of the roof between the vertical lamellae. Whether these slits were covered or not I am unable to say on account of the insufficiency of material for study. EARLIER CLASSIFICATION. As already remarked, the present classification is largely based on external resemblances and is a very arbitrary one, lacking a good foundation of morphologic as well as onto- genetic characters, in consequence of which it becomes inade- quate. This induces me to offer anew classification based on determinative and permanent anatomical differences as well as ontogenetic peculiarities. If the Blastoideae form an inde- pendent class like the Crinoideae or Cystoideae, which I believe is now generally admitted, then in revising the pres- ent classification all names that have an ending " crinus " ought to be canceled and new and proper ones substituted for them. This was already recommended by Quenstedt in 1876.* If this had been done it would have avoided the con- fusion resulting from the retention of improper names and from referring species to genera to which they do not belong, especially when the author is doubtful about their propriety, which is always indicated by a question mark, or from substi- tuting new names for parts of the body which are not as significant as the old ones. The ontogeny of extinct families can only be studied with a large amount of material from one and the same locality, which will enable us to make comparisons between the young and adult specimens, to ascertain if all parts are keeping step in the progress of development, or if one part has developed more rapidly than the others, and in which direction this development has taken place. For the purpose of proving the arbitrary condition I will review the genus Gi^anatocrinus and for the convenience of * F.A. Quenstedt. PetrefactenkundeDeutschlands, Vierter Band., p. 719. 22 T7-ans. Acad. Sci. of St. Louis. the reader, I will recapitulate the various views of our most distinguished palaeontologists concerning this question, which will show that very little attention was given to anatomical differences, and that all specimens enumerated in this genus were placed there on merely external resemblances. If anat- omical differences had been considered, Shumard would never have proposed to put species like Granatocrinus norwoodi, curtus, gramdatiis, sayi, roemeri, cornutus, etc., into one genus* In 1861, Meek and Worthen say, in speaking about Pen- tremites cornutus and Pentremites meIo:'\ " Both of these forms differ from the typical species of the genus Pentremites in having each pair of ovarian openings distinctly separated, instead of closely united with merely a thin septum between. In this character, as well as in form, and the prolongation of the pseudo-ambulacral areas, they agree with the genus ISfucleocrinus of Conrad {=^ Elaeacrinus, Roemer), from which they differ in having the anal and oral openings dis- tinct as in the true Pentremites. Thev constitute a sub- genus of Pe7itre?nites, occupying a position between the typical forms of that genus and yucleocrinus.^' In 1862 Prof. Hall says in speaking about the genus jSTu- cleocrinus: J — " Regarding only the general form of these bodies, this genus would include several species, heretofore described under Pentremites, from the Carboniferous limestones of the Western States, viz. : Pentre^nites norwoodi, Owen and Shumard; Pentremites nielo, Owen and Shumard; Pentremites curtus, Shumard, and others ; while the Pentremites ( Olivan- ites) verneuili = Elaeacrinus verneuili, Eoemer, and Olivan- ites angidaris, Lyon, are of the age of the upper Helder- berg limestones; and the JSfucleocrinus elegans, Conrad, and at least one other species, occur in the Hamilton group. The * Roemer's Pentremites granulatus is taken as type of the gerius. — See B. F. Shumard, Transactions of The Academy of Science of St. Louis, Vol. IL,p. 375. t Proceedings of The Academy of Natural Sciences of Philadelphia, 1861, p. U2. X Fifteenth Annual Report of the Regents of the University of the State of New York, p. 145. Hambach — Revision of the Blastoideae. 23 Pentremites roemeri, Shumard, is referred to the Chemuno- group. "Looking at other characters than those of general form, the specimens before me scarcely warrant the union of all these species under the genus N^ucleocriniis or Elaeacrinus. In jSTucleocrinus elegans, and allied forms, we have three small basal plates and five short radials, which embrace the base of the pseudambulacral fields; while the interradial plates are extremely large, extending nearly the whole length of the pseudambulacral areas. The anal side is often, or usually, flattened, a little broader than the others, and is marked by a narrow lanceolate plate, which extends from the opening to the summitof the radial plates, resting upon them; thus, as it were, dividing the interradial plate, leaving a narrow portion on each side adjacent to the pseudambulacral fields. The central area at the summit, between the ovarian openings, is occupied by several small plates, which, in JVucleocrinus ele- gans, converge to the center. ' ' In the structure of the body, the typical forms of this genus differ from Pentremites m the shoYi radial plates and extremely elongated interradials, which fill nearly all the space between the pseudambulacral areas; while the elongate anal plate is a marked feature. Now when we compare Pentremites norwoodi and Pentremites melo, we have the same general form of body, with the extremely elongate, instead of the short, radial or forked plates which embrace the pseudambulacral fields ; and a small inter- radial at the summit. The ovarian apertures, as well as per- haps the central opening, sometimes preserve minute plates, which close these orifices. The form alone can scarcely be of generic importance; for, although the base of JSfucleocrinus is usually concave, I have before me a species where the base is not concave, and the three basal plates are quite prominent. The only conspicuous difference between Pentremites nor- woodi and Pent7^emites godoni and others of the latter form, is in the depressed base and greater rotundity of the former species, giving to it its similarity to Nucleocrinus. The Pen- tremites norwoodi and Pentremites melo have not the anal 24 Trans. Acad. Sci. of St. Louis. side conspicuously wider, more prominent, or flattened ; which is the character observed in all true JTudeocrini . ' ' The different arrangement of parts, also, in the tvro genera, causes a different mode of increase in the plates, and a differ- ent surface-character. "There is likewise an intermediate form represented by the Gh'aiiatocrinus of Troost (jPentremites granidatus ? of Roemer). This species is elliptical in form, with depressed base embracing in the bottom of the cavity the three small basal plates, while the radial plates reach halfway up the sides of the body. The anal side is not conspicuously different from the others, and the summit is unlike JSFucleocrinus ; while it is more nearly like Pentremites noriooodi. This species is strongly granulose or tuberculose. The Pentre- mites sayi appears to me to belong to the same tj-pe ; its base is not depressed, leaving the three basal plates protruding ; while the radial plates reach about one-third the entire length, in this respect approaching yucleocrinus . In both these species the plate on the anal side occupies the entire space between the pseudambulacral fields, presenting scarcely any important difference from the other interambulacral or interradial spaces. ' ' I would therefore suggest the separation of the species under the name oriijinallv siven bv Dr. Troost, viz., Granato- criniis.^^ In 1863 Dr. Shumard's remarks regarding thegenus Elaea- o o o crinus are as follows : * — " There is, in my opinion, good grounds for separating from the genus Pentremites those forms that have been hitherto in- eluded in the group EUiptici of Prof. Roemer, and placing them in the genus Elaeacriiius of the same author. We therefore propose now to group in the latter genus such forms as Pentremites melo, Pentremites norwoodi, P . curtus, P. granidatus, P. roemeri, P. sayi, P. cornutus, and the species we are about to describe ; also the N^ucleocrinus angidaris of Lyon. Among European species, the following may be * Transactions St. Louis Academy, Vol. II,, p. 111. Hambach — Revision of the Blastoideae. 25 grouped in this genus : Pentremites ellipticus, P. orbicularis, P. derbiensis, P. oblongus, and P. angulatus. " These form a very natural group, easily recognizable, and distinguished from the typical species of Pentremites by well marked characters. They are always of an elliptical or sub- globular shape, Thepseudo-ambulacral areas are narrow, with sides subparallel, and extend usually the entire length of the body. The basal pieces are nearly always concave, and gen- erally situated at the bottom of a deep excavation. The tubular lamellae, which in the interior reach from the ovarial apertures to the base of the pseudo-ambulacral fields, are more simple in structure, being much less convoluted, while the relative position of the ovarial apertures is different. " The typical species of the genus Elaeacrinus, viz., Elaea- crinus verneuili, long previous to the publication of Prof. Eoemer's description with figures was well known to Ameri- can and also to some European palaeontologists as Olivanites verneuili, under which name it was designated by Prof. G. Troost in his Monograph on North American Crinoidea, which valuable memoir was completed a short time previous to the death of its author, but is not yet published. According therefore to the laws of priority, Eoemer's name, Elaeacrinus, proposed in 1852, must be adopted, although it is to be re- gretted that the learned author did not adopt Troost' s generic name in preference to creating a new one. " It is possible that the genus N'ucleocrinus, proposed by Conrad in 1842 (Jour. Acad. Nat. Sci., Philad., Vol. VIII., p. 280, PI. XV., Fig. 17), may be identical with Elaeacrinus; but the meager and unsatisfactory description of Conrad (' this genus differs from Pentremites, Say, in having only one perforation at top, which is central ') does not apply to any of the forms we propose to group in Elaeacrinus.'" In 1866 Dr. Shumard adopts the suggestion of Prof. Hall. He says : * — " Adopting the suggestion of Prof. Hall, I here include under Granatocrinus (genus proposed by the late Dr. Troost), * Transact., Vol. II., p. 375. 26 Trans. Acad. Set. of St. Louis. a number of elliptical Blastoideans which have hitherto been grouped with Pentremites and Elaeacrinus. The Granaio- crinus (^Pentatrematites) granulatus, Hoeuier = Granato- crinus cidariformis, Troost, may be regarded as the type of the genus, and for the present it may be extended so as to include such species as Pentremites melo and Peritremites norwoodi, Owen and Shumard, and allied forms, though it may become necessary after a while to remove these from Granatocrinus and group them in a separate subsection under another name. They differ from Elaeacrinus in having elongate radial plates, extending, in some instances, almost the entire length of the pseudambulacral fields, while the interradials are in most instances extremely short. The structure of the summit is also quite different ; the anal field is not flattened and conspicuously wider than the others, and it is not provided with a supplementary lanceolate piece as we find in Elaeacrinus proper." In the same year, 1866, F. B. Meek and Prof. Worthen give us a description of the genus Granatocrinus,* which is as follows : — " The generic formula of this group is exactly the same as that of Pentremites, Say, so far as regards the number and arrangement of the pieces forming the body, though the form and proportions of these pieces are so different as to give a very different outline and general physiognomy to the entire fossil. They are therefore readily distinguished from Say's genus, as properly restricted, by their regular oval, elliptical, or subglobose form, concave or less protuberant base, and much narrower and more elongated pseudo-ambulacral areas, which extend the entire length of the body, so as to give it more the appearance of an Echinoid. They likewise present differences in the arrangement of the ovarian ? openings of the summit, which are more intimately connected with the inter- radial pieces, being sometimes excavated, one into each lateral margin of these pieces (^G. sayi); or in other instances piercing directly through them, so that each pair appears * Meek and Worthea. Geological Survey of Illinois, Vol. II., p. 274. Hamhach — Revision of the Blastoideae. 27 externally, as a single opening ( G. melo * and G. norwoodi), though they divide into two distinct canals before passing entirely through the plates. The typical forms of this genus also have the interradial pieces proportionally much larger than in the true Pentremites,'] though this is not a constant character. " In the possession of numerous, extremely slender, thread- like, simple arms, arranged along the pseudo-ambulacral areas, this type also agrees (as might have been inferred from analogy) with the true Pentremites, as we know from the examination of a beautiful specimen belonging to Mr. Wachs- muth. This specimen seems to be related to G. norwoodi^ as near as can be determined, and shows at least thirty (there are probably more) of these delicate, simple arms, arising from each pseudo-ambulacral area, and extending up so that the lower ones must be quite twice as long as the body. They are all composed of equal joints, about as long as wide. So far as we know, this is the only example of a specimen of this type showing the arms, yet found. " As now understood, this genus includes species differing materially in the comparative size of the interradial pieces, the typical species having those pieces very large; J while in another section of the genus, represented by such forms as G. melo and G. no7nvoodi, they are as small as in Pentre- mites. There are so many gradations in this character, how- ever, that it does not seem to be possible to make it a means of separating the species into two well defined sections." The first one to use the name Graiiatoamms was Dr. Troost in a list of new species of Crinoideae from Tennessee, which was read by Prof. L. Agassiz at the meeting of the A. A. A. S. in 1850, and published in the Proceedings of Amer. Assoc, Cambridge Meeting, p. (i2, but, as a descrip- tion of the different species was never furnished, these names * hoc. cit. 274. Here no difference is made between the summit con- struction of G. melo and G. norwoodi. t Meeli and Worthen. Geological Survey of Illinois, Vol. II., p. 275. X Referring evidently to the original species of Dr. Troost, G. cidari- formis Meek and Worthen, Geological Survey of Illinois, Vol. II., p. 275. 28 Trans. Acad. Sci. of St. Louis. are of no vakie and have no right to claim priority- The species which Dr. Troost had designated b}^ this name was first described by Dr. Roemer in 1851 * under the name of Pentatrematites granulatus, to which Dr. Roemer remarks that he had retained the specific name found on the label of Troost' s specimen in the Doctor's collection. However, this name does not appear in Troost' s list, but I can state with permission of the Smithsonian Institution, which is now in possession of the Troost collection, that the collection con- tains specimens labeled by Dr. Troost as Granatocrinus gran- ularis, as is to be seen from the following list : — Troost's number. Granatocrinus granularis (cast) G. cidariformis, 2 specimens G. granularis, 2 specimens (casts) G. globosus, 2 sp., one a cast and one silicifled. . G. (nov.) (cast) 10 miles north of HuntS' ville, Ala G. (cast) Fayetteville, N. C 1993 2839 2788 2788i Number of Smithsonian Institution. 33087 33080 33097 33077 33089 11476 The last two are like the specimens in the Troost collection, but do not belong to it. All these specimens seem to be one and the same species, with the only difference that granularis is a little smaller than cidariformis. Most of them are silicious casts and not in a good state of preservation. With permission of the Smithsonian Institution I will give the Doctor's description, copied from his manuscript together with a figure of both specimens. This description is very deficient as some of the most essential parts have been omitted or misrepresented. The one labeled granularis is a little smaller and deformed but shows the articulation surface of the column, and indica- tions of genital openings, which are ver}'- small for the size of the specimen, but in none of the specimens is the deltoid piece perforated as we find it in G. noriooodi. * Wiegmann's Archiv fur Naturgeschichte, 1851, p. 363. Hambach — Revision of the Blastoideae. 29 " Granatocrinites mihi, new genus. " This genus in some of its characters approaches OUvan- ites and Pentremites, having like these genera five double rows of pores. It is distinguished from the Pentremites by the absence of a column,* and by being destitute of the five characteristic apertures upon which the generic name of Pentremites is founded, and from the Olivanites by the division of the fields between the ambulacrals which in the Granatocrinites is composed of three plates and which is not the case with the Olivanites. " Granatocrinites cidariformis mihi. PI. III., Fig. 1, 2, 3. " Globular slightly elongated. " Pelvis more or less stellated or pentagonal, composed of small plates, forming a small concave dome without any marks of insertion of a column or of an appearance of an alimentary aperture. The five plates which surround the pelvis are elongated sub-pentagonal approaching in form similar plates in the Pentremites, their superior margin being circular and having a longitudinal incision which terminates near the base, where they form the margin of the pelvic cavity and thence rising they enclose partly the double rows of pores which descend from the summit and terminate near the lower margin. " These five plates combined form a cup with five circular elevations at the rim, re-entering angles of which are placed five isosceles triangular plates being beveled at the base so as to fit the rounded margin of the inferior plates. f " Five double rows of pores proceed from the very summit, running along the triangular plates above mentioned and * This I must contradict, as the Doctor certainly has overlooked alto- gether the very plainly marked articulation surface of the column to be seen on his specimen. t Footnote : As given in Troost MSS. 30 Trans. Acad. Set. of St. Louis. entering into the incision of lower series of plates first mentioned terminate near the lower margin of them. The whole surface is granulated; these grains have a tendency to run parallel to the sides of the plates.* " No ovary or oral aperture is visible on the surface; they may nevertheless have existed in the live state, and have been obliterated during fossilification, because judging from siliceous internal casts of the same I think I perceive traces of such apertures. They occur near Shelby ville, Bedford Co., Devonian, and in Allen County, Ky. " Granatocrinites globosus mihi. PI. III., Fig. 4. " It differs from G. cidariformis in being globular, having at the base a circular cavity, the junction of the lower series of plates with those of the superior being curvilinear, and the surface being very irregularly granulated, whereas the G. cidariformis is oval, has a pentagonal basal cavity, the junction of the above mentioned place is rectilinear and its surface regularly granulated. Bedford County, Tennessee." To judge from this insufficient description it is not un- reasonable to suppose that as the Doctor received more material, he changed the name without removing the label gramdaris, regarding both as the same species, otherwise I should think he would have inserted this name in his list. Although this species is a very rare one it was well known to our most distinguished palaeontologists, for Dr. Shumard possessed specimens of it in his collection. It is also rep- resented in Doctor Yandell's collection, and in the catalogue of Worthen's collection offered for sale in 1889, we find under number 66 two specimens named by Worthen, Granato- crinus granulosus, Roemer, from Maury County, Tennessee. These two specimens are now in the Illinois State Col- lection with the same label under number 10066, and one of • This is an incorrect statement, because the specinaen shows just the reverse. Hambach — Revision of the Blastoideae. 31 the specimens shows remarkably well the genital openino-s, ten in number, but no perforation of the deltoid piece as we find in G. norwoodi. From the foregoing it will be seen that our most distinguished palaeontologists, Hall, Shumard, Meek, Worthen, and others were very well acquainted with Penfremites granulatus Roemer = Granatocrinus cidariformis Troost, but from all appearance, they bestowed very little attention upon the morphological conditions of this species. Their main object for consideration seems to have been the general form and appearance. If this had not been the case, one can hardly perceive how Shumard, Hall, Meek and others could have grouped species together in such a way as they have done. If it was necessary to remove Pentremites nor- woodi from the true genus Pentremites on account of its dif- ference in structure, it was equally necessary to separate it from Troost' s Granatocrinus because Pentremites norwoodi differs as much from one as from the other. The same uncertainty is manifested in all the later classifi- cations as will be seen from the following abstracts : Zittel, Handbuch der Palaeontologie, Band I., p. 434, gives it as follows : — " Gattung, Granatocrinus Troost. Elliptisch, eiformig oder kugelich. Kelch wie bei voriger Gattung zusammen- gesetzt, aber B. [Basalstiicke] klein, eingesenkt, seitlich nicht sichtbar. Gabelstiicke verhaltnissmiissig klein, etwa zur halben H5he reichend. Deltoidstiicke gross. Psuedo- ambulacralfelder schmal, linear, bis zur Basis des Korpers herablaufend. Kohlenkalk. Gr. ellipticus, norwoodi, etc." But one of the type specimens shows just the reverse, i. e., 6r. norwoodi. We see here that the most characteristic part, i. e., the nature and construction of the genital open- ings, is not considered, whereas great stress is laid upon all features of a more general character. Hoerne's definition, Elemente der Palaeontologie, p. 128, is:— " Granatocrinus Troost. Kelch wie bei Pentremites zu- sammengesetzt, mit sehr kleinen Basalia, welche seitlich nicht sichtbar sind, auch die Radialstiicke sind klein und 32 Trans. Acad. Sci. of St. Louis. reichen nur zur halben Hohe, wiilirend die luterradialstiicke ungewohnlich gross sind. Granatocrinus norwoodi Owen und Shumard. Kohlenkalk. Hierher gehoren aucli die Pentremites JElUptici Roemer's." Granatocrinus norwoodi is taken as the type, but, in this species, the deltoid-interradial is very small, and the main peculiarity, i. e., the perforation of the deltoid, is not mentioned. Nicholson and Lydekker, Manual of Palaeontology, Vol. I., p. 464, define the genus thus: — " Granatoblastidae. Calyx globular or ovoidal with a flattened or concave base and linear ambulacra. Spiracles five, piercing the deltoids; or ten grooving their lateral edges. This family includes the genera Granatocrinus and Hetero- blasfus." This arrangement shows a marked inconsistenc}^ because Heterohlastus possesses more essentially the characters of Cryptoblastus, and has more aflnnities with it than with Grana- tocrinus, so that it would more properly belong to this genus. Eastman's* definition is the following: — "Calyx globular or ovoidal with flattened or concave base and long linear ambulacra. Spiracles five piercing the deltoids, or ten grooving their lateral edges. Consisting of Granato- crinus and Ileteroblastus.'" Here we have the same inconsistency. The last genus has all the essential characters of Cr}/2)toblastus, with the exception of spine-like processes on the deltoids, though these spine-like projections are met with in many species, for example Pentremites sidcatus, where it seems the deltoid pieces are very much inclined to develop spiny projections. I have a number of specimens showing them of various forms and sizes. Those from the neighbor- hood of Ste. Genevieve show it most, whereas those from Chester or Evansville rarely show any such hypertrophic growth, while we meet with it again in specimens from Baldwin and other localities. Another case which shows very clearly the arbitrary way * Text-Book of Palaeontology, Vol. I., p. 196. Hambach — Revision of the Blastoideae. 33 of classification is to be found in the diagnosis of Nucleoblas- tidae, Etheridge and Carpenter. This family is divided into Sub-family A. Elaeacrinidae and Sub-family B. Schizoblas- tidae. The only peculiarities common to both are the elliptical or ovoidal form of the body and the extremely short fork-pieces, which latter fact is not mentioned in their diagnosis. Elaea- crinus has its posterior deltoid divided and an elongated piece inserted, which is never the case in 8cMzohlastus. Moreover the center of the summit is firmly closed by pieces of a uni- form shape and position in Elaeacrinus, which is not the case in 8cMzoblastus where the center is open, or closed only by the ambulacral integument. Nicholson and Lydekker's description of this family, which is accompanied by two figures, is still more confused, reading as follows : — "Family III. Nucleoblastidae. Calyx usually globular or ovoidal with flattened or concave base and linear ambu- lacra. Spiracles distinctly double, and chiefly formed by the opposition of notches in the lancet plates and deltoids. This family includes Elaeacrinus (with an anal plate) and Schizoblasfus, Fig. 332 c and d, Cryptoblastus and Acento- tremites (without an anal plate)." PROPOSED CLASSIFICATION. The classification here offered is based mainly on the con- struction of the summit openings, because they exhibit a uniformity in structure, remaining always the same in their respective genera — a fact which must be of great value for classification. Next the development of the deltoids is con- sidered, also the aspect of the outer surf ace (whether smooth or spiny). Whereas the general size and shape of the body, whether globose, pyriform, ovoidal, conical or clavate, depends upon the variations in the form of the parts which construct the body, and whereas the relations of these parts to each other remain the same throughout the whole class, the difference can be only specific and not generic. Nor can we attribute any more than specific value to the hydrospiric tubes, or plications, on account of the variability often 34 Trans. Acad. Sci. of St. Louis. observed in one and the same specimen — a fact sufficiently recognized by the very authors who regard them as being of importance for classification. All names ending in " crinus " are omitted. I also wish to remark that this classification embraces only our American species, although most of the European species, I believe (judging from my small collection of European specimens), will fit into one or another of these genera, with the exception of aberrant forms, like some of our American ones, of which it is still doubtful whether they should be regarded as Blastoids or Cystoids, for the reception of which a separate class should be established. This class may in- clude all doubtful specimens and those insufficiently described and doubtfully illustrated because of the fragmentary con- dition of the material. CLASS BLASTOIDEAE. A. Order Regulares. 1. Family Pentremidae. 1. Genus Pentremites, Say. 2. Genus Cribroblastus. 3. Genus Saccoblastus. 4. Genus Clavaeblastus. 5. Genus Mesoblastus, Etheridge fil. and Carpenter. 6. Genus Cidaroblastus. 7. Genus Globoblastus. 8. Genus Codonites, Meek and Worthen. 2.;Family Codasteridae. 1. Genus Codaster, Maccoy. Hambach — Revision of the Blastoideae. 35 B. Order Irregulares. 1. Family Olivanidae. 1. Genus Olivanites. 2. Family Eleutheroblastidae. 1. Genus Eleutheroblastus. Blastoideae are dicyclical Pelmatozoa. The body is com- posed of twenty pieces (at least in the embryonic state), arranged in two circles of even numbers and an irregular number of accessory pieces (say poral pieces), with the exception of one order, Irregulares, where one or the other circle contains an odd piece, a total difference from all others. All were supported by a slender round or triangular column, except one genus {Eleutherohlastus) as far as known. Geolog- ically they belong to the Palaeozoic Age, commencing in the upper Silurian, gradually increasing until they reach their culmination point in the upper Subcarboniferous, and becom- ing extinct with the close of the Chester limestone. Geo- graphically they have been observed in Europe, Australia and America, from which country the greatest number of species has been described. Family Pentremidae. Body of various forms, all supported by a round or trian- gular column. None of the summit openings permanently closed except by the ambulacral integument. All of this family, whenperfectly preserved, are known to possess pinnulae and probably many of them, if not all, had a short proboscis. 1. Genus Pentremites. General form of body globose, ovoid, conical, pyriform or club shaped. Central orifice never closed except by the am- bulacral integument, surrounded by eleven openings, which appear externally as five, and are constructed by the junction of deltoid and lancet pieces. Deltoid pieces variable, visible 36 Trans. Acad. Sci. of St. Louis. externally in the adult species, and in others they are never visible externally. Ambulacrum rather broad. Column round. This genus will include the following species : — 1. Pentremites abbreviatus, Hambach, 1880. Chester limestone. This species is erroneously taken to be identical with Pentremites godoni, by Etheridge, Jr., and P. H. Car- penter, C. R. Keyes, and others. In so doing they mis- take the facts, and I must say that none of these gentlemen is acquainted with this species. If they were, or if they had taken the trouble to compare my figure and description* with Pentremites godoni, they would have seen that they are not one and the same species. Carpenter's figuref does not represent the essential characters given in my description, which makes it differ from the typical Pentremites godoni. M}^ species is quite rare, and has, as far as I know, been found only at one small locality, about 500 feet square, in a semi-oolitic limestone, although the whole country around is rich in Pentremites, esj)ecially in Pentremites sidcatus. The specimen figured by me is the largest I have ever seen of this spe- cies. In all specimens, whether large or small, the transverse diameter is i larger than the vertical one. The in- terambulacral space is more rounded, also the ambulacrum, and there is not a sharp crest at Fig. 12. a. b. a. Pentremites abbreviatus. b. " godoni. c. florealis. both sides of it as we find in Pentremites godoni. * Transactions St. Louis Academy of Science, Vol. IV., p. 155, Fig. 3. t Catalogue of the Blastoidea, Plate II., Fig. 4. Hambach — Revision of the Blastoideae. 37 In a lateral view the base is never visible. For com- parison see the accompanying figure 12. 2. Pentremites ANGULARis, Lyon, 1860. Chester limestone. 3. Pentremites basilaris, Hambach, 1880. Chester lime- stone. 4. Pentremites Broadheadi, Hambach, 1880. Chester limestone. 5. Pentremites burlingtonensis. Meek & Worthen, 1869. Burlington limestone. 6. Pentremites CALYCiNUS, Lyon, 1860. Chester limestone. 7. Pentremites cervinus. Hall, 1858. Chester limestone. 8. Pentremites chesterensis, Hambach, 1880. Chester limestone. 9. Pentremites clavatus, Hambach, 1880. Chester lime- stone. 10. Pentremites conoideus, Hall, 1856. Warsaw limestone. This species is synonymous with Pentremites kon- inckana, Hall, which is only the young stage of P. conoideus. 11. Pentremites elegans, Lyon, 1860. Chester limestone. This species is synonymous with the one designated by Dr. Troost as tennesseae, nom. nud. The descrip- tion of Troost was never published. The specimens so designated by Troost, now in the collection of the Smithsonian Institution, No. 33,072, are the same as those described by Lyon as Pentremites elegans. 12. Pentremites elongatus, Shumard, 1855. Burlington limestone. 13. Pentremites florealis, v. Schlotheim, 1820. Chester limestone. Pentremites symmetricus, Hall. Chester limestone. Pentremites altus, Rowley. 38 Trans. Acad. Sei. of St. Louis. Shumard and many later authors confound this species with Pentremites godoni, which is a sad mis- take because there is a considerable difference between these two species. In the typical P. jlorealis the body is more elongated, the base portion drawn out and more prolonged than in Pentremites gocloni, and the plications of the ambulacral integument are coarser than in P. gocloni. The typical Pentremites Jlo7'ealis is comparatively rare in Alabama and Kentucky but not so at Chester, Illinois, where Pentremites godoni does not occur at all. We find it again at Waterloo, Illinois, associated with Pentremites Jlorealis, but it is by far the predominating species here. 14. Pentremites gemmiformis, Hambach, 1884. Chester limestone. 15. Pentremites godoni, De France, 1818. Chester lime- stone. Kentucky arterial fossil, Parkinson, 1808. Pentremites globosiis, Troost. 16. Pentremites hemisphericus, Hambach 1880. Chester limestone. 17. Pentremites nodosus, Hambach 1880. Chester lime stone. 18. Pentremites obesus, Lyon, 1857. Chester limestone. 19. Pentremites pyriformis. Say, 1825. Chester limestone. Pentremites subconoideusy Meek, a young form of pyriformis. This species differs from P. Jlorealis, its nearest relative, in having its greatest diameter at the apex of the ambulacrum, dividing the calyx in two equal halves, i. e., the distance from the articulation surface of the column equals the distance from the apex of the ambulacrum to the summit. 20. Pentremites spinosus, Hambach, 1880. Chester lime- stone. Hambach — Revision of the Blastoideae. 39 21. Pentremites suLCATUSjEoemer, 1852. Chester limestone. Pentremites cherokeeus, Troost M. S. Pentremites robustus, Lyon. Pentremites laterniformis, Ovvtn and Shumard. The hitter, which has been regarded as a synonj^m for Pentremites ohliquatus, is the cast of Pentremites sulcatus. The confounding of this species with P. obliquatus must have been caused by assuming that a cast of ohliquatus would furnish an elongated prismatic lower calyx part, as we have in P. laterni- formis, which is due to the internally straight base portion of the fork pieces in Pentremites sulcatus, as I have described and figured years ago. Moreover all Pentremites laterniformis have been described as com- ing from the Chester limestone, where such casts are frequently met with, but the Saccoblastns ohliquatus (= P. laterniformis, Troostocrinus laterniformis, Tricoelocrinus ohliquatus) does not occur in this formation and so far has been found only in the Warsaw or Keokuk formation. 22. Pentremites bradleyi, Meek. Subcarboniferous. 2. Genus Cribroblastus. General form of body elliptical or globose, of medium size, seldom over ^ inch vertical diameter. Ambulacrum narrow, linear, and extending almost over the whole body. Central opening never closed, except by ambulacral integument, sur- rounded by eleven openings constructed by the junction of deltoid and lancet piece, very small and never confluent with each other. Anal opening on the posterior side between two genital openings, from which it is separated by two fine septa. Deltoid pieces very variable, occupying from i^j- to f of the interambulacral space. Base portion small, more or less depressed. Column round. This genus will include the fol- lowing species. 40 Trans. Acad. Sci. of St. Louis. 1. Cribeoblastus cornutus, F. B. Meek and A. H. Wortben. St. Louis limestone. Pentremites cornutus, Meek and Worthea. Granatocrinus cornutus, Shumard. Elaeacrinus cornutus, Shumard. Heteroblastus cornutus, EcherHge and Carpenter. 2. Cribroblastus CURTUS, Shumard. St. Louis limestone. PenP'emites curtus, Saumard. Oranatocrinus crirtus, Shumard. Orbitremites curtus, Bather. *3. Cribroblastus GRANULOSUS, Meek and Wortlien. Bur- lino;ton limestone. Pentremit'is granulosus, Meek and Worthen. Granatocrinus granulosus, Meek and Worthen. Schizoblastus granulosus, E:ihcridge and Carpenter. 4. Cribroblastus kirkwoodensis, B. F. Shumard. St. Louis limestone. Elaeacrinus kirkiooodensis, Shumard. Cryptoblastus kirkiooodensis, Keyes. Nucleocrinus kirkiooodensis, Miller. Schizoblastus missouriensis, Etheridge anrl Carp'inter. 5. Cribroblastus LOTOBLASTUS, C. A. White. Lower Car- boniferous 2.V. Granatoc7-inus lotoblastus, White. Orbitremites lotoblasCus, Bather. Schizoblastus lotoblastus, Weller. It is ver}' doubtful whether this species belongs here. Nothino;, however, can be said until more material has been collected. The only specimen known is the type of "White's description, now in the collection of the Smithsonian Institution, No. 8541. The specimen is much incrusted and does not show an3^thing of the sum- mit openings which are mostl}' covered by foreign matter. 6. Cribroblastus melo, Owen and Shumard. Burlington limestone. Pentremites melo, Owen and Shumard. Granitocrinus melo, Shumard. Elaeacrinus melo, Shumard. Cryptoblastus melo, Etheridge and Carpenter. * Hamhach — Revision of the Blastoideae. 41 7. Cribroblastus MELONOiDES, Meek and Worthen. Bur- lington limestone. Oraiiatocrinus melonoides, Meek and Worth ;n. Schizoblastus melonoides, Etheridge and Carpenter, *8. Cribroblastus neglectus, Meek and Wortlien. Bur- lington limestone. Oranatocrinus neglectus, Meek and Worthen. Schizoblastus neglectus, Etheridge and Carpenter *9. Cribroblastus pisum, Meek and Wortlien. Burlington limestone. Oranatocrinus pisum, Meek and Worthen. Cryptoblastus pisum, Etheridge and Carpenter. Schizoblastus pisum, Etheridge and Carpenter. 10. Cribroblastus potteri, Hambach. Burlington lime- stone . Pentremites potteri, Hambach. Schizoblastus sayi, Etheridge and Carpenter, 11. Cribroblastus projectus, Meek and Worthen. Bur- lington limestone. Pentremites melo, Yir, projectus, Meek and Worthen. Granatocrirms projectus, Meek and Worthen. Cryptoblastus projectus. Bather. '12. Cribroblastus roemeri, Shumard. Chemung and Chouteau limestone. Pentremites roemeri, B. F, Shumard. Oranatocrinus roemeri, Shumard. Orbitremites roemeri, B ither. Schizoblastus roemeri, Keyes. '13. Cribroblastus sampsoni, Hambach. Chouteau lime stone. Pentremites sampsoni, Hambach. Schizoblastus sampsoni, Etheridj;e and Carpenter. Schizoblastus roemeri, Keyes. This species is not synonymous with C . roemeri as Keyes takes it. The external ornamentation of the interambulacrum differs very much from that of roemeri (see PL V., Figs. 9 and 10). Moreover the relative width of the interambulacrum is about \ 42 Trans. Acad. Sci. of St. Louis. greater than in C. roemeri. Crihrohlastus roemeri is much rarer than C . sampsoni. *14. Cribroblastus sayi, Shumarcl. Burlington limestone. Ferdremites sayi, Shumard. Granatocrinus sayi, Shumard. Schizohlastus sayi, Etheridge and Carpenter. Schizoblastus potteri, Etheridge and Carpenter. My species O. potteri has been taken as synonym for O. sayi. The interambulacrum of C. sai/i is broader and transversely striated and more elevated than in C . potteri. The base portion in O . sayi is depressed so that the basal part is not visible in a lateral view, which is the case in O . potteri. The slit-like openings at the summit in both species, as well as in C . melonoides, are due to the ambulacral integument in the immediate neighborhood of the genital openings. The perfectly round form of the genital openings can be sufficiently proved in weath- ered specimens, where the ambulacral integument is eroded. Moreover it seems that this species is very rare at Burlington, as of all specimens coming from that locality, I have not noticed more than a dozen typical specimens. Shumard' s type specimen came from Marion County in the neighborhood of Palmyra. It also occurs in Boone County, St. Louis County, and at Louisiana, Missouri. 15. Cribroblastus shumardi, Meek and AVorthen. Bur- lington limestone. G-ranatocrinus shumardi. Meek and Wortheu. Mesoblastus simmardi, Etheridge and Carpenter. Schizohlastus shumardi, Etheridge and Carpenter. For difference of those species marked with an aste- risk, see Plate V., Fig. 9, 10, 11, 12, 13, 14, 15. 3. Genus Saccoblastus. General form of the body pyriform, compressed cylindri- drically, or club-shaped. Ambulacra narrow and linear, gen- Hambach — Revision of the Blastoideae. 43 erally, sunk into the fork piece sinus so that the surface does not touch the upper margin of the fork piece sinus. Lower part of the body shows three distinctly depressed areas ; the amount of depression varies in the different species. Inter- ambulacral surface smooth or very finely striated. Summit opening never closed except by the ambulacral integument. Genital openings ten, of a slit-like appearance, on account of the orifice opening obliquely. Anal opening so far below the genitals that in large specimens it is almost J inch below the summit, and as far as known not covered. All specimens which I have had an opportunity to examine (over six hun- dred) did not show any sign of a covering. Column triangu- lar. This genus comprises Troostocrinus , Tricoelocrimis and MeAablastus, and to show the gradual transformation from one to the other I have given good figures of all our American species on Plate IV. All described specimens are from the Warsaw limestone or below from the lower Subcarboniferous rocks. 1. Saccoblastus bipyramidalis, Hall. Warsaw limestone. Fentremites bipyramidalis Hall. Troostocrinus bipyramidalis Hall. Metablastus bipyramidalis, R. Etheridge fll. and P. H. Carpenter. 2. Saccoblastus lineatus, B. F. Shumard. Burlington limestone. Fentremites lineatus, Shumard. Troostocrinus lineatus, Shumard. Metablastus lineatus, Etheridge fll. and Carpenter. 3. Saccoblastus obliquatus, Roemer. Warsaw hmestone. Fentatrematites obliquatus, Roemer, Fentremites occidentalis, Shumard. Tricoelocrimis obliquatus, R. Etheridge fll. and Carpenter. Troostocrinus later niformis, Shumard. 4. Saccoblastus woodmani, Meek and Worthen. Warsaw and Keokuk limestone. Tricoelocrinus woodmani, Meek and Wortheu. Troostocrinus woodmani, Meek and Worthen. 5. Saccoblastus wortheni, I. Hall. Warsaw limestone and Keokuk. Metablastus wortheni, R. Etheridge fll. and Carpenter. 44 Trails. Acad. Sci. of St. Louis. Pentremites grosvenori, Shuraard. Troostocrinus grosvenori, Etherid^e and Carpenter. Troostocrinus nitidulus, S. A. Miller and Gurley. Metablastus varsoziviensis, Etheridge and Carpenter. Pentremites varsoitviensis, Meek and Worthen. Metablastus xoachsmuthi, Gurley. Troostocrinus loachsmuthi, Gurley. 6, Saccoblastusmeekianus, R. Etheridge fil . and Carpenter. Warsaw limestone. Tricoelocrimts meekianus, Eth. and Carp. 4. Genus Clavaeblastus. General form of the body club-shaped, or elliptical. Am- bulacra narrow and linear. Deltoids not visible externally, except on the posterior side, where the deltoid piece supports the anal opening which lies outside of the genital openings, which are confluent and surround the central opening. Col- umn round. Upper Silurian and Devonian. If more material should be collected from the Devonian rocks, it may bring to light characteristics as yet unknown, which may necessitate the creation of a new genus for this form. This genus will include the following species : — 1. Clavaeblastus amekicana, W. H. Barris. Hamilton group. Pentremitidea americana, W. H. Barris. 2. Clavaeblastus filosa, I. F. Whiteaves. Hamilton group. Pentremitidea filosa, I. F. Whiteaves. Pentremites lohitei, Hal!. 3. Clavaeblastus milwaukensis, S. Weller. Hamilton group. Pentremitidea milwaukensis, S. Weller. 4. Clavaeblastus REiNWARDTii, G. Troost. Niagara group. Pentremites reinwardtii, Troost. Troostocrinus reinwardtii, Shumard. Pentremites subcylindricus, Hall and Whitfield. Hambach — Revision of the Blastoideae. 45 5. Genus Mesoblastus, Etheridge fil. and Carpenter. Body small, round or elliptical. Base small and flat. Am bulacra narrow and convex, extending the whole length of the body. Ambulacral integument scroll-like. Deltoids very small, hardly visible in a lateral view, but more so in a sum- mit view, except the posterior one which supports the anal opening, which is outside of the genital openings. Genital openings not confluent, but connected by a small sulcus, run- ning from one to the other in a V shape. Column round. With only one species. 1. Mesoblastus glaber. Meek and Worthen. St. Louig limestone. Qranatocrinus glaber, Meek and Worthen. 6. Genus Cidaroblastus. General form of body elliptical or globose. Ambulacra narrow and linear, extending almost over the whole surface of the body. Central opening never closed except by ambu- lacral integument. Genital openings ten, constructed by the junction of the deltoid and lancet pieces, very small and never confluent with each other. Anal opening on the posterior side between two of the genital openings. Deltoid pieces very large in all known species, occupying almost half of the interambulacrum. Whole interambulacral space covered with large tubercles for the attachment of spines. Base pieces small and depressed, being never visible in a side view. Column round. This genus contains the typical Granatocrinus of Dr. Troost of which I give three figures on Plate III., drawn from the type specimens in the Troost Collection now in the Smithsonian Institution. Geological position, in the Subcarboniferous rocks. 1. Cidaroblastus GRANULATUS, Roemer. Subcarboniferous. Pentatrematites granidatus, Roemer. Qranatocrinus cidariformis, Troost. G-ranatocrinus globosus, Troost. Orbitremites granulatus, Bather. 46 Trans. Acad. Set. of St. Louis. 7. Genus Globoblastus. General form of body globose or elliptical. Ambulacrum narrow and linear, extending almost over the whole surface of the body. Central opening never closed except by am- bulacral integument. Genital openings five, piercing the deltoid pieces and bifurcating in the substance of the shell toward the interior. Anal opening large to receive the anal tube which is on the posterior side in the center of this bi- furcation, making this opening twice as large as the others. Deltoid pieces of variable size, in some species occupying almost half of the interambulacral surface. Base small and very much depressed. Column round. My reason for not using the name Granatocrinus is suffici- ently explained in the foregoing pages. Besides its ending in ' ' crinus ' ' the genus contains so many di:fferent forms among the various authors, that it is apt to be misleading to the student. The name Orhitremites , Austin, which Mr. Bather adopted as the one which should have priority, is only a name without a generic diagnosis, and therefore equally inadequate. To avoid all confusion I propose the above used name. The genus includes the following species : — Globoblastus norwoodi, Owen and Shumard. Burling- ton limestone. Pentremites noriooodi, Owen and Shumard. Granatocrinus noriooodi, Shumard. Orbitremites noricoodi, F. A. Bather. 8. Genus Codonites. General form of the body, bell or star-shaped. Ambulacra narrow and linear, extending out and downward, thus giving a more or less star-shaped appearance to the summit. Central opening very small and usually covered by the ambulacra! integument. Genital openings, long slits at each side of the ambulacrum. Anal opening large and lateral. Base, funnel- shaped. Column round and large for the size of the specimen Eamhacli — Revision of the Blastoideae. 47 when compared with Pentremiles* All known species belong to the lower Subcarboniferous. This genus will include the following species : — 1. CoDONiTES coNicus, C. Wachsmuth and F. Springer. Kinderhook gr. Orophocrimis conicus, Wachsmuth and Springer. 2. CoDONiTES CAMPANULATUS, Hambach. Lower Burling- ton limestone. Orophocrimis campanulatus , Keyes. Orophocrimis stelliformis, Ethericlge and Carpenter. 3. CoDONiTES FusiFORMis, Wachsmuth and Springer. Kinderhook gr. 07'ophocrinus fusiformis, Wachsmuth and Springer. 4. CoDONiTES GRACILIS, Mcck and Worthen. Lower Bur- lington limestone. Orophocrimis gracilis, Meek and Worthen. 5. CoDONiTES STELLiFORMis, Owcn and Shumard. Lower Burlington limestone. Pentremites stelliformis, Owen and Sauraard. Orophocrimis stelliformis, Meek and Worthen. 6. CoDONiTES WHiTEi, Hall. Burliugtou limestone. Codastus whitei, Hall. Orop>hocrimis whitei, Whitfield. 2. Family Codasteridae. 1. Genus Codaster. General form of the body bell-shaped or obconical. Am- bulacral side more or less horizontal. Ambulacra linear. Mouth small and central. Anus large and lateral, placed be- tween two ambulacra. Numerous slits at each side of the ambulacrum, except on the posterior side, i. e., on the side which faces the anal opening, where they are wanting. Inter- * It is more closely ralated to Pentremites than to Codaster on account of the hydrospires. 48 Trans. Acad. Sci. of St. Louis. ambulacral areas often acute and projecting beyond the sum- mit. Column thin and round. Geoloo;ical range from the upper Silurian to the Coal Measures. The following species belons: to this genus : — 1. CoDASTER ATTENUATUS, Lyon. Devonian. Cadaster attenuatus, Owen. Heteroschisma alternatum, Wachsmuth. Heteroschisma alternatum var. elongatum, Wachsmuth. 2. Cod ASTER americanus, Shumard. Devonian. 3. CoDASTER cInadensis, E. Billiugs. Devonian. Cadaster hindei, Whiteaves. 4. CoDASTER GRACILIS, Wachsmuth. Devonian. Heteroschisma gracilis, Wachsmuth. 5. CoDASTER KENTUCKYENSis, Shumard. Lower Subcarbo- niferous. Pentremites kentiickyensis, Shumard. Phaenoschisma, Etheridge and Carpenter. 6. CoDASTER PULCHELLUS, S. A. Miller and C. B. Dyer. Niagara gr. Stephanocrinus puchellus, Miller and Dyer. 7. CoDASTER PYRAMiDATUS, Shumard. Devonian. Cadaster alternatus (pars), Lyon. 8. CoDASTER suBTRUNCATUS, Hall. Devonian. Pentremites suhtruncatus , Hall. Heteroschisma gracile, "Wachsmuth. Traastocrinus suhtruncatus, Etheridge and Carpenter. B. Order Irregulares. 1. Family Olivanidae. 1. Genus Olivanites. General form of the body oval or round. Base very small and depressed. Fork pieces very short, hardly more than -g- of the whole length of the body. Ambulacra narrow, linear and extending the full length of the body. Deltoids very Hambach — Revision of the Blastoideae. 49 large, occupying nearly f of the whole length. Genital openings constructed by the junction of the deltoid and lancet piece, and not confluent. Poral pieces varying in number ac- cording to the size of the species. Center of the summit closed by additional pieces. The main opening (the anal ?) is lateral and posterior, i. e., the posterior deltoid is divided in half and an elongated piece inserted as a support for the opening. Column round. Nearly all the material collected so far is of such a nature as to make a more accurate description impossibie. Geologi- cally they belong to the Devonian. Here we hnd the first irregularity in the construction of the calyx. It is difficult to say whether the elongated piece should be counted to the ambulacral or the interambulacral cycle, giving one or the other an old number of pieces. The name Nucleocrinus , introduced by Conrad in 1842, is here rejected, first because of its ending in "crinus," and secondly because of the insufficient diagnosis, which reads as follows : " This genus differs from Pentremites sayi in having only one perforation at top, which is central."* Oii account of this insufficiency it was not adopted by most of our Amer- ican palaeontologists. It is absolutely impossible to recognize or identify a specimen from the above description, accom- panied by an incorrect drawing. Roemer's name Elaeacrinus has to be rejected also on account of its ending in "crinus." By so doing, and not to increase the nomenclature with synonyms, I have adopted Lyon's designation as the most suitable one. This genus will include the following species : — 1. Olivanites angularis, Lyon. Devonian. Nucleocrinus angularis Etheridge and Carpenter. Elaeacrinus angularis, Shumard. *2. Olivanites conradi, Hall. Devonian. Nucleocrinus conradi, Hall. Elaeacrinus conradi, Hall. Nucleocrinus verneuili. Hall. * Journal of the Academy of Natural Sciences of Philadelphia, 1842, Vol. VIII., page 280, PI. XV ;- Fig. 17. 50 Trans. Acad. Sci. of St. Louis. 3. Olivanites elegans, T. a. Conrad. Devonian. Nucleocrinus canadensis, H. Montgomery. Nucleocrinus hallii, L. Vanuxem. Elaeacrinus elegans, Shumard. Nucleocrinus veniistus, Miller aud Gurley. *4. Olivanites greeni, S. A., Miller and W. F. E. Gurley. Devonian. Nucleocrinus greeni, Miller and Gurley. *5. Olivanites globosus, Troost. Devonian. 6. Olivanites lugina, Hall. Devonian. Nucleocrinus lucina. Hall. *7. Olivanites meloniformis, W. H. Barris. Devonian. Elaeacrinus meloniformis, Barris. 8. Olivanites obovatus, W. H. Barris. Devonian. Elaeacrinus obovatus, Barris. 9. Olivanites verneuili, Lyon. Devonian. Pentremites verneuili, Troost. Elaeacrinus vernenili, Roemer. Nucleocrinus verneuili, Bather. Those marked with an asterisk may have to be placed in another orenus or mav prove to be identical with one or another abeady known species, which facts can only be established when more material for comparison is available. 2. Family Eleutheroblastidae. 1. Genus Eleutheroblastus. General form elliptical, truncated at the summit and sub- triangular at the base. Base very irregular, subtriangular at the lower part, and prolonged on one of its sides to a remark- able length. It consists of three pieces, one small rhombic piece and two large pieces prolonged nearly to the middle of the calyx. Fork pieces four, non-symmetrical, each having a lono' sinus in the center for the reception of the ambulacrum. The two middle pieces have a shorter sinus, whereas the two Hambach — Revision of the Blasioideae. 51 lateral pieces have a sinus at least ^ inch longer, and, con- sequently, a longer ambulacrum. The fifth fork piece is shortest, being only half as long as the others, but much wider and rests upon the upper edges of the two large basals. This piece has a very broad but short sinus, and correspond- ing ambulacrum. Deltoids five and small. Ambulacra nar- row and linear; the fifth broad and triangular and lying horizontally on the summit. Mouth central. No anal open- ing visible. Genital openings five, each one divided by a septum. I consider the side with the short and broad ambulacrum the posterior part of the calyx. No column. Devonian. 1. Eleutheroblastus canedayi, B. F. Shumard and L. P. Yandell. Devonian. Eleutherocrinus canedayi, Shumard and Yandell. 2. Eleutheroblastus whitfieldi. Hall. Hamilton group. Eleutherocrinus whitfieldi, Hall. The followmg species are insufficiently described and illus- trated to be identified and classified with certainty : — Blastoidocrinus carchariaedens, Billings. Pentremites decussatus, Shumard. Pentremites maia, Hall. Pentremites leda, Hall. Pentremites calyce, Hall. Pentremites lycories. Hall, Pentremites whitei, Hall. Codaster blairi, Miller and Gurlev. Codaster jessieae, Miller and Gurley. Nucleocrinus venustus, Miller and Gurlev. Granatocrinus sphaeroidalis. Miller and Gurley. Granatocrincus winslowi, Miller and Gurley. Granatocrinus aplatus, Rowley and Hare. Granatocrinus concinnulus, Rowley and Hare. Granatocrinus pyriformis, Rowley and Plare. Granatocrinus exiguus, Rowley and Hare. 52 Trans. Acad. Sci. of St. Louis. Codonites inopinatus, Rowley and Hare. Granatocrinus excavatus, Rowley and Hare. Codaster gracillimus, Rowley and Hare. Codaster grandis, Rowley. Lophoblastus conoideus, Rowley. Lophoblastus marginulus, Rowley. Carpeuteroblastus pentagonus, Rowley. Carpenteroblastus magnibasis, Rowley. Carpenteroblastus pentalobus, Rowley. Carpenteroblastus stella, Rowley. Codaster laeviculus, Rowlev. Granatocrinus calycinus, Rowley. Granatocrinus spinuliferus, Rowley. Pentremites benedicti, Rowley. Troostocrinus dubius, Rowley. DESCRIPTIONS OF NEW SPECIES. Pentremites tulipaformis n. s. Plate IV., Fig. 10, 11. Body oval in outline with the broadest part downward and the greatest transverse diameter at the apex of the ambulac- rum. Basals small, each rounded and nodose, causing the articulation surface of the column to become a little depressed or sunk between these three nodules and therefore not visible in a lateral view. Ambulacrum broad, leaf -like and groove- like, occupying three-fourths of the whole length of the body. Poral pieces ten to one-eighth of an inch. Interambulacral space smooth and not depressed, giving the lower part of the body a somewhat rounded form. Lateral expansion of the deltoid occupying about one-third of the whole length of the calyx. Genital openings and mouth small and close together. This species belongs to the Chester limestone and is found at Kaskaskia, Illinois, but is by no means common. Hambach — Revision of the Blastoideae. 53 Pentremites obtusus n. s. Fig. 13. Among the great number of Pentremites {Pentrevnites co- noideus) so characteristic of the Boonville locality, we find by close examination of a large amount of material that they are not all one and the same kind and we can readily pick out a number which, although re- sembling very much Pentremites conoideus, differ constantly in certain characters from this spe- cies, so that we are forced to regard them as a distinct species. Their body is conical with a flat basal portion, the small basal pieces not visible in a side view; ambulacrum narrow with a rounded surface and extending to the base of the body. Vertical diameter never, even in a small specimen, greater than the horizontal one, by which it can easily be recognized from P. conoideus. Interambu- lacral space smooth and not as much depressed as we find it in Pentremites conoideus. Genital openings small and close together. It is a distinct Warsaw species. Geological position and locality : It occurs in the Warsaw limestone of Boonville, Missouri. Fig. 13. Pentremites angustus n. s. Fig. 14. Body elongate, obtuse, conical. Base small, flat and not visible in a side view. Ambulacrea as Ions; as the whole body and nearly three-sixteenths of an inch in width, extend- ing a little above the fork piece sinus and slightly rounded on the surface. Poral openings twelve to one- eighth of an inch. Interambulacral space smooth and not de- pressed in the center. Lateral expansion of the deltoid externally . -^ a. Pentremites angustus. Visible and occupying b. " " base view, fully one-half of the c. Pentremites conoideus, base view. 54 Trans. Acad. Sci. of St. Louis. whole length of the body. Genital openings small and close together, appearing on the outer surface as five, of which one is twice as large as the others. This species resembles some- what Pentremites conoideus though it is easily recognized and distinguished from P. conoideus by not having the summit as acute as conoideMs, by its wider ambulacra and by its inter- ambulacral space not being depressed as in conoideus. It is distinguished from Pentremites elongatus by its more conical form, perfectly flat basal portion, having the greatest diam- eter of the body right at the apex of the ambulacrum and not having the interambulacral space finely striated as we find it in Pentremites elongatus. It belongs to the Chester limestone, but has been so far known only from Washington County in Arkansas. Pentremites turbinatus n. s. Plate v., Fig. 6. Body turbinate or inverted pyramidal. Base large for the size of the specimen and funnel shaped. Fork pieces elon- gate, square and large; sinus broad extending down only half the length of the piece. Ambulacrum broad, leaf -like and flat. Poral pieces eleven to one-eighth of an inch. Deltoids externally not visible. Interambulacral space rather flat and smooth. Genital openings close together. Greatest trans- verse diameter at the apex of the ambulacrum which occupies the upper third of the body. Geological position and locality: Chester limestone, Evans- ville, Illinois. Very rare. Pentremites rusticus n. s. Fig. 15. Body almost cylindrical, i. e., the diameter at the base is as great as near the summit. Basal plates very small and not visible in a lateral view. Ambulacra as long as the body with a somewhat rounded surface and sunk into the fork piece sinus which has a sharp and prominent margin. Poral openings Fig. 15. thirteen to one-eighth of an inch. Lateral expres- sion of deltoid one-third of the whole length of the body, Hambach — Revision of the Blastoideae. 55 extending near the summit prominently outward, giving to the body a square appearance. Interambulacral space not depressed as in Pentre'mites conoideus and covered with fine striae, running parallel to the sutures. Genital openings small and close together as in the foregoing species. Geological position and locality : It occurs in the Chester limestone and is known so far only from Washington County, Arkansas. Pentremites kirki n. s, Plate v., FifT. 18. General form of the body cylindrical, about | of an inch in length and -{"^ of an inch in width. Base very robust and funnel shaped, with a large articulation surface for the column, almost as wide as in Codoniies. Distance from the articulation surface of the column to the apex of the ambu- lacrum about two-fifths of the entire length of the body. Ambulacra broad and slightly rounded with a very coarse plicable integument with only eight plications to one-eighth of an inch. Interambulacral space rather narrow, with a slight depression in the center and a sharp, projecting, spiny crest at the apex of the ambulacrum. Whole surface of the interambulacral space and the base portion ornamented with fine striations, running parallel to the sutures. Deltoids hardly visible externally, but the summit projects about Yt of an inch above the sharp point of the fork piece. Genital openings, as in Penfremifes elongatus or burlington- ensis where the anterior portion, or the outer septa of the deltoid base, divide each opening in two, while the posterior one is divided into three so that the summit shows very dis- tinctly twelve openings. Geological formation and locality : Lower Burlington lime- stone. It gives me great pleasure to name this beautiful little Blastoid in honor of Mr. E. Kirk, the lucky finder, who is a very energetic and prominent young collector. 56 Trans. Acad. Sci. of St. Louis. Pentremites bradleyi Meek. Plate v., Fig. 7. TBodv small, obtuse, conical. Basal portion almost flat, and resembling that of Pentrevmtes conoideus very much, but be- ing more rounded and having a larger articulation surface for the column, in proportion to its size, than Pentremites conoideus. Ambulacra broad, excavated along the middle, and having rather narrow integumental plications, there being about twelve to one-eighth of an inch. Deltoids visible externally. Genital openings as in all true Pentremites. This species was first described by Meek, but merely in a foot note, comparing it with Pentremites koninchiana = conoideus Hall. It differs from Pentremites conoideus in being more obtuse, with broader and more deeply excavated ambu- lacra than Pentremites conoideus, in which the ambulacra are narrow, more rounded, and the surface plications coarser. The interambulacral spaces are depressed more in Pentremites conoideus than in this species. It differs from Pentremites godoni in being not as round, with more depressed ambulacra, and in not having the sharp crest-like margin around the sinus. Geological formation and locality : Subcarboniferous on the Divide between Ross Fork and Lincoln Valley, Montana. First mentioned in F. V. Hay den's Sixth Annual Report of the United States Geological Survey of the Territories, 1872, p. 470. Types in the Smithsonian Collection, numbered 24,529. Pentremites serratus n. s. Plate IV., Fig. 9. Body rol)ust and resembling Pentremites sulcatus very much. Base flat and disk-like, showing a distinctly triangular depres- sion around the articulation surface of the column. Ambu- Hambach — Revision of the Blastoideae. 57 lacra concave, broad, leaf-like, and sunk so that the surface does not reach the upper margin of the sinus. Interambu- lacral area not so depressed as in Pentremites sulcatus, with a very prominent and coarsely serrated margin at each side of ambulacrum from the base of the sinus to the deltoid suture. External deltoid surface rather convex, smooth, with a sharp prominent base point, projecting much over the summit. Whole surface finely striated. Poral pieces 9 to ^ inch. Genital openings as in Peniremites sulcatus. All my specimens vary from ^ to 1^ inches in diameter. Transverse diameter one-fourth orreater than the vertical diameter. The serrated edge of each side of the ambulacrum distinguishes this species readily from Peniremites sulcatus^ its nearest ally. The geological formation is the Chester limestone, but I have never found it at Chester or Evansville, Illinois, or around there. It occurs at Ste. Genevieve, Missouri, and at Baldwin, Illinois. Cribeoblastus incisus n. s. Plate v., Fig. 2. Body globose, of medium size, seldom more than f inch in diameter. Base very small, depressed, not visible in a lateral view. Ambulacrum narrow, linear, running almost over the whole surface of the body. Deltoid pieces very small, visible externally, but entirely confined to the summit. Interambulacral area convex and granulated, with a deep suture in the center and a luuary impression at each side of the ambulacral margin, dividing each side of the ambulacral sinus in two ; and a little spine-like projection at the apex of the sinus readily distinguishes it from G . melo and other allied forms. Genital openings very small but not confluent with each other. Geological formation and locality: Lower Burlington lime- stone, Burlington, Iowa. 58 Trans. Acad. Sci. of St. Loxds. CiDAROBLASTUS PARVUS n. S. Plate v., Fig. 1. Body ovoidal, a little wider at the summit than at the base. Base very small and depressed, but not as much as in the typical specimen of this genus. Ambulacrum narrow and linear, running almost over the whole surface of the body. Fork pieces broad, occupying a little more than half the vertical height of the calyx, with an elongated depression in the center of the interambulacrum where two of them join. Deltoid very broad, occupying nearly half the interambulac- rum, covered with small granules, arranged in regular trans- verse rows, for the reception of little spines. Genital openings very small, not confluent. Of this unique species I have several silicious casts, as well as the surrounding molds, which show distinctly the fine spines adhering to them. All the specimens are of a cherty nature and on the whole not as well preserved as most other specimens, but, nevertheless, showing all the above described characters very distinctly. Geological formation and locality : In cherty rock of the St. Louis age, in southwestern Missouri. Cribroblastus verrucosus n. s. Plate v., Fig. 3. General form of body globose, vertical and transverse diameters equal. Basals very small and almost concealed by the column, or extending very little beyond it. Ambulacra narrow and linear, running almost over the whole surface of the body. Fork pieces very short occupying hardly one- fourth of the vertical diameter of the body with a very dis- tinctly depressed suture. Deltoids very broad, occupying fully three-fourths of the vertical length of the body, separa- ted from the upper fork piece suture by a double linear de- pression. The whole interambulacral space is rounded and ornamented by coarse granulation very irregularly arranged. Hamhach — Revision of the Blastoideae. 59 This species is easily separated from its nearest relatives, as Cribroblastus sayi (^Pentremites sayi of Shumard), by its coarse granular surface. Of this nice unique Blastoid I possess only a silicious cast and mould though sufficiently preserved to recognize its distinction from similar species. Geological formation and locality : It was discovered in a cherty rock of the Burlington formation at Allenton, St. Louis County, Mo. Cribroblastus tenuistriatus n. s. Plate v., Fig. 16. Body small and oval in outline, being a little wider at the summit than at the base. Basals very small but visible in a lateral view. Ambulacra narrow and linear, not extending over the whole surface of the body, occupying only three- fourths of its entire length. Deltoids about one-third of the whole length, the whole interambulacral space rounded and with a lancet-shaped longitudinally striated elevation extending from the base to the apex of the deltoid whereas the deltoid, surface and the surface at both sides of the lancet-shaped elevation are ornamented with little granules arrans-ed in a dis- tinctly transverse manner. Genital openings very small and formed by the junction of the deltoid and lancet piece. Ver- tical diameter one-third greater than the transverse. Whole length of the specimen -^\ of an inch, width -^^ inch. Geological position and locality : In the Burlington lime- stone. Cooper County, Missouri. Cribroblastus schucherti n. s. Plate v., Fig. 8, 8a. Body globose, about as broad as long. It is one of the smallest species known. Basal portion very small and de- pressed. Fork pieces narrow, with a narrow sinus for the reception of the ambulacrum extending almost the whole 60 Trans. Acad. Sci. of St. Louis. length of the piece. Margins of the sinus drawn out to form a prominent crest on both sides of the ambulacrum, thus causing the interambulacral space to be slightly concave. Deltoids small, the upper portion running out to a small projecting spine. Summit openings, ^. e., mouth, anus and genital openings, twelve in number and not confluent. This species, which resembles C. cormitus Meek and Wor- then, differs from it, however, in the following characters : The base is not depressed as much, the margins of the ambu- lacral sini are less prominent, and the interambulacral spaces are not excavated as much as in C. cormdus. The interam- bulacra are twice as wide as in C . cornutus, in which species the interambulacra are about as wide as the ambulacra. The spiny projection is not as long or as prominent as in C. cornutus. Besides the f oregoins: differences the surface orna- mentation is different in the two species, being granular in C. coriiutuSy and finely striated in the species under consider- ation. Geological formation and locality : Subcarboniferous. Divide between Koss Fork and Lincoln Valley, Montana. The specimens were collected by Hay den's party, and first mentioned in the Annual Report for 1872, page 470, un- der the name Pentremites bradleyi. Meek. Types in the Smithsonian Collection, numbered 24,529. By close exami- nation it was found that the specimens under this number con- sisted of two different species, one of these I have here named in honor of mv friend, C. Schuchert. Saccoblastus vextricosus, n. s. Plate IV., Fig. 7. Body bipyramidal. Base cup-shaped, with three charac- teristic impressions peculiar to this genus. Articulation sur- face of the column triangular. Column triansfular. Ambu- lacrum very narrow, linear and sunk into the very prominent ambulacral sinus. Interambulacrum smooth and dipping a little toward the fork piece suture. Genital openings near Hamhach — Revision of the Blastoideae. 61 the summit, not confluent, the oblique opening giving a slit- like appearance to them. Anal opening ^ inch below the summit. Poral openings 11 to ^ inch. The greatest trans- verse diameter is at the apex of the ambulacrum, which is about f below the summit. Vertical diameter f and the transverse diameter about f of an inch. Geological formation and locality: Warsaw limestone, Boonville, Missouri. Globoblastus magnificus n. s. Plate III,, Fig. 5. This specimen, although only a silicious cast, differs so much from all other known species, that I am thoroughly convinced of its specific value. It is nearly twice as large as an ordinary G. noriooodi, from which it is readily separated by the fol- lowing characteristics. The base, though small, is not depressed, as in G. norwoodi. Fork pieces resemble those of G. norivoodi, but are larger and reach nearly to the summit of the calyx. The sinus of the ambulacrum is very narrow, extending, as in G. norwoodi, nearly the whole length of the ambulacrum. Deltoids, to judge by the impressions of the suture mark- ings, are perforated as in G. norivoodi. This is shown plainly on a small part of a deltoid piece remaining in the cast, which leaves no doubt as to its generic affinities. Interambu- lacral spaces seem to be more rounded and convex than in G. norwoodi. External ornamentation not known. Ambu- lacra narrow and seemingly extending over the whole surface as in the true noi^woodi. The main differences, beside the size, between this species and G. norwoodi, are the shallow depression or almost flat basal plates and the more rounded interambulacral spaces, and, probably, a different external ornamentation . Geological formation and locality : In a chert rock be- longing to the same age as the Burlington limestone, in the southwestern portion of Missouri, near the Arkansas boun- dary line. Height of specimen, 1^ inch. Width, 1 inch. 62 Trans. Acad. Sci. of St. Louis. Globoblastus ornatus n. s. Plate v., Fig. 4. Body elliptical, longer than wide. Basals very small and depressed. Ambulacrum narrow and linear, extending the whole length of the body. Interambulacral space slightly rounded, wider in the center than near the base where it is rather depressed with little spine-like projections at the base of the sinus for the apex of the ambulacrum. The whole interambulacral space has an outer granulated margin, where- as the inner surface is ornamented by granulations shaped like an elongated spear head. Deltoids very small, with a horn-like projection above the summit and perforated in the center. This species is also easily recognized b}^ the orna- mentation of its interambulacrum. Geological position and locality : It occurs in the Burling- ton limestone at various places in Missouri. Globoblastus spathatus n. s. Plate v., Fig. 5. Body globose, resembling somewhat G. norwoodi in out- line. Vertical and transverse diameters equal. Ambulac- rum narrow and linear extending over the whole length of the body. Interambulacral space flat, ornamented at the outer margin by a row of granulations running down on each side of the fork piece sutures, giving in this manner a double row of granules in the center of each interambulacrum. Each interambulacral half so marked is ornamented by gran- ulations in the form of a spatula. Deltoids small and protu- berant, perforated in the center. The peculiar ornamenta- tion of the interambulacral space is sufficient to separate it at once from allied forms. Geological position and locality: It occurs in the Bur- lington limestone at Allenton, St. Louis County, Missouri. Hambach — Revision of the Blastoideae. 63 Cribroblastus tenuis n. s. Plate v., F;g. 17, 17a. Body small, cylindrical, about twice as long as wide. Am- bulacra extending almost over the whole surface of the body. Interambulacra rather convex with a marked crest in the cen- ter. The sutures where the forkpieces meet present a fine furrow as well as the sutures between the fork and deltoid pieces, whose external surface is finely granulated and occupies about one-fifth of the entire length of the body. The rest of the interambulacrum is transversely striated at both sides of the central crest. Genital openings very small, and not con- fluent. Basal part small and flat, visible externally only the thickness of the shell. It is easily distinguished from Cribroblastus roemeri and samjpsoni by its more slender form and by the external orna- mentation. Geological position and locality : Chouteau limestone, Pet- tis County, Missouri. Induced by the sweeping statement of Mr. F. A. Bather, I give the following list, comparing the Blastoids in my collection with those of the British Museum. Accordino- to Mr. Bather's statement, p. x.. Introduction to his Cata- logue, the collection contained then (1899) 1,223 specimens. Quoting his remarks : " These figures speak for themselves. However numerous may be the specimens of Blastoidea in other museums, there can scarcely be any collection so repre- sentative of the class as a whole or as rich in specimens of the highest scientific importance as is that of the British Museum." This is a strong expression, especially since Mr. Bather has not seen all collections. Considering that America contains the bulk of the material, although admitting that the British Museum has the very valuable collections of Gilbertson, I. Rofe and L. G. de Koninck of unique specimens, I venture to say that our American material is on the whole better pre- served than that found in Europe, and being confident that the American collectors did not send their best specimens across 64 Trans. Acad. Sci. of St. Louis. the water, it is not very doubtful to say that, for the study of this particular class of fossils, the best material is found on this side of the water. Comparing the figures of the British collection with mv own, shows at a glance on which side the most material is to be found. Aside from this, my collection, which was brought together in fifty years, and comprises about ten thousand specimens, contains a number of real scientific specimens (pathologic and abnormal developments and specimens illustrating mor- phology) hardly to be found in any other collection. A student could learn more on a dozen or two picked specimens from our material than from the whole collection of Gilbert- son, Rofe or de Koninck. Besides specimens illustrating the morphology, my collection contains considerably over one hundred pathologic and abnormal specimens. I give the names as arranged in Bather's Catalogue, and an asterisk denotes the type specimen. Br. M. stands for Briiish Museum and H. for Hambach. Br. M. H. Codaster acutus o o •' canadensis o " gracilis o o * " kentuckyensis o " pulchellus o * " pyramidatus o o " trilobatus o o *Codonite3 campanulatus o o ' ' conicus • " fusiformis o o " gracilis o " stelliformls o o ♦Cryptoblastus kirkwoodensis. o '■ melo o o " pisum o «« projectus o Cryptoschisma schulzi o o Eleutherocrinus cassedayi o o Granatocrinus cornutus o f ' curtus o '' campanulatus.. o " derbiensis o o " ellipticus o o ••' exiguus '. o Hambach — Revision of the Blastoideae. 65 Br. M. H. Granatocrinus glaber o •' granulatus o " maccoyi o *' norwoodi o o " orbicularis o * (I roemeri. Heteroblastus cumberlandi o Mesoblastus angulatus o " crenulatus o " elonsatus »^ o " rofei 0 " shumardi o " sowerbyi o Metablastus bipyramidalis o " cottaldi o " hispanicus o " lineatus o o " varsouviensis o o " wachsrautlii o " wortheni o o Nucleocrinus angularis o o " elegans o o •' greenei o " Incina o " meloniformis o " obovatus o o /M, FiLASTOIDEAE . Plate 111. From specimens in tiie author's collection, unless otherwise stated. 1. Cidaroblastiis grannlaris, — loaned by G. K. Green. 2. Lateral view of same species, — Troost Collection, Smithsonian Institu- tion, No. 33080. 3. Summit view of same. 4. Cidaroblastus glohosus, — Troost Collection, Smithsonian Institution^ No. 38077. 5. Globoblastus magnificus. 6. 7. Lateral and basal views of Pentremites sulcatus, showing an elongated piece inserted between two fork pieces. 8, 9. Pentremites pyriformis, showing an undeveloped fork piece and ambulacrum. 10. Pentremites sidcatus, showing a crippled ambulacrum. 11, 12. Pentremites sulcatus, with only four ambulacra developed and a fifth fork piece solid. 13, 14. Pentremites snlcatus, with only four ambulacra. 15, 16. Pentremites pyriformis, with six fork pieces but only four ambu- lacra developed. 17. Saccoblastus, with live fork pieces but six ambulacra, of which two occupy one sinus. 18. Pentremites godoni, with four fork pieces but with five ambulacra, of which two occupy one sinus. Trans. Acad. Sci. OF St Louis, Vol. XIII. Plate . ill . G.HdKibach ad nat, de: LithWeniei-4Vfinter,?iaiikfor(°/M. BLASTOIDEAE. Platk IV. From specimens iu the author's collection. 1. Saccoblastus woodmani, lateral view. 2. Same, base view. 3. Saccoblastus obliquatus, lateral view. 4. Same, base view. 5. Saccoblastus wortheni, lateral view. 6. Saccoblastus pyramidalis, lateral view. 7. Saccoblastus ventricosus, n. s., latei'al view. 8. Saccoblastus lineatus, lateral view. This row of figures shows the gradual development from one species to the other. 9. Pentremites serratus, from Ste. Genevieve, Mo. 10. II. Pentremites t^dipaformis, n. s., lateral and basal views. TIJANS.ACAD. SCI. OFST. LOUIS, VOL.XIII . PL.\TE I\'. 1_ ro *■ «o 03 -id nat.del. Ln'ii Werner (Winter, praKkfon °K . BLASTOIDEAE. Plate V. From specimens iu the author's collection, unless otherwise noted. 1. Cidaroblastus parvus, n. s., showing one interambulacrum. 2. Cribroblastus incisus, n. s. 3. CrihrobJastus verrucosus, u. s., showing the interambulacrum. 4. Globoblastus ornatus, n. s., showing iuterambulacral space. 5. Interambulacrum of Globoblastus spatatus, n. s. 6. PentremUes turbinatus, n. s., lateral view. 7. Pentremites b7-adleyi Meek. — from specimen iu the Smithsonian Insti- tution. 8. Cribroblastus schucherti, n. s., magnified, — from specimen in the Smith- sonian Institution. 8a. The same specimen, natural size. 9. Interambulacrum of Cribroblastus sanipsoni. 10. Interambulacrum of Cribroblastus Itoemeri. 11. Iuterambulacral space of Cribroblastus neglectus. 12. Iuterambulacral space of Cribroblastus gramilosus. 13. Interambulacrum of Cribroblastus jyisitm. 14. Cribroblastus sayi, — from Shumard's type specimen. 15. Outline of Cribroblastus potteri. 16. Cribroblastus tenuistriatrts, n. s. 17. Interambulacrum of Cribroblastus tenuis, n. s. 17a. Outline of specimen, natural size. 18. Pentremites kirki, n. s., lateral view, — from specimen in the collection of Mr. Kirk. TptANS.ACAD.SCl.OF ST. Lol'lS. \'0L.X111. Plate \' G/Hambac'h ad nat del Lil>i.Wen>ertWinter,pranl: 1,3,4,7, 9 2,5,8 6 25 cts. each. 50 cts. each, §1.25 3.75 3.60 101 9 2, i, 5, 10 1 3, 6, 7, 8, 11 10 cts. 25 cts. each. 40 cts. 50 cts. each. 8.75 3.50 lit 2,3 5-^, 10, 11 1 4 9 15 cts. each. 25 ctg. each. 45 cts. 75 cts. 1.00 3.75 3.50 is: 1,9,10 5 3,8 2, 4, 6, 7 25 cts. each. 30 cts. 35 cts. each. 50 cts. each. 3.75 3.50 MEMOIRS (in quarto). Contributions to the archaeology of Missouri, by the Archaeological Section. Parti. Pottery. 1880. 02.00. The total eclipse of the .sun, January 1, 1889. A report of the observations iTiade by the Washington Universitv Eclipse Party, at Norman, Califor- iiia. 1891. $2.00. * Supply exhausted. t Can be sold oiJy to pnrchasers of the entire volume,— so far as this can be ^^upplicd. t Each number is a brochure containing one complete paper (or rarely two). Transactions of The Academy of Science of St. Louis. VOL. XIII. No. 2. ON THE PEEDETERMINATION OF THE SPEED OF THE TROTTING HORSE. FRANGIS E. NIPHER. Issued July 9, 1903. ON THE PEEDETEEMINATION OF THE SPEED OF THE TROTTING HORSE. Francis E. Nipher. In a paper published in 1883 in the Transactions of The Academy of Science of St. Louis, the writer gave a discussion of numerical data covering the performance of all trotting horses making public records, between the years 1843 and 1883. The equation which gives the speed of the best horse at any date as function of the time, counted from any assumed date, was then published. It was found that the speed of the horse was approaching a limit, which was ap- proximately that of the running horse. The limiting speed indicated by the data was 1:38, or 98 seconds to the mile. This was somewhat below the speed of the running horse, on an oval track, and it is evident that a limit of 100 seconds to the mile will also fit the observations in a very satisfactory way. The equation published in 1883 was — kt s^ a -{- b Here s is the speed, in seconds per mile, t years after any assumed date. At this assumed date t = 0,and s =a + b. It is evident that a is the limiting speed reached in an infinite time, and that b is the difference between the limiting speed, and the speed at the assumed zero date. Mr. W. H. Pickering offered some criticisms on the method of obtaining the constants in the above equation, as it ap- peared in a preliminary form,* and in an appendix to the paper in the Transactions,! a slightly different method was- employed. The constants so determined were — 0.0127< 5 = 98 + 43.56 or log (s— 98) =1.637 — 0.0055^ ♦ American Journal of Science. III. 26 : 20-24. July, 1883. t Trans. Acad, of Science of St. Louis. Vol. IV. No. 3, pp. 514-5. 1883, (69) 70 Trans. Acad. Sci. of St. Louis. where t is measured in years from 1860. According to this equation the speed of the trotting horse in 1903 would be obtained by making t = 43. The value so com- puted is s = 123.1 or two minutes and three seconds per mile (2:03). The date when the two-minute horse will appear is found by making s = 120. The corresponding value of t is 54. The date is therefore 1860 + 54=1914. These two results do not at present seem very far from the mark. If in the above equation s be made 180, the date when the three-minute horse appeared is found to correspond to ^ = — 50. The date is 1810. As a matter of fact the date when the three-minute horse appeared was, as I am informed, 1818, in response to a bet of a thousand dollars that no such horse could be produced. Nearly all of the fast trotters belong to a few families. A very large per cent, have descended from Rysdyk's Haynhle- toniati, foaled 1849, and Mamhrino Chief, foaled 1844, both of whom were descended from the thoroughbred Mamhrino. It would therefore be unreasonable to expect a very close agree- ment between observed speeds, of a century ago, and those computed from the above formula. If in the equation, s be made 99, the time when the horse will have reached within one second of his limiting speed, is found to be 298 vears after 1860. The data from which the above equation was deduced were published in the American Journal of Science for April, 1883, by Professor Brewer, of Yale. The data covered all known official trotting records between the dates 1843 and 1883. From 1854 to the present time the speed of the trotter has increased from s = 145 to s = 123. This is a change of 22 seconds in the time of trottino^ a mile. Accordino; to the equation as shown above, it will take 255 years, or until the year 2158 to change the speed by 24 seconds more. In all time thereafter, the speed will be practically constant, as the «peed of the running horse is now. In 1892 when JSfancy Hanks lowered the trotting record, the writer applied the above equation to her standard track Nipher — Predetermination of Speed of Trotting Horse. 71 record as published at that time, and covering the four years 1889 to 1892 inclusive. Estimating t in years from 1889, the equation for her performance was found to be — C.693< s= 124.5 + 20. Oe The constants in this equation were computed from the observed and published values reproduced in columns one, two and three of the followino- table. Column four shows the corresponding values of s computed from the last equation. The agreement between observed and computed values could not be more precise. NANCY HANKS. STANDARD TRACK RECORDS. t Date. s Obs. s. Calc. Diffs. 0 1889 144.5 144.5 0.0 1 1890 134.5 134.5 0.0 2 1891 129.5 129.5 0.0 3 1892 127.25 127.0 0.25 4 1893 125.7 — 5 1894 125.1 . — OD 124.5 — The computed speeds for the years 1893 and 1894 are also given, and the limiting speed which this horse would make after an infinite time (if she could have continued to train indefinitely) is also given at the bottom of column four. It will be seen that this horse must have reached within one second of her own possible speed during 1893. In about four years the speed of this horse changed 19 seconds and came within one second of the final speed possible, even if this horse had been immortal and could have continued the pro- cess forever.* * In September, 1892, this horse trotted a mile in 2:04, but this record was made with the newly adopted 28-inch wheel, with pneumatic tire and ball bearings. It is thought that this diminishes the time by about three seconds. I also find on examination that the record 2:07.25 in the table above was made with the same running gear. This makes the record for that year of less weight, in discussing the records of this particular horse. 72 Trans, Acad. Sci. of St. Louis. In 1865 Goldsmith Maid began her career as a trotter, at the age of eight years. In the nine years which followed, her speed steadilj^ increased, and is represented by the equation — 0.193< 5= 131.0 4- 13. 5e Her track record for this period is given in the following table, and the speed computed from the last equation is given in the fourth column of the table. GOLDSMITH MAID. STANDARD TRACK RECORDS. t Date. s Obs. s Calc. DifEs. 0 1865 146.0 151.0 + 5.0 3 1868 141.5 142.2 + 0.7 4 1869 140.5 140.2 — 0.3 6 1871 137.0 137.2 + 0.2 7 1872 136.75 136.2 — 0.5 9 1874 134.0 134.5 + 0.5 Another horse, American Girl, 1862, began her track record in 1867, and reached her best speed in 1874. Her change in speed is represented by the equation s= 136.4 + 14.46e - 0.707< AMERICAN GIRL. STANDARD TRACK RECORDS. t Date. s Obs. s Calc. Diffs. 0 1867 152.5 150.90 — 1.60 1 1868 144.0 143.53 — 0.47 2 1869 139.0 139.92 + 0.92 4 1871 137.25 136.86 — 0.39 7 1874 136.5 137.43 + 0.93 The last record that will be given is that of Judge Ful- lerton, 1865, whose track record covers the years 1871-5 in- clusive. Nipher — Predetermination of Speed of Trotting Horse. 73 His performance is represented by the equation — 0.518< 5 = 137 + 7.94e A comparison of observed and computed values follows : — JUDGE FULLERTON. STANDARD TRACK RECORDS. t Date. s Obs. s Calc. DifEs. 0 1871 145.25 144.94 — 0.31 1 1872 141.75 141.73 — 0.02 2 1873 139.25 139.82 + 0.57 3 1874 139.00 138.68 — 0.32 4 1875 138.00 138.00 0.00 It is evident that a slight change in the values of the con- stants, would in some cases make the agreement between observed and computed values somewhat closer. They are, however, very satisfactory, when we consider that the owners and drivers of these horses were not primarily seeking to secure accurate data for this discussion. It is evident also that the trainer's record would afford much more satisfactory material for a discussion of the subject, than can be realized in the track records. A record of three or four years might be expected to give a very fair idea of the future record of a horse . In the original paper the date when any given speed orig- inated, was obtained from the data of Brewer's table, by a discussion of the subsequent increase in the number of horses capable of that speed. For example in 1859 there was one horse who could trot a mile in 2: 23 or better. In the next year there were two. Ten years later there were sixteen, and in 1882 there were 275. When these numbers were platted on a time axis, a logarithmic curve resulted. When the logarithm of the number of horses was similarly platted, a straight line was obtained. This straight line intersected the time axis at the date 1857, instead of 1859. This date for the origin of the speed 2 : 23 was considered much more weighty, than the date when some trotting match revealed 74 Trans. Acad. Sci. of iSt. Louis. the fact that the first horse capable of making this speed had already appeared. Horses who are by their owners known to be capable of breaking the record, are much more likely to be held back for advantageous conditions, than a horse of the same class would be after this speed has become a common one. The effect of ball bearings, the pneumatic tire and the 28- inch wheel was to produce a sudden change in speed in 1892, but this is an effect that must and should be considered a part of the problem. The old high-wheeled sulky was also con- tinually being improved, between 1850 and 1890. The inter- esting fact remains that the record to-day is within a second of that predicted twenty years ago. The results here given also seem to be sufficient to estab- lish another confirmation of a general principle of evolution. It would seem that each horse goes through during the few years of its track life, the same kind of evolution that its race goes through during the centuries. The same equation which represents the result of training the individual horse, represents also the supreme result of selection, breeding and training of the family. Just as this paper is going to press, the world's record of the running horse has been lowered by Alan-a-Dale, to s=^ 97.6 (1: 37.6). This, in connection with the well-known record of Legal Tender in 1865 and of Ten Broeck in 1887, will give the basis for a fair determination of the final limit of the running horse. The observed speeds are given in the following table : — THE RUNNING HORSE. OVAL TRACK. t Date. s Obs. 8 Calc. DifCs. 0 1865 104.0 104.0 0.0 22 1887 99.75 99.76 0.0 38 1903 97.6 97.6 0.0 The values of speed in the fourth column are computed from the equation log (s — 91.5)= 1.097 — 0.0082^ or s = 91.5 + 12. 5e -G.0189* Nipher — Predetermination of Speed of Trotting Horse. 75 The differences between observed and computed values are certainly inside of the errors of observation. Only the three observations above given are known to me, but they are so far apart in time that they certainly give a fairly good deter- mination. According to this equation, the limiting speed of the running horse on a standard track is 91.5 seconds to the mile (1 :31.5). The speed of 1:32.5 will be reached when ( = 134. This date is therefore ninety-six years from the present time. At this date, or in A. D. 1999, the running horse will be within one second of his final speed. The change in the time of running a mile during the next century will therefore be about six seconds. This result is something of a surprise. A previous knowledge of it would have caused me to somewhat modify certain passages in the present paper. From the previous equations it will be seen that at the present time, the annual change in the time required to make one mile on a standard track, is for the running horse 0.12 sec, andfor the trottins; horse 0.29 sec. o Issued July 9, 1903. PUBLICATIONS. The following publications of the Academy are ofEered for sale at the net prices indicated. Applications should be addressed to The Librarian, The Academy of Science of St. Louis, St. Louis, Mo. TRANSACTIONS (in octavo). Vol. Number. Price per number. Price per vol. Price in set. 1* 2t 3,4 $7.50 (Nos. 2-4 only.) 1 #4,00 2.00 each. #7.00 (Nos. 2-4 only.) 2 1 to 3 2.00 each. 5.50 5.00 3 1 tod 2.00 each. 7.50 7.00 4 1 to 4 2.00 each. 7.50 7.00 5 1-2, 3-4 1 4.00 each, (donljle unmbers) 7.50 7.00 et 1, 2, 6, 8, 10, 11. 16, 17 4, 6, '7, 13, 14, 15, 18 3,9 12 1 25 cts. each. i 50 cts. each. 75 cts, each. ■fl.CO 7.50 7.00 7t 2, 3, 4, 6, 7, 8, 13, 16, IG, 18, 19 5, 9 to 12, 14, 20 17 1 I 25 cts. each. • \ 50 cts. each. 75 cts. #1.00 7.50 7.00 8t 1, 3 to 6 8, 10, 12 2, 7, 9, 11 I 25 cts. each. 50 cts. each. 3.75 3.50 ot 1, 3, 4, 7, 9 2, 5, 8 6 25 cts. each. 50 cts, each. $1.25 3.75 3,50 lot 9 2, 4, 5, 10 1 3, 6, 7,8,11 10 cts. 25 cts. each. 40 cts. 50 cts. each. 3.75 3.50 lit 2,3 i>-8, 10, 11 1 4 9 15 cts. each. 2 5 cts. each. 45 cts. 75 cts. 1.00 3.75 4 3.50 12t 1, 9, 10 5 3,8 2.4,6,7 2'} cts. each. 30 cts. 35 cts. each. CO cts. each. 1 ! 3.75 3.50 MEMOIRS (in quarto). Contributions to the archaeology of Missouri, by the Archaeological Section. Parti. Pottery. 1880. $2.00. The total eclipse of the sun, January 1, 1889. A report of the obseiTations made by the T^ashington University Eclipse Party, at Norman, Califor- nia. ISri. #2.00. * Supply exhaUEtedi t Can be sold only to purchasers of tbe entire volume,— so far as this can be Eupplied. J Each number Ic a brochure containing one complete paper (or rarely tvvo). Transactions of The Academy of Science of St. Louis. VOL. XIII. No. 3. SECOND CONTRIBUTION TO THE HERPETOLOGY OF MISSOURI. JULIUS HURTER. Issued July 31 , 1903. SECOND CONTKIBUTION TO THE HERPETOLOGY OF MISSOURI.* Julius Hurter. In 1897 I had the honor to report on a number of reptiles and batrachians that I had ascertained to occur in the State of Missouri, and this evening I am able to add nineteen new species not before found nor reported for the State. But before I proceed let me give you an idea of the difficulty in finding co-workers in my line of collecting. Prof. H. M. Whelpley, editor of the Meyer Brother's' Druggist, had the kindness to distribute with that periodical a circular, asking for assistance in collecting and sending in specimens from their respective counties. This circular reached about 1,300 druggists in the State of Missouri, and in response to it I received fifteen answers from persons that would like to help ; but to my great regret I found out that even they were more interested from a financial than from a scientific standpoint. This gives an idea how difficult it is to get assistance from outside parties in this particular branch of study. Still, I am under obligations to the following gentlemen who offered their services and procured me a good deal of material from their respective counties, viz.: J. H. Black, Esq., Newton County; J. C. Miles, Jasper County; J. M. Parker, Mont- gomery County; Prof. R. R. Rowley, Pike County; Fuller Smith, Clark County; Robt. Lotze, Oregon County; Dr. A. Schaffraneck, St. Charles County ; George Miller of our city, who brought in quite a number of specimens from Stoddard County; also Mr. H. N. Force, Ozark County; Dr. J. R. Terry who collected in Adair County, and W. K. Smith, Crawford County. All of these gentlemen brought in valuable additions, which are mentioned in their proper places. The increase over my previous list consists of nineteen species as before mentioned, viz., six batrachia and thirteen reptilia. * Presented to The Academy of Science of St. Louis, January 5, 1903. (77) 78 Trans. Acad. Sci. of St. Louis. Class BATRACHIA. Order Urodela. The Tailed Batrachians. 1. Amblystoma punctatum, L. — The spotted salamander. This salamander when alive is one of our prettiest speci- mens, being of a dark bluish-black color with a number of yellowish-white shining spots on the back and abruptly light olivaceous underneath. The legs are of the color of the under parts, not of the upper. This animal is one of those that uses its tail as an organ of prehension. When taken up and held so that it expects to be dropped, it is its habit to take a hold of some support with the tail and if one is not found at once, the tail is moved about in search of an object that might answer this purpose. It is mostly found under decaying logs in damp shady places, but is in no way plentiful : — Drake, St. Louis County, April 24; Butler County, April 16 and July 17; Stoddard Countv, October 26. 2. Hemidactylium scutatum, Tschudi. — The scaly sala- mander. This is a small species. I copy the description from Cope's " Batrachia of North America," as one of the best: Back, dark chestnut, but above much lighter, both sprinkled with black, the latter more especially along the dorsal line. Snout above, eyes above and in certain lights the furrows above the lateral longitudinal lines light chestnut approaching to golden bronze, faintly clouded in spots with darker. Sides of body finely mottled brown and bluish-white. Head, body, and tail below, chalk white with a tinge of blue. Spar- ingly and irregularly marked with rather large black spots ; spots disposed along sides and the white of tail beneath. Central tract unspotted. One or two furrows or constrictions 20 entirely around the tail behind the vent, marking the narrow base of the tail, which then swells abruptly in many speci- mens. Neither the late Professor Cope nor the museum catalogue Hurler — Ilerpetology of Missouri. 79 of the Smithsonian mentions the animal as being ever caught west of the Mississippi. I am under obligations to my friend Dr. George W. Bock, who found one specimen near Bourbon, Crawford County, October 15, 1899, and presented it to me. 3. Spelerpes maculicaudus Cope. — The western cave sala- mander. In 1880 Professor E. D. Cope described this as a new sala- mander from a spring at Brookville, Indiana. This species has since been found to be the common cave salamander of the Mississippi Valley along with Spelerpes longicaudus. It is similar in build to the cave salamander, Spelerpes longicau- dus and also to the next species, the newly discovered Speler- pes stejnegeri, but differs in color. All the specimens, old or young, are of a Chinese orange color in life and have the back and sides of the body, tail and limbs covered with sharply defined irregular rounded and elongated spots. It is a twilight species. So far I have only found it in Jefferson County, in a small ravine, but it has been found also by other collectors at the mouth of Fisher's cave near Springfield, Green County ; near Marble cave. Stone County; Rockhouse cave, Barry County; and Wilson's cave, near Sarcoxie, in Jasper County. 4. Spelerpes stejnegeri, Eigenmann. The latest discovered species. I have not yet seen this species and therefore have to give the description from its discoverer, Professor Eigenmann : — The back is raw sienna with many spots, coalescing in places and irregularly arranged in two series on each side of the median line. The median line and a streak from the eye back to above the hind limbs are free from spots. Sides dark brown with irregular dots of marbling of sienna. The belly is clear. This salamander has been found in Rockhouse cave, Barry County; near Marble cave, Stone County; Wilson's cave, Jasper County ; and Fisher's cave. Green County : all in south- western Missouri. 80 Trans. Acad. Sci. of St. Louis. 5. Typhlotriton Spelaeus Steju. — Blind cave salamander of Missouri. The first specimen of this salamander was collected by F. A. Sampson, of Sedalia, inEockhouse cave, Barry County, and described by Dr. L. Stejneger of the National Museum. Afterwards Professor E. D. Cope found some in Marble cave. Stone County. It is rather a rare species. The color in life is pale flesh color. I have not yet been able to secure a specimen for my collection. Order Salientia. The Frogs. 1. AcRis GRYLLUS Le Conte. — The cricket frog. I include it in my list because it is mentioned in Cope and Yarrow's list as No. 35601 of the Smithsonian collections: — six specimens from New Madrid County, collected by R. Kennicott, one of the pioneer collectors. The best character to distinguish this frog from its west- ern representative, Acris gryllus crepitans, is that in the former when the hind limb is carried forward along the side of the body, the tibio-tarsal articulation reaches to the tip of the snout or a little beyond, whereas in crepitans the same articu- lation hardly reaches to the tip of the snout. Also, Acris gryllus is the longer one of the two, measuring lyV inch, where ct^epitans reaches only 1^ to 1^ in. in length of body. Class REPTILIA. Order Chelonia. The Turtles. 1. Chrysemys margin ATA Agassiz. C. cinerea Brown. A so-called painted turtle from the lively red markings on the edge of the carapace. This turtle is common in the low- lands across the Mississippi, in Illinois. Some specimens are found in the back-waters of this river on the Missouri side. The plastron in the adult is usually all blood red, hiding a Hurler — Herpetology of Missouri. 81 large dull black mark that extends from near the gula on the center of the belly to the anals without any lateral branches as in Chrysemys hellii. The young are very differ- ent in the marking of the plastron from Chrysemys mar- ginata of Indiana, Eastern Illinois, and Michigan. The shields of the plastron are alternately red and yellowish-white on each side of a dark center streak. This turtle is called bv the fishermen "Eed belly " and with right, as in spring noth- ing of the dark central mark of the plastron can be seen. 2. Chrysemys dorsalis Asjz. This is another rather scarce turtle that I have found in our most southeastern counties in the so-called " sunken lands." It is easily recognizable from a wide reddish streak along the center of the back. So far I have specimens from Butler County, May 1, 1898. 3. PsEUDEMYS TEXANA, Baur. — The Tcxas Cootci. This turtle has gone so far under the name Pseudemys con- cinna, Le Conte. Le Conte says it inhaliits the rivers of Georgia and Carolina. I have never seen it below Augusta on the Savannah or Columbia on the Congaree ; we have therefore to consider specimens from these localities as typical. The species is characterized by its broad and low shell and its small head. Dr. Baur considers Pseudemys texana as the representative of Pseudemys in the southern portion of the country west of the Mississippi: — Texas, Indian Territory, Northern Mexico, Missouri. Professor Agassiz mentions in his mono- graph on turtles some that were collected by Dr. Roy, in Southwestern Missouri. I have received two nice specimens, one from Mr. F. A. Black, from Newton County, and the other from Mr. J. Carroll Miles, from Carthage, Jasper County, where he collected it from the Spring Eiver, which empties into the Neosho, a tributary of the Arkansas River. In 1895, when on a business trip to Paris, Texas, I collected there a very fine specimen, the carapace of which is a good deal higher than of any other I have seen so far. 82 Trans. Acad. Sci. of St. Louis. 4. Aromochelys tristycha Agz. — A musk turtle. About a month ago Mr. H. N, Force, Ph. G., sent me quite a collection of reptiles from Ozark County, and amongst them I found one half-grown specimen of this variety. Professor Louis Agassiz, in his monograph on turtles, 1857, mentions specimens that were sent to him by Mr. G. Stolley from the Osage Kiver, in Missouri. Agassiz writes: "Al- though Ozotheca odorata^ its eastern congener, varies greatly not only in color but even in outline, I have no doubt that this is a distinct species characterized when young by the great prominence of the keels upon the vertebral and costal plates and by numerous dark dots between the scales of the sternum, and when adult by a marked difference in the form of the snout. In Ozotheca odorata the snout is much more prominent on account of the slope of the upper jaw, which extends further back and is therefore less steep than in 0. tristycha, the lower jaw of which is broader below the symphysis than in odorata, and suddenly turned up." Order Squamata. Suborder Sauria. Lizards. Iguanidae. 1. Phrynosoma cornutum Harlan. — Commonly called ' ' horned toad . ' ' Mr. H. Q. Taylor, a resident of St. Louis, informed me that he captured a specimen on the sandy river shore opposite Leavenworth, in Missouri. Through advertising in the papers, I received letters from gentlemen stating that this animal had been caught in the streets of their respective places but all these seem to have been escaped specimens and were thus caught. The only authentic record of this lizard, as occurring in the State, I find in the United States National Museum reports by Dr. E. D. Cope, Crocodilians, Lizards and Snakes of North America, on page 436 under No. 17397-99 : — three specimens collected by C. W. Eichmond in South- western Missouri. Hurter — Herpetology of Missouri. 83 Suborder Ophidia. Snakes. Poisonous Snakes. 1. SiSTRURUS MiLiARius Linn. — Ground rattlesnake. It gives me pleasure to bring to notice another pit viper, that has been caught by my friend Mr. Eob. Lotzein Oregon County. He was not aware that he had killed a poisonous snake. On an inquiry he wrote me that he captured it from under some debris of an old shanty on the slope of a hill. This specimen looks more similar to those from Texas than to some from Alabama and Florida that are in my collection. Harmless Snakes. 2. Farancia abacura Holbrook. — The so-called hoop snake or horn snake. The color of this snake is bluish-black above. On the two outer rows the ground color assumes the shape of vertical bands, from one and a half to two scales broad, leaving an intermediate space from two to three scales wide, which is red in life. Both the red and bluish-black extend on the abdomen, the former being the ground color. The vertical bands of the flanks are confluent on the middle of the abdomen, either directly opposite or alternating. My son Henry collected six specimens near Poplar Bluff, Butler County, April 24. The snake lives near the shores of stagnant waters and is generally found beneath dead logs and other objects. 3. LioPELTis VERNALis DcKay. — The grass snake. The scales of this little snake are smooth. It is dark green above, lighter on the flanks and yellowish-white beneath. I received the only specimen that I have come across from Dr. A. Schaffraneck of St. Charles. The doctor caught it and two others in his garden. I have never encountered this snake in the last twenty years during which I have paid atten- tion to the collecting of reptiles, and I am of the opinion that the Missouri river stops it from coming farther south in this 84 Trans. Acad. Sci. of St. Louis. region. I remember very plainly that about twenty-five years ago I caught and played with about ten or twelve specimens that I found at one spot on the side of a fence in Madison County, Ills. E. Kennicott also reports in the Smithsonian Catalogue, under number 2204, on a specimen that he col- lected in Monroe County, Ills. I think that cultivation has destroyed its haunts and more or less exterminated it. 4. Coluber vulpinus Baird and Girard. — The fox snake. April 22 I found the first specimen of this snake at Dar- denne prairie, St. Charles County. The same day I came across two other dead specimens that somebody had killed and mutilated. Mr. Charles Aldrich sent three specimens to the Smithsonian that he collected in Webster City, Iowa. Cope states that it is distributed over the northwest of the eastern district, not being known from east of Illinois, or south of the Missouri River. This is the most robust species of the genus and reaches as large a size as any. 5. Coluber spiloides, Dumeril and Bibron. Professor Cope in his work " Crocodilians, Lizards and Snakes of North America," mentions on page 843 one speci- men, under No. 5505 of the Smithsonian collections, as col- lected at Independence, Jackson County. The snake is of common occurrence in Texas and Indian Territory and should therefore be in our western counties. I have specimens only from Waco, Texas, in my collection. 6. Coluber guttatus Linnaeus. — The spotted racer. For three years successively I have found a young specimen of this species near Pevely, Jefferson County, and curious to say they were found always under a small rock on the top of a large one, nearly at the same place. Last year my son had the good fortune to capture a fine adult specimen, but this time in the fields, though not far from the first place: — May 15, 1898; May 13, 1900; May 7, 1899; and May 26, 1901; the adult specimen. Hurter — Herpetology of Missouri. 85 7. PiTYOPHis SAYi Schlegel. — The bullsnake. I have heard a good deal about this snake but never had the opportunity to capture one myself, Mr. Carroll Miles of Carthage, Jasper County, has sent me a fine living speci- men. This snake was one of the most vicious snakes that I ever came across, and it may be accounted for, as Mr. Miles wrote me on inquiry that they had it for quite a while in the school where it was always teased to the utmost. This last fall Mr. Frank Schwarz gave me also a fine specimen that had been caught in the bluffs in St. Clair County, Ills., opposite the city of St. Louis. 8. Bascanion constrictor flaviventris Say. — The green racer. From the same place, Jasper County, and from the same gentleman, I received a specimen of this western variety, and a year ago a second specimen from Mr. W. K. Smith of Cuba, Crawford County. The color of the back of this species is olive green, and the whole under-surface greenish-white to bright yellow. 9. Natrix cyclopium Baird and Girard. — Cyclope water- snake. My son Henry found some of these in a small lake near Poplar Bluff, Butler County, May 19 and 22 and October 3, 1897. They are hard to catch as they always seek refuge in the deeper waters. The late Professor Cope gives the following very good description of this snake: Color brown above, yellow below. On the upper surface there are on each side two rows of alternating short crossbars of a darker color, which are about one and one half scales wide, and are separated by in- terspaces of about three scales. The median line for a width of four scales is not spotted, or is very imperfectly so, form- ing a broad vertebral band of a color darker than the general ground. In young specimens the pattern is very distinctly seen ; but in adults the ground becomes so dark as to obscure it very much. The head is uniform brown, the oral edge of 86 Trans. Acad. Set. of St. Louis. the superior labial plates only being yellow. On the yellow ground of the inferior surfaces there appear, on the anterior third only of the length, dark shades on the anterior parts of the gastrosteges. These extend and blend so that on the posterior two-thirds of the length in the adult the color may be said to be blackish-brown with yellow spots. This well marked species is nearest to N'atrix rhomhifera, also found in the State. The present contribution brings the number of Batrachians and Reptiles recorded as found in the State of Missouri to ninety- three, as follows : — 16 Tailed Batrachians. 13 Toads and frogs. 18 Turtles. 7 Lizards. 39 Snakes. I do not doubt whatever that this list will in time reach one hundred and over, as there are quite a number of species of this class in northern Arkansas, Indian Territory and Kansas, that will eventually also be found in the State of Missouri. Issued July 31 , 1903. •(OjW4 i\sivi JO) S9dvd ajeidnioo otto Snraiujtioo aanqoojq b 3v J9