OCEANOGRAPHIC OBSERVATIONS IN WEST COAST FLORIDA WATERS, 1949-52 Marine Biolog ologc cal Laboratory JUN a Mag bof f wots HOLE, MASS, | oscars area SPECIAL SCIENTIFIC pEPORT- FISHERIES No. 149 UNITED STATES DEPARTMENT OF THE INTERIOR FISH AND WILDLIFE SERVICE EXPLANATORY NOTE The series embodies results of investigations, usually of restricted scope, intended to aid or direct management or utilization practices and as guides for administrative or legislative action. it is issued in limited quantities for official use of Federal, State or cooperating agencies and in processed form for economy and to avoid delay in publication. United States Department of the Interior, Douglas McKay, Secretary Fish and Wildlife Service, John L. Farley, Director OCEANOGRAPHIC OBSERVATIONS IN WEST COAST FLORIDA WATERS, 1949-52 By Kenneth T. Marvin U.S. Fish and Wildlife Service Fort Crockett, Galveston, Texas Special Scientific Report: Fisheries No. 149 Washington, D. C. May, 1955 OCEANOGRAPHIC OBSERVATIONS IN WEST COAST FLORIDA WATERS, 1949-52 The swarming of a poisonous plankter, which results in extensive destruction of fish, has been known to occur periegdically off the west coast of Florida since 1844. This fish-killing plague, known popularly as "red tide" be- cause of the simultaneous appearance of large patches and streaks of water of various degrees of discoloration, resulted in much speculation as to its cause. Most theories advanced, as pointed out by Galtsoff (1948), were not supported by evidence. It was not until 1948 that the cause of the red tide was positively identified as the intense blooming or overgrowth of the dinoflagellate, Gymno- dinium brevis Davis. In 1948 following destructive outbreaks in 1946 and 1947, the U. S. Fish and Wildlife Service set up an investigation based at Sarasota, Florida, for the purpose of determining fact ors responsible for the intense blooming of G. brevis. The goal of this investigation was te develop methods for prediction and control of red tide outbreaks. This work is now being continued by the Fish and Wildlife Service at Galveston, Texas, and Fort Myers, Florida, and by the Florida State Board of Conservation through the University of Miami Marine Laboratory and the Department of Engineering of the University of Florida. The .riginal program included the collection of chemical, meteorological, and hydrographic information at approximately monthly intervals at various river, coastal, and offshore stations (figs. 1 and 2). Presented in tables I through XXVII are data collected between 1949 and 1952, which includes phosphorus data already presented by Graham, et al (1954). These data will be used for comparison with more recent findings and are pre- sented here for use by scientists engaged in red-tide research. ~ CRUISE PATTERNS The initial cruise pattern, which consisted of two river and six Gulf stations, was followed from 1949 to 1950 when a modified pattern was established which consisted of six Gulf stations. This pattern was followed until this particular oceanographic phase of the investigation was terminated in 1952. METHODS Nansen bottles were used for collection of water samples. These were lowered from the 62-foot motor vessel Pompano to the desired depth by means of a 1/8-inch hydrographic cable attached to an electrically-driven winch. Depths were determined by measuring the length of cable unwound from the drum. No attempt was made to correet for wire angles caused by drift of the vessel. Wind velocities were estimated according to the Beaufort scale and wind directions were determined with the aid ofthe ship's flag and compass. Inorganic phosphate and nitrate determinations were made according to the methods described by Robinson and Thompson (1948}. Total phosphate was determined by the method described by Harvey (1948), except that comparisons were made by means of Nessler tubes. Oxygen was determined by the modified Winkler method which increased the concen- tration of the alkali-iodide reagent from 2.5 N ands@%:respectively. Water temperatures were taken with reversing syecnnn See attached to the Nansen bottles. Temperature values presented in the tables are not corrected and for this reason are not recorded beyond the nearest tenth ofa degree. The pH measure- ments were made with a Hellige comparator and were corrected for salinity. Salinities were determined by the method described by Martin Knudsen (1901). Water transparency was measured with a standard secchi disc. Rose Mary Calaway assisted in tabulating and proof reading the data presented in this paper and also constructed and photographed the cruise pattern figures. N44 10,5 N and 7A LITERATURE CITED Galtsoff, Paul S. 1948. Red Tide, U. S. Fish and Wildlife Service, Special Scientific Report No. 46. Graham, H. W., John M. Amison, and Kenneth T. Marvin. 1954. : Phosphorus Content of Waters Along the West Coast of Florida. U.S. Fish and Wildlife Service, Special Scientific Report: Fisheries No. 122. Harvey. H. W. 1948. The Estimation of Phosphorus and Total Phosphorus in Sea Water, Journal of Marine Biological Association, vol. 27, pp. 337-359. Knudsen, Martin. 1901, Hydrographical Tables. Copenhagen and London Robinson, Rex J., and IT. G. Thompson. 1948. The Determination of Phosvuhates in Sea Water. Journal of Marine Research, vol. 7, pp. 33-41. 1948. The Determination of Nitrites in Sea Water. Journal of Marine Research, vol. 7, pp. 42-48. Winkler, L. W. 1888. The Determination of Dissolved Oxygen in Water. Ber., vol. 21, p. 2843. PS & or 9S mY rc) STATION DEPTHS( FATHOMS) STA.1 = APP .5 Figure 1.--Location of stations for cruise pattern Noe 1 GEORGIA Pee westen oa meee sao L STATION DEPTH ( FATHOM! $TA 5°10 6220 9°10 10s 20 11210 12°20 Ficure 2e-- Location of stations for cruise pattern No.» 2 EXPLANATION OF TABLES Units: Depth Meiers Temperature (e, O» (Oxygen) cc/1 T. PO, (Total Phosphate) ugat PO,-P/1 ~ Ay (Inorganic Phosphate) ugat PO,-P/1 > (Nitrite) ugat NO,-N/1 ae (Salinity) o0/oo Wind Velocity Beaufort Force No. Sky Eighths of Sky Covered Stations 1 and 2 of cruise pattern number one marked with an asterisk on tables I through XVII were occupied from the shore and water samples were trans- ported by automobile. 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