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OCCASIONAL  PAPERS 


OF  THE 


California  Academy  of  Sciences 


No.  56,  15  pages,  21  figures. 


June  30,  1966 


A  NEW  DEEP-WATER  CHITON 

FROM  THE 

NORTHEASTERN  PACIFIC 

By 

Allyn  G.  Smith 

California  Academy  of  Sciences 

and 

Ian  McT.  Cowan 

University  of  British  Columbia 


JUL  1  11966 


SAN   FRANCISCO 

PUBLISHED  BY  THE  ACADEMY 
1966 


OCCASIONAL  PAPERS 

OF  THE 

CALIFORNIA  ACADEMY  OF  SCIENCES 

No.  56,  15  pages,  21  figures.  June  30,   1966 


A  NEW  DEEP-WATER  CHITON 

FROM  THE 

NORTHEASTERN  PACIFIC 

By 

Allyn  G.  Smith 

California  Academy  of  Sciences 

and 
Ian  McT.  Cowan 

University  of  British   Columbia 


Abstract,  lschnochiton  abyssicola,  a  new  species  of  deep-water  chiton 
from  the  northeastern  Pacific,  is  described  and  illustrated  in  detail.  Compari- 
son is  made  between  this  and  lschnochiton  stearnsi  Dall,  1902,  figured  for 
the  first  time  from  the  holotype  specimen  in  the  United  States  National  Mu- 
seum, and  lschnochiton  (Tripoplax)  trifidus  (Carpenter,  1864),  which  is  also 
figured. 


A  series  of  exploratory  dredgings  undertaken  in  1964  in  the  northeast 
Pacific  by  the  Fisheries  Research  Board  of  Canada  research  vessel  B.  G.  Reed 
has  produced  several  specimens  of  a  large  undescribed  chiton.  The  first  was 
collected  by  I.  McT.  Cowan  from  among  fishes  brought  up  in  an  otter  trawl  op- 
erating off  the  Semidi  Islands,  Alaska,  in  140-118  fathoms.  Others  were  col- 
lected subsequently  from  Queen  Charlotte  Sound,  British  Columbia,  and  off 
Cape  Flattery,  Washington,  in  the  500-fathom  range.  Another  was  dredged  off 
the  coast  of  Oregon  in  over  1000  fathoms  by  the  Oregon  State  University  De- 


CALIFORNIA  ACADEMY  OF  SCIENCES 


(Occ.  Papers 


Figures  1-3.  Ischnochiton  abyssicola  Smith  and  Cowan,  new  species.  Holo- 
type  (CAS  Invertebrate  Zoology  Type  Series  no.  287)  from  470-480  fathoms,  Queen 
Charlotte  Sound,  British  Columbia,  Canada.  (1)  dorsal;  (2)  side;  and  (3)  ventral 
views.   Length,  46  mm. 


No.  56) 


SMITH  &  COWAN:  NEW  DEEP-WATER  CHITON 


partment  of  Oceanography.  A  further  specimen  was  obtained  by  the  United 
States  Bureau  of  Commercial  Fisheries  in  291-300  fathoms  off  the  mouth  of 
the  Columbia  River.  It  would  appear,  therefore,  that  this  chiton  has  a  rather 
wide  distribution  along  the  northwest  coast  of  North  America  from  the  Aleu- 
tian Islands  as  far  south  as  Oregon,  and  that  it  may  turn  out  to  be  a  reason- 
ably common  species  in  depths  ranging  from  over  100  to  more  than  1000  fath- 
oms with  its  bathymetric  mid-point  in  the  vicinity  of  500  fathoms. 

This  new  species  belongs  in  the  family  Ischnochitonidae,  genus    Isch- 
nochiton Gray,   1847,    the  genotype  being  the  South  African  /.    texilis  (Gray, 
1828).     Ischnochiton,   sensu  lato,  is  widespread,  containing  many  described 
species.  Numerous  attempts  have  been  made  to  divide  the  group  into  smaller 
units  of  more  or  less  closely  related  forms  and  thus  far  no  less  than  sixteen 
valid  names  have  been  used  to  designate  sections,  subgenera,  or  genera,  the 
systematic  positions  chosen  depending  on  the  current  view  of  taxonomists  who 
have  endeavored  to  solve  the  complex  problem  (Smith,  1960,  pp.  55-56)-  Of  all 
the  names  available  for  use  as  possible  subgenera  of  Ischnochiton.  none  ap- 
pears to  encompass  both  the  general  characters  and  the  bathymetric  range  of 
specimens  at  hand.    In  spite  of  this  we  hesitate  to  add  a  new  subgeneric  tax- 
on  to  cover  this  new  species  until  further  critical  work  has  been  done  on  spe- 
cies assigned  to  the  genus  Ischnochiton  in  order  to  define  species  and  group 
relationships  more  clearly  and  place  them  in  a  proper  systematic  order. 


Figures  4-5.  Ischnochiton  abyssicola  Smith  and  Cowan,  new  species.  Para- 
type  (University  of  British  Columbia  Museum  of  Zoology  Collection)  from  149-118 
fathoms  south  of  the  Semidi  Islands,  Alaska.  (4)  dorsal,  and  (5)  ventral  views. 
Length  (assembled  shells  only),  89.8  mm. 


CALIFORNIA  ACADEMY  OF  SCIENCES 


(Occ.  Papers 


Figures  6-7-  Same  specimen  as  figures  4  and  5-  Enlarged  dorsal  views  of 
head  valve  (figure  6)  and  tail  valve  (figure  7).  Width  of  head  valve,  25-5  mm.;  of 
tail  valve,  22-9  mm. 


Ischnochiton  abyssicola  Smith  and  Cowan,  new  species. 
(Figures   1  -  19.) 

General  description.    Adult  animals  large  for  the  genus,  ranging  up  to 
nearly  four  inches  in  total  length,  elongate  with  a  length  somewhat  more  than 


No.  56) 


SMITH  &  COWAN:  NEW  DEEP-WATER  CHITON 


Figure   8.    Same   specimen  as  figures  4-5-    Enlarged  dorsal  view,   left  side    of 
intermediate  valve  iv.  Maximum  distance,  jugum  to  anterior  margin,  20.6  mm. 


twice  the  width,  and  with  straight  sides.  Dorsal  sculpture  on  the  head  valve, 
lateral  areas  of  intermediate  valves,  and  posterior  area  of  tail  valve  consist- 
ing of  numerous,  closely  spaced,  diagonal,  beaded  riblets  or  of  more  widely 
spaced,  granulated  ribs,  the  lateral  areas  well  defined.  Insertion  plates  on 
the  head  valve  cut  by  many  deeply  incised  slits,  of  intermediate  valves  by 
one  to  three  slits,  and  of  tail  valve  by  twelve  or  more  slits.  Teeth  between 
the  slits  short  and  blunt,  roughly  laciniated  at  their  summits  and  on  the  out- 
side, especially  on  the  head  and  tail  valves,  but  not  pectinated  as  in  the  Chi- 
tonidae.  Eaves  narrow,  solid.  Girdle  armature  of  erect,  small,  closely  packed, 
inwardly  curving,  blunt  spinules,  with  rounded  tops  giving  the  girdle  a  finely 
divided,  pebbly  surface.  Gills  ambient. 

Holotype.  A  medium-sized  adult,  its  length  2-3  times  its  width.  Head 
valve  nearly  semicircular,  the  side-slope  straight,  the  apex  slightly  everted. 
Intermediate  valves  with  straight  posterior  margins  and  slightly  convex  side- 
slopes,  making  an  angle  of  about  100°with  an  acute  jugum;  lateral  areas  prom- 
inently offset  from  the  lateropleural  areas,  narrowly  triangular,  slightly  round- 
ed at  the  side  margins.  Tail  valve  with  posterior  margin  broadly  ovate,  the 
posterior  area  set  off  from  the  anterior  by  a  rib  of  a  wideV-shape  that  is  most 


CALIFORNIA  ACADEMY  OF  SCIENCES 


(Occ.  Papers 


No.  56)  SMITH  &  COWAN:  NEW  DEEP-WATER  CHITON  7 

prominent  at  the  margin  and  gradually  becomes  obsolete  toward  the  low,   cen- 
trally placed  mucro. 

Dorsal  sculpture  of  the  head  valve,  lateral  areas  of  the  intermediate 
valves,  and  the  posterior  area  of  the  tail  valve  consisting  of  closely  spaced, 
diagonally  arranged,  somewhat  anastomosing,  finely  beaded  riblets,  the  beads 
occurring  generally  in  curving  rows  paralleling  the  lines  of  growth.  Counted 
at  the  valve  margins  there  are  about  85  riblets  on  the  head  valve,  11-13  on  the 
lateral  areas  of  the  intermediate  valves,  and  65  on  the  posterior  area  of  the 
tail  valve.  The  lateropleural  areas  of  intermediate  valves  and  the  anterior 
area  of  the  tail  valve  are  sculptured  with  a  more  or  less  parallel,  somewhat 
sinuous  network  of  very  fine  longitudinal  riblets  crossed  by  less  prominent 
lines  of  growth,  forming  a  finely  decussated  pattern  not  raised  into  beads  as 
on  the  other  shell  areas.  Thejugal  areas  are  not  prominently  outlined  and  have 
much  the  same  sculptural  pattern,  the  fine  riblets  sweeping  down  from  the  ju- 
gum  anteriorly  in  curving,  V-shaped  arrangement.  No  enlarged,  scattered  pus- 
tules occur  on  the  end  valves  or  on  the  lateral  areas  of  the  intermediate  val- 
ves as  in  some  species  of  the  related  genus  Lepidozona. 

The  girdle,  about  4  mm.  wide,  is  relatively  narrow  for  the  size  of  the 
animal,  the  dorsal  side  being  thickly  set  with  smooth,  stout,  inwardly  curved, 
scale-like  spinules,  somewhat  resembling  diminutive  surfboards  in  general 
form.  They  are  erect,  crowded  but  not  imbricate,  and  are  in  close  contact  with 
each  other  being  randomly  placed  in  their  short-axis  orientation.  They  vary 
in  size  and  shape  somewhat,  also  in  a  random  manner.  A  narrow  band  around 
the  outside  margin  of  the  girdle  has  the  stout  spinules  replaced  by  a  fringe  of 
slender  white  spines.  At  the  junction  of  the  two  spinous  areas  there  is  a  con- 
tinuous row  of  fine  setae,  the  longest  1  mm.  in  length.  The  ventral  side  of 
the  girdle  has  a  surface  composed  of  closely  appressed,  parallel  fibers  direc- 
ted crossways.  These  are  of  random  length  and  have  their  tips  free  from  the 
surface  so  that  the  entire  undersurface  of  the  girdle  is  minutely  roughened. 
They  vary  in  color  from  white  to  brown.  At  the  girdle  margin  they  extend  free, 
forming  the  band  of  delicate  fringing  spines. 

The  foot  terminates  in  a  horseshoe-shaped  oral  plate,  about  as  broad 
as  long.  Gills  are  ambient,  the  anteriormost  branchiae  being  immediately  be- 
neath or  just  in  front  of  the  posterior  lappet  of  the  oral  plate.  There  are  41 
branchiae  in  the  left  branchial  groove  and  42  on  the  right.  At  the  level  of  the 
posteriormost  branchiae,  the  inside  pedal  margins  of  the  girdle  project  inward 
in  the  form  of  a  pronounced  lappet.    The  anal  opening  is  well  behind  the  foot. 


Figures  9-11.  Same  specimen  as  figures  4-5-  Enlarged  views  of  ventral  side. 
(9)  Head  valve  in  normal  position  overlapping  the  sutural  laminae  of  intermediate 
valve  ii  showing  slits  and  teeth  in  the  insertion  plate.  (10)  Looking  down  on  the 
insertion-plate  margins  of  intermediate  valves  ii,  iii,  and  iv  showing  multiple  slits 
and  teeth.  (11)  Tail  valve  in  normal  position  showing  configuration  of  slits  and 
teeth. 


CALIFORNIA  ACADEMY  OF  SCIENCES  (Occ.  Papers 

*  7AV  jf  4     1' 

■  *  ,    ':.;'-    .  •  *V  If      '  *  -A1}  f.v 

Figure    12.      Same  specimen  as  figures  4-5-   Portion  of  girdle,   much  enlarged, 
showing  girdle  scales. 

Dorsal  color  of  the  valves  is  a  dark  red-brown,  especially  on  the  lateral 
areas  of  the  intermediate  valves,  becoming  darker  toward  the  jugum.  To  the 
unaided  eye  the  girdle  appears  to  be  a  uniform  blackish  brown,  but  under  mag- 
nification the  rounded  tips  of  the  spinules  are  a  random  mixture  of  black, 
brown,  and  whitish  colors. 

Measurements  are:  length,  46  mm.;  width,  19.5mm.;  height,  9  mm. 

Holotype  and  paratypes.  Holotype,  a  slightly  curled  perfect  specimen, 
preserved  in  alcohol,  dredged  in  470-480  fathoms  (860-878  meters) WNW.  of 
Triangle  Island,  Queen  Charlotte  Sound,  British  Columbia,  Canada  (lat.  31° 
09' W.)  by  M/V  G.  B.  Reed,  Fisheries  Research  Board  Station  no.  863,  haul 
no.  63-214,  D.  B.  Quayle  and  I.  McT.  Cowan,  collectors,  September  11,  1964. 
Deposited  in  the  California  Academy  of  Sciences  Invertebrate  Zoology  type 
series  no.  287.  The  holotype  is  of  medium  size  for  the  species  and  is  some- 
what contracted  from  preservation.  Other  specimens,  here  designated  as  para- 
types, are  as  follows: 

(1)  Three  specimens  collected  with  the  holotype,  preserved  in  alcohol: 
(a)  A  damaged  adult  measuring  approximately  60  mm.  in  length;  (b)  A  perfect 
adult  measuring  approximately  48  mm.  in  length,  23  mm.  in  width,  and  10  mm. 
in  height;  (c)  A  fairly  perfect  juvenile  measuring  in  length,  27-5  mm.,  width, 
13.5mm.,  and  height,  4-8  mm.  Numbers  of  slits  in  this  partially  disarticulated 
third  specimen  are  14+  in  the  incomplete  head  valve  and  15  in  the  tail  valve. 

(2)  A  single  very  large  adult  specimen  from  140-118  fathoms  (256-216 
meters)  south  of  the  Semidi  Islands,  Aleutian  Chain,  Alaska  (lat.  55°  15'N.; 
long.  188°  W.),  gravel  bottom,  I.  McT.  Cowan,  collector;  August,  1964,  Uni- 
versity of  British  Columbia  Museum  of  Zoology,  no.  5299  (Cowan  collection). 
Animal  preserved  in  alcohol.  The  somewhat  damaged  valves  have  been  repair- 
ed and  assembled  separately.  Measurements  of  valves  only:  length  (assem- 
bled), 89.8  mm.;  maximum  width,  293  mm.;  height,  15-2  mm.;  angle  of  diver- 
gence, 102°. 


No.  56) 


SMITH  &  COWAN:  NEW  DEEP-WATER  CHITON 


(3)  Two  badly  damaged  adult  or  subadult  specimens  from  534  fathoms 
(975  meters)  off  Swiftsure  Bank,  Washington  (lat.  55°  15'N.;  long.  156°  18' 
W.),  gravel  bottom,  Station  835,  I.  McT.  Cowan  and  D.  B.  Quayle,  collectors, 
September  6,  1964,  University  of  British  Columbia  Museum  of  Zoology,  no. 
5369  (Cowan  collection).  The  shells  of  one  specimen  were  complete  enough 
to  assemble  apart  from  the  preserved  animal.  This  measures:  length,  52  mm.; 
width,  21.5  mm.;  height,  8-5  mm.,  the  slit  formula  being  22-2/3-14.  All  val- 
ves of  the  second  specimen  were  too  shattered  to  assemble,  but  it  appears  to 
be  about  the  same  size  as  the  other.  There  are  16  slits  in  the  nearly  complete 
tail  valve  of  this  latter  specimen.  This  lot  also  contains  four  juvenile  speci- 
mens ranging  in  length  from  6.5  -  14.1  mm. 


14 


Figures  13-14-  I schno chiton  aby ssicola  Smith  and  Cowan,  new  species.  En- 
larged views  of  juvenile  specimens.  (13)Paratype  (CAS  Invertebrate  Type  Series  no. 
288)  from  2000  meters  (1093  fathoms)  off  the  coast  of  Oregon.  Length,  about  20  mm. 
(14)   Paratype  from  534  fathoms  off  Swiftsure  Bank,  Washington.     Length,    14.1  mm. 


10  CALIFORNIA  ACADEMY  OF  SCIENCES  (Occ.  Papers 

(4)  A  juvenile  with  tail  valve  missing  from  1093  fathoms  (2000  meters) 
off  the  coast  of  Oregon  (lat.  44°  33-5' N.;  long.  125°  14.6'  W.),  collected  July 
6,  1962  with  an  anchor  dredge  by  R/V< 4  cona,  cruise  no.  6207,  Oregon  State  Uni- 
versity accession  no.  06-M-06  (Department  of  Oceanography).  The  length  of 
this  specimen  is  approximately  20  mm.,  the  slit  formula  being  16-2/3-?.  De- 
posited in  the  California  Academy  of  Sciences,  Department  of  Invertebrate  Zo- 
ology, type  series  no.  288- 

Another  specimen  was   taken  in   an   otter-board  trawl  in  291-300  fath- 
oms SW.  of  the  mouth  of  the   Columbia  River  in  lat.  45°  59'  N.;  long  124°  49' 
W.  by  the  R/V  Commando  of  the  U-  S.  Bureau  of  Commercial  Fisheries   at  Sta- 
tion A-42,  collected  September  13,  1961-  It  is  a  large  adult  specimen  in  the 
Department  of  Geology,  Stanford  University. 

Paratypes  from  the  type  locality  have  been  deposited  in  the  Division  of 
Mollusks,  U.S.  National  Museum;  and  in  the  National  Museum  of  Canada,  Ot- 
tawa. 

Extended  Description  and  Discussion.  Because  the  holotype  is  a  per- 
fect specimen  we  decided  to  leave  it  intact  and  rely  on  paratype  specimens 
for  a  description  of  the  ventral  surfaces  of  the  valves  and  other  features.  The 
large  paratype  of  Ischnochiton  abyssicola  from  140-118  fathoms  off  the  Semidi 
Islands  was  used  for  this  purpose,  reference  being  made  also  to  the  assem- 
bled valves  of  the  paratype  from  534  fathoms  off  Swiftsure  Bank,  Washington, 
and  to  the  two  juvenile  specimens. 

Dorsally  the  numbers  of  riblets  on  the  Semidi  Island  paratype  are  great- 
er than  on  the  holotype,  being  125  on  the  head  valve,  11-13  on  the  lateral  ar- 
eas of  the  intermediate  valves,  and  about  80  on  the  posterior  area  of  the  tail 
valve.  On  the  youngest,  27-5  mm.  specimen  collected  with  the  holotype,  the 
corresponding  riblet  count  is  36+,  6-7,  and  35,  respectively.  On  the  Oregon 
specimen,  which  is  somewhat  smaller,  the  number  of  riblets  is  46  on  the  head 
valve,  and  9-11  on  the  lateral  areas  of  the  intermediate  valves.  Thus  it  seems 
obvious  that  this  sculptural  feature  varies  with  the  size  and  probably  with 
the  age  of  the  animal. 

Another  dorsal  feature,  seen  only  on  disarticulated  valves  ii  through 
viii,  is  a  small  rounded  extension  of  the  posterior  margin  of  the  tegmentum  at 
the  sutural  sinuses  to  form  well  developed  false  beaks. 

Ventrally,  the  tegmentum  of  valves  i  through  vii  on  the  large  Semidi 
Island  paratype  forms  a  narrow  apical  area  1.8-2.3  mm.  wide,  at  the  apex, 
becoming  much  reduced  in  width  toward  the  valve  margins.  Articulamentum 
of  the  head  valve  terminates  in  a  narrow  insertion  plate  cut  into  many  blunt 
teeth  by  deeply  incised  slits.  The  first  five  teeth  on  each  side  are  rather 
broad,  about  equally  spaced,  and  are  marked  further  by  three  to  five  shallow 
grooves  at  their  summits  that  extend  over  the  outside  surfaces.     Toward  the 


No.  56)  SMITH  &  COWAN:  NEW  DEEP-WATER  CHITON  11 

center  of  this    valve  the  teeth  are  much  broken  up  by  many  closely  spaced, 
deeply  incised  slits,  resulting  in  a  total  of  about  30  in  all.    On  the  intermed- 
iate  valves  the  insertion  plates   are  faintly  grooved  on  the  outside  and  are 
cut  by  two  shallow  slits  on  each  side,  with  indications  of  a  third  subobsolete 
one  just  behind  the  posterior  valve  margin.     Insertion  plate  of  tail  valve  cut 
by  about  12  irregularly  placed  slits  into  a  series  of  blunt  teeth,  strongly  groov- 
ed on  the  outside,  with  a  tendency  toward  the  center  of  the  valve  to  be  broken 
up  by  6  or  7  shallow  subsidiary  slits.  The  sutural  laminae  are  smooth,   broad, 
rounded,  sharp-edged,  and  continue  the  gentle  curvature  of  the  valve  margins 
to  the  rather  narrow,  generally  semicircular-shaped  sutural  sinus.    The  latter 
is  crossed  by  a  narrow  sutural  plate  set  off  from  the  ends   of  the  sutural  lam- 
inae by  shallow  notches.    On  the  tail  valve  the  sutural  laminae  are  a  bit  trun- 
cated at  the  anterior  ends  and  the  sutural  sinus  is  squared  off  by  a  much  more 
prominent  sutural  plate  that  is  delicately   grooved  on  the  outside.  The  muscle 
scars  on  the  articulamentum  of  both  head  and  tail  valves  form  a  rough,   irreg- 
ular pattern.  On  the  intermediate  valves  they  consist  of  a  low,  broad  V-shaped 
ridge,  widest  at  the  jugum  and  tapering  toward  the  valve  margins.    All  valves 
of  this  large  specimen  have  narrow  solid  eaves  that  do  not  project  beyond  the 
edges  of  the  insertion  plates.  No  slit  rays  occur. 

The  articulamentum  of  younger  specimens  with  thinner  shells  is  por- 
cellaneous and  less  chalky  than  in  older  ones;  the  slits  are  more  regularly 
placed,  the  teeth  not  being  divided  by  subsidiary  slits  although  the  tendency 
toward  subsidiary  slitting  begins  to  show  on  the  head  valves.  Well  developed 
slit  rays  are  present  in  the  valves  of  these  younger  specimens.  Their  color  is 
lighter  brown  dorsally,  with  the  valve  margins  whitish. 


Radula.  The  radulae  of  two  animals,  one  from  the  large  Semidi  Island 
specimen  and  another  from  a  somewhat  smaller  specimen  from  off  Triangle  Is- 
land, were  extracted  and  studied  by  Mr.  Spencer  R.  Thorpe,  Jr.,  of  El  Cerrito, 
California,  who  also  has  contributed  the  accompanying  drawings  (figures  15- 
19),  which  speak  for  themselves.  He  is  of  the  opinion  that  the  radula  of  /.  ab- 
yssicola  is  clearly  of  the  Lepidozona  type,  taking  into  consideration  the  con- 
figuration of  all  the  separate  parts  and  radula  size  in  relation  to  the  size  of 
the  animal.  Within  these  general  limits  Thorpe  says  that  the  subgenus  Tripo- 
plax  Berry,  1919,  represented  by  the  single  species  Ischnochiton  trifidus  (Car- 
penter, 1864)  from  Alaskan  waters  has  the  same  bidentate  cusps  on  the  major 
laterals  as  /.  abyssicola.  However,  he  points  out  that  the  broad  and  massive 
character  of  the  spatulate  uncinals,  the  markedly  bilobed  configuration  of  the 
alate  process,  and  the  general  ruggedness  of  the  radular  parts  distinguish 
/.  abyssicola  from  /.  trifidus,  although  the  two  species  appear  to  be  quite 
closely  related  on  the  basis  of  the  radula  only. 


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-Ky^ 


17 


19 


0.20  mm 


Figures   15-19.    I schno chiton  abyssicola  Smith  and  Cowan,  new  species.   Rad- 
ula  details.    (15)  Major  lateral,  large  paratype  from  the  Semidi  Islands,  viewed  from 
the  anterior.  The  outline  of  the  cusp  where  it  joins  the  shaft  may  not  be  completely 
correct    as   it  is  not  clearly   defined  because   of  the  thickness   and  translucence  of 
the    shaft.        (16)    Cusp  of  major  lateral,    smaller  paratype   from   off  Triangle  Island, 


No.  56)  SMITH  &  COWAN:  NEW  DEEP-WATER  CHITON  13 

Comparative  relationships.  Ischnochiton  abyssicola  is  by  far  the  larg- 
est Ischnochiton  ever  taken  from  deep  water  of  the  Pacific  Coast  of  North 
America.  In  size  and  general  shape  it  is  much  like  the  larger  ischnochitonid 
species  in  the  genus  Stenoplax,  such  as  the  Panamic  S.  magdalenensis  (Hinds) 
and  the  Californian  S.  conspicua  (Dall),  S.  heathiana  Berry,  and  S.  fallax  (Car- 
penter). The  configuration  of  the  head  and  tail  valves  of  /.  abyssicola  is  much 
the  same  as  in  these  species  of  Stenoplax.  However,  the  finely  beaded  dorsal 
sculpture,  the  tendency  toward  multiple  slitting  of  the  end  valves  with  age, 
and  the  peculiar  girdle  decoration  all  are  markedly  different  from  Stenoplax. 
Moreover  the  benthic  range  of  /.  abyssicola  leaves  a  wide  gap  in  habitat,  as 
all  the  larger  species  of  Stenoplax  live  in  a  low  intertidal  or  high  subtidal 
zone;  so  far  as  we  are  aware  there  are  no  dredging  records  for  any  of  the  lat- 
ter. The  geographical  range  of  the  new  species,  based  on  the  material  at  hand, 
extends  well  to  the  north  of  any  known  member  of  the  genus  Stenoplax,  the 
northernmost  record  being  Vancouver  Island  for  S.  fallax.  and  Coos  Bay,  Ore- 
gon, for  S.  heathiana. 

The  relationship   to  the  Alaskan  Ischnochiton  trijidus  based  on  radular 
characters   only,   has  already  been   mentioned.     Ischnochiton  trijidus  (figure 
20)  also  has  multiple-slitted  insertion  plates  in  the  intermediate  valves,  but 
the  dorsal  sculpture  of  the  valves  and  girdle  armature  of  solid,  rather  convex 
scales  are  different  from  /.  abyssicola.     While  the  bathymetric  range   of  /.  tri- 
jidus is  not  well  known,   it  is  generally  found  in  moderate  depths  widely  sep- 
arated from  the  abyssal  niche  of  /.  abyssicola.    A  possible  other  near  relative 
is  the  little-known  Ischnochiton  stearnsi  Dall,   1902,  until  recently  based  on 
a  single  specimen  inthe  United  States  National  Museum  (holotype  no.  109024) 
collected   by  the  U.  S.  S.    Albatross  in  391   fathoms  off  the  Farallon  Islands, 
California.     Another  specimen  of  1.  stearnsi  was  dredged    by  the  R/V    Velero 
IV.  cruise  no.  641,  on  February  13,  1965,  in  255  fathoms,  7-2  miles  190°  True 
from  Long  Point,  Santa  Catalina  Island,  California  (Los  Angeles  County  Mu- 
seum no.  10328).  Comparison  of  this  second  specimen,  which  was  made  avail- 
able by  James  H.  McLean  of  the  Los  Angeles  County  Museum,  with  the  holo- 
type loaned  through  the  courtesy  of  Dr.  Harald  A.  Rehder  of  the  U.S.  National 
Museum  (figure  21)  leaves  no  doubt  as  to  its  identity.    Ischnochiton  stearnsi 
is  a  relatively  small  species,  around  25  mm.  in  length,    and  has  a  more  or  less 
typically  granular  Lepidozona-type  dorsal  sculpture  with  no  enlarged  scattered 
pustules  on  the  valve  surfaces.  Ventrally  some  of  the  intermediate  valves  are 
double-slitted  although  there  seems  to  be  no  tendency  toward  subsidiary  slit- 
Queen  Charlotte  Sound.    Ventral  Aspect.     (17)  Detail  of  central  tooth,   Semidi  Island 
paratype:   (a)  from  directly  above,  (b)  from  the  side.      (18)   Two  views  of  a  spatulate 
uncinal,    Semidi  Island  paratype.      The   smaller  branching  part  at  the  bottom   of  the 
bottom  of  the  figure  is  directed  anteriorly  in  the  complete  radula.   (19)    Detail  of  cen- 
tral portion  of  radula,   Semidi  Island  paratype:     (a)  central  tooth,   (b)  minor  laterals, 
(c)  bases  of  major  laterals.     Dorsal  view. 


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ting  in  the  end  valves.  The  general  configuration  of  the  teeth  in  the  insertion 
plates  and  the  similarity  of  the  girdle  scales  of  both  /.  abyssicola  and  /.  steam- 
si  seem  to  us  to  be  sufficient  evidence  to  warrant  placing  the  two  in  the  same 


21 


Figure   20-     Ischnochiton  trifidus  (Carpenter).     Dorsal  view  of  adult  specimen 
from  Auke  Hay,  Alaska.  Jack  R.   Bailey,  collector.   Length,  37.6  mm. 

Figure  21.  Ischnochiton  stearnsi  Dall.  Enlarged  side  view  of  the  holotype 
(United  States  National  Museum  no.  10^024)  from  3Q1  fathoms  off  the  Farallon  Is- 
lands, California,  showing  intermediate  valves  iii-vi,  inclusive,  and  girdle  scales. 
Height,  6  mm. 


No.  56)  SMITH  &  COWAN:  NEW  DEEP-WATER  CHITON  15 

species-group.  Although  the  sculptural  pattern  of  /.  stearnsi  is  quite  different 
from  that  of  /.  abyssicola  this  appears  to  be  a  specific  rather  than  a  subgener- 
ic  or  generic  difference  in  this  instance. 

In  conclusion,  the  authors  wish  to  express  special  thanks  to  Mr.  Spen- 
cer Thorpe  for  his  study  of  the  radula  of  the  new  species  and  for  his  coopera- 
tion in  providing  excellent  illustrations  (figures  15-19)  for  inclusion  in  this 
paper;  to  Mrs.  G.  Samuel  Alspach  of  the  Department  of  Oceanography,  Oregon 
State  University,  for  supplying  the  Oregon  specimen;  and  to  Mr.  Maurice  Giles 
and  Dr.  G  Dallas  Hanna  of  the  California  Academy  of  Sciences  for  assistance 
with  the  production  of  the  illustrations.  Figures  1-14  and  20-21  are  from  Koda- 
chrome  slides  by  the  senior  author. 

REFERENCES 

Berry,   S.  Stillman 

1946-  A  re-examination  of  the  chiton,  Stenop lax  magdalenensis  (Hinds),  with 
description  of  a  new  species.  Proceedings  of  the  Malacological  So- 
ciety of  London,  vol.  26,  pt.  6,  pp.  161-166,  pis.  4-5,  text  figs.  1-6, 
January  31. 

Dall,  William  H. 

1902-      Illustrations   and  descriptions   of  new,    unfigured,   or  imperfectly  known 
shells,   chiefly  American,   in  the  U.  S.  National  Museum.   Proceedings 
of  the  United  States  National  Museum,    vol.   24,    no.    1264,   pp-   499- 
566,  pis.  27-40.  Washington.  (Is chno chiton  stearnsi  Dall,  pp.  557-588.) 

Pilsbry,  Henry  A. 

1892-   Polyplacophora.    Manual   of  Conchology,    vol.    14,   pp.    i-xxxiv,    1-350,   pis. 
1893.  1-68-   Philadelphia.   (Genus  Ischnochiton,  pp.  53-148.) 

Smith,  Allyn  G. 

I960-  Amphineura.  Treatise  on  Invertebrate  Paleontology  (R.  C-  Moore,  ed.), 
pt.  I,  Mollusca  1,  pp.  41-76,  text  figs.  31-45-  Geological  Society 
of  America.   University  of  Kansas  Press. 


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