﻿m:\v 
  FORE 
  I 
  [M 
  

  

  fauna 
  wa> 
  found 
  to 
  contain 
  some 
  valuable 
  additions 
  to 
  the 
  

  

  nton 
  and 
  Lorraine 
  fossils 
  observed 
  in 
  the 
  (Jtica 
  beds 
  of 
  

  

  this 
  i. 
  and 
  h 
  sid< 
  b, 
  Indicates 
  the 
  presence 
  of 
  the 
  upper 
  Dicel- 
  

  

  rapms 
  ione, 
  which 
  hitherto 
  lias 
  not 
  been 
  observed 
  south 
  of 
  

  

  the 
  B 
  i 
  t-wrence 
  region, 
  in 
  eastern 
  New 
  Fork. 
  The 
  fossils 
  col- 
  

  

  .1 
  are: 
  

  

  Sponge, 
  r 
  

  

  Oorynoidea 
  cartas, 
  Lapworih. 
  cc 
  

  

  Diplograptns 
  qoadrimucrouatus, 
  //'///. 
  cc 
  

  

  1 
  ». 
  folia.-. 
  -us. 
  Murchison 
  sp. 
  <• 
  

  

  Olimacograptus 
  candatns, 
  Lapworih. 
  c 
  

  

  Dawsonis 
  campanolata, 
  Nicholson, 
  c 
  

  

  Pontobdellopsis 
  cometa 
  *•/>. 
  n. 
  1 
  

  

  Lingnla 
  carta, 
  Conrad, 
  c 
  

  

  Leptobolus 
  insignis, 
  EaU. 
  c 
  

  

  B 
  oizocranis 
  ftlosa, 
  //(///. 
  r 
  

  

  Pholidops 
  snbtrnncata, 
  Hall, 
  c 
  

  

  Plectambonites 
  plicatella^ 
  Ulrich. 
  cc 
  

  

  P. 
  sericea, 
  Sowerby 
  »p. 
  

  

  Oyclospira 
  bisnlcata, 
  Emmons 
  sp. 
  c 
  

  

  Archinacella 
  patelliformis, 
  //</// 
  sp. 
  cc 
  

  

  Protowarthia 
  cancellata, 
  EaU 
  sp. 
  i=Bellerophon 
  bilobatns. 
  

   Ilulh 
  r 
  

  

  < 
  \\ 
  i 
  toceras 
  annnlatnm, 
  EaU. 
  rr 
  

  

  Bfodiolopsis 
  modiolaris, 
  Conrad, 
  r 
  

  

  M. 
  '.' 
  Quculiformis, 
  //*///. 
  p 
  

  

  « 
  toniophora 
  carinata, 
  //'/// 
  sp. 
  <• 
  

  

  • 
  taneamya, 
  sp. 
  fragment, 
  r 
  

   ita 
  levata, 
  EaU. 
  t 
  

  

  ( 
  fcmnlaris 
  trentonensis, 
  EaU. 
  

  

  inn 
  with 
  the 
  type 
  species 
  of 
  Conularia 
  

  

  lis, 
  Ball, 
  preserved 
  In 
  the 
  New 
  York 
  stare 
  museum, 
  and 
  

  

  i 
  material 
  of 
  Con 
  alar 
  la 
  hud 
  son 
  i 
  a, 
  Emmons, 
  from 
  the 
  

  

  i 
  thai 
  i 
  .i 
  form, 
  Instead 
  of 
  approaching 
  the 
  

  

  ber 
  coai 
  «>f 
  its 
  sculpture, 
  has, 
  if 
  any 
  dif- 
  

  

  n.l 
  Oner 
  arrangement 
  of 
  the 
  transversal 
  

  

  : 
  ea 
  than 
  even 
  the 
  Trenton 
  form. 
  

  

  