
 
        
         
		Figs.  1  and  2  belong  to  the  family  of Curculionidae, of  
 which  the  Diamond  beetle  is  a  familiar  example.  
 They were discovered by Mr.Wm. Anstice in nodules  
 of Iron stone from the Coal  formation of Coalbrook  
 Dale. 
 Fig.  1  nearly  resembles  some  of  the  South  American  
 types of Curculio, but  the  antennae  are  longer and  
 stronger  than  is  usual in  living  species.  Only the  
 back of the  head  is visible, with faint indications of  
 the place of the  eyes;  the Rostrum is not apparent,  
 it  probably descends  into  the  Iron  stone  beneath,  
 and  this  position  will  explain  the  appearance  and  
 place of the Antennae. 
 The  Elytra  seem  to  have  been connate  towards  
 their  lower  extremity,  but  their  line  of junction  is  
 visible towards the Thorax.  The  substance  of  the  
 Elytra  and  Thorax,  and  of  portions  of  the  legs  is  
 replaced  by  white  Iron  ore,  having  the  lustre  of  
 Satin. 
 Mr.  Curtis conceives  that the  tufted  appearance  
 of the legs may have  been  caused  by  fungi formed  
 after  death,  as  often  happens  in  tropical  climates.  
 The enlargement of the Femur  of the hindmost leg  
 in our fossil  is  a  character  peculiar  to  the  Curculionidae.* 
   (Original.) 
 Fig. 2.  Mr.  Samouelle  considers  this  extinct fossil  species  
 to  approach  most  nearly  to  the  Brachycerus  
 apterus of Africa.f  (Original.) 
 *  Until more perfect data are found,  on which  generic characters  
 can be established,  I  propose  to  designate  this  Insect  by  the  provisional  
 name of Curculioides Ansticii. 
 t   The  animal  lies  on  its  hack  with  the  left side  raised upwards,  
 and exhibiting  a portion  of the exterior surface  of the left Elytron.' 
 At a. b. are  the  remains of  antennae,  and near  the  base  of«, ap- 
 Fig.  3.  Limulus  trilobitoides  (nobis)  forming  the  Nucleus  
 of  a  nodule  of  Iron  ore  from  Coalbrook  
 Dale.  V.  I. p. 396.*  (Original.) 
 parently a fragment of the proboscis ;  the legs are  all imperfect;  the  
 thorax  is  very  large, and  only its  inferior  surface  is visible, being  
 exposed by the removal  of  the  pectoral  portion  of  the  tru n k ;  this  
 surface  is  covered with  irregular  indentations, which  represent the  
 hollow interior  of a  series of  spinous tubercles,  and verrucose projections  
 on the back of the thorax. 
 In the centre of the  thorax is a compound  depression larger  than  
 the rest, indicating the presence of a corresponding projection on the  
 back. 
 Among living Curculionidae irregular tubercles and projections of  
 this kind occur on the thorax of the Brachycerus apterus. 
 The  left  Elytron  only  is  distinctly  visible,  embracing  with  its  
 margin the side  of the Abdomen;  its outer surface is irregularly and  
 minutely punctate.  Two spinous tubercles project from near its posterior  
 extremity,  and  a corresponding tubercle from the extremity of  
 the right elytron.  Similar  spines occur on the Elytrons of Brachycerus; 
   and  of  some  Curculionidas of N. Holland.  The  abdominal  
 rings are very distinct.  I  shall designate this Insect by the provisional  
 name of Curculioides Prestvicii. 
 M. Audouin exhibited atthe meeting of the Naturforscher at Bonn,  
 in  September, 1835,  a  beautiful wing of a neuropterous  Insect,  in  a  
 nodule  of clay Iron  stone,  apparently also  from the neighbourhood  
 of Coalbrook Dale, which had been purchased at  the  sale  of Parkinson’s  
 collection  by Mr.  Mantell,  and  transmitted  by  him  to  M.  
 Brongniart.  This wing  is nearly  three inches long,  and closely  resembles  
 that  of the  living Corydalis  of Carolina  and Pensylvania;  
 it  is  much  broader  and nearly of the length  of the wing of  a large  
 Dragon Fly. 
 *  Several specimens of this  species  are  in  the  collection  of Mr.  
 Wm. Anstice  at Madely Wood.  Our figure is taken from a cast or  
 impression  of  the  back  of  the  animal  in  Iron  stone,  in  which  the  
 transverse  lines  across  the  abdominal  segment  are  not very apparent  
 ;  other  specimens  exhibit  deep  transverse  flutings,  externally  
 resembling  the  separate  segments  of  the  back  of  a  Trilobite,  but  
 apparently  not  dividing  the  shell  into  more  than  one  abdominal  
 Plate, nor  admitting  of flexure  like  the  articulating  segments  of  a  
 Trilobite. 
 The  transverse  depressions on the back of  the  second segment of