KCIIINOIUKA. II. 



187 



not have been overlooked in the regions, from where they are hitherto not recorded. It seems then 

 really to be the ease, that also the Atlantic deep sea comprises several distinct regions, though it seems 

 impossible for the present to point out special physical characters, which distinguish the separate re- 

 gions. As seen in Gerh. Schott's admirable Oceanographie und maritime Meteorologies the bottom 

 temperature is in the whole Atlantic, in depths beyond 1000 M., over 2°. Only in the Davis Strait 

 and in the large Brazilian basin to the West of the midatlantic ridge (from near St. Paul down to the 

 antarctic sea) the temperature is below 2°. But this difference in the temperature does not seem to 

 be sufficient to cause corresponding marked differences in the deep-sea Echinoid-fauna. 



The subdivision of the deep-sea regions into an archibenthal and abyssal zone is upon the whole 

 not supported by the bathymetrical distribution of the species; most of the species occurring in the 

 abyssal zone also occur in the archibenthal zone, and probably several of the species hitherto not 

 known beyond the archibenthal zone will ultimately prove to have a greater bathymetrical distribution. 

 Still it is worth noticing that the Meridosternata almost exclusively belong to the abyssal zone. 



The European Atlantic deep-sea region comprises the Northern Atlantic, to the East of a 

 line from the Denmark Strait to the Gibraltar Strait. 2 It is limited from the cold area of the Nor- 

 wegian Sea by the ridges across the Denmark-Strait, the Faroe-Channel and between Iceland and the 

 Faroe Islands. 



The following species are known from this region : 



Trigonocidaris albida 

 Hypsiechinus coronatus 

 Echinus eseulentus 



— acutus 



— elegans 



— Alexandri 

 affinis 



Strongylocentrotus drobachiensis Spataugus purpureus 

 Sphaerechiuus granulans — Raschi 



Echinocyamus pusillus Echiuocardium flavescens 



Neolampas rostellata Brissopsis lyrifera. 



Of these species we may first eliminate the following as occasional intruders from the boreal 

 and Mediterranean regions: Ecliiuus eseulentus, Strongyloccntrotus drobachiensis, Spliarcchiniis granu- 

 lar is and Echiuocardium flavescens. Of the rest the following are known from this region only: ArcB- 

 osoma violaccum, Echinosoma uranus, Hypsiechinus coronatus, Plexecliinus hirsutus, Ecliinosigra (Pour- 

 talcsia) pliiale and paradoxa. Porocidaris purpurata and Sperosovia Grimaldi are known only from this 

 and the West African region. These species are, however, (except Porocidaris purpurata and Spero- 

 sovia Grimaldi) either small or easily confused with other species. It is certainly not much to 

 characterize the region by, but especially Porocidaris purpurata and Spcrosoma Grimaldi are so mag- 

 nificent and peculiar forms that they can certainly not have been confused with other species; the 



Dorocidaris papillata 

 Stereocidaris ingolfiana 

 Porocidaris purpurata 

 Phormosoma placenta 

 Calveria hystrix 

 Araeosoma tenestratum 



violaeeum 

 Hygrosoma Petersi 

 Sperosoma Grimaldi 

 Echinosoma uranus 

 Salenia hastigera 



Urechinus naresianus 

 Plexecliinus hirsutus 

 Pourtalesia Wandeli 

 Echinosigra (Pourtalesia) phiale 



— paradoxa 



Hemiaster expergitus 

 Brisaster fragilis 



1 Wissensch. Ergebn. d. deutsch. Tiefsee-Exp. I. 1902. 



2 The limit between the European and the East American Atlantic deep-sea regions will undoubtedly prove not to 

 be a straight line of the course here indicated. P'or the present, however, our knowledge of the deep-sea fauna of the Mid- 

 Atlantic is too insufficient for pointing out the limit between these regions more exactly. 



24* 



