Ancient origin of the modern deep-sea fauna.

The origin and possible antiquity of the spectacularly diverse modern deep-sea fauna has been debated since the beginning of deep-sea research in the mid-nineteenth century. Recent hypotheses, based on biogeographic patterns and molecular clock estimates, support a latest Mesozoic or early Cenozoic...

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Autores principales: Ben Thuy, Andy S Gale, Andreas Kroh, Michal Kucera, Lea D Numberger-Thuy, Mike Reich, Sabine Stöhr
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Publicado: Public Library of Science (PLoS) 2012
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Acceso en línea:https://doaj.org/article/d775df8e86e149908f930985f0151ea4
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spelling oai:doaj.org-article:d775df8e86e149908f930985f0151ea42021-11-18T08:12:33ZAncient origin of the modern deep-sea fauna.1932-620310.1371/journal.pone.0046913https://doaj.org/article/d775df8e86e149908f930985f0151ea42012-01-01T00:00:00Zhttps://www.ncbi.nlm.nih.gov/pmc/articles/pmid/23071660/?tool=EBIhttps://doaj.org/toc/1932-6203The origin and possible antiquity of the spectacularly diverse modern deep-sea fauna has been debated since the beginning of deep-sea research in the mid-nineteenth century. Recent hypotheses, based on biogeographic patterns and molecular clock estimates, support a latest Mesozoic or early Cenozoic date for the origin of key groups of the present deep-sea fauna (echinoids, octopods). This relatively young age is consistent with hypotheses that argue for extensive extinction during Jurassic and Cretaceous Oceanic Anoxic Events (OAEs) and the mid-Cenozoic cooling of deep-water masses, implying repeated re-colonization by immigration of taxa from shallow-water habitats. Here we report on a well-preserved echinoderm assemblage from deep-sea (1000-1500 m paleodepth) sediments of the NE-Atlantic of Early Cretaceous age (114 Ma). The assemblage is strikingly similar to that of extant bathyal echinoderm communities in composition, including families and genera found exclusively in modern deep-sea habitats. A number of taxa found in the assemblage have no fossil record at shelf depths postdating the assemblage, which precludes the possibility of deep-sea recolonization from shallow habitats following episodic extinction at least for those groups. Our discovery provides the first key fossil evidence that a significant part of the modern deep-sea fauna is considerably older than previously assumed. As a consequence, most major paleoceanographic events had far less impact on the diversity of deep-sea faunas than has been implied. It also suggests that deep-sea biota are more resilient to extinction events than shallow-water forms, and that the unusual deep-sea environment, indeed, provides evolutionary stability which is very rarely punctuated on macroevolutionary time scales.Ben ThuyAndy S GaleAndreas KrohMichal KuceraLea D Numberger-ThuyMike ReichSabine StöhrPublic Library of Science (PLoS)articleMedicineRScienceQENPLoS ONE, Vol 7, Iss 10, p e46913 (2012)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Ben Thuy
Andy S Gale
Andreas Kroh
Michal Kucera
Lea D Numberger-Thuy
Mike Reich
Sabine Stöhr
Ancient origin of the modern deep-sea fauna.
description The origin and possible antiquity of the spectacularly diverse modern deep-sea fauna has been debated since the beginning of deep-sea research in the mid-nineteenth century. Recent hypotheses, based on biogeographic patterns and molecular clock estimates, support a latest Mesozoic or early Cenozoic date for the origin of key groups of the present deep-sea fauna (echinoids, octopods). This relatively young age is consistent with hypotheses that argue for extensive extinction during Jurassic and Cretaceous Oceanic Anoxic Events (OAEs) and the mid-Cenozoic cooling of deep-water masses, implying repeated re-colonization by immigration of taxa from shallow-water habitats. Here we report on a well-preserved echinoderm assemblage from deep-sea (1000-1500 m paleodepth) sediments of the NE-Atlantic of Early Cretaceous age (114 Ma). The assemblage is strikingly similar to that of extant bathyal echinoderm communities in composition, including families and genera found exclusively in modern deep-sea habitats. A number of taxa found in the assemblage have no fossil record at shelf depths postdating the assemblage, which precludes the possibility of deep-sea recolonization from shallow habitats following episodic extinction at least for those groups. Our discovery provides the first key fossil evidence that a significant part of the modern deep-sea fauna is considerably older than previously assumed. As a consequence, most major paleoceanographic events had far less impact on the diversity of deep-sea faunas than has been implied. It also suggests that deep-sea biota are more resilient to extinction events than shallow-water forms, and that the unusual deep-sea environment, indeed, provides evolutionary stability which is very rarely punctuated on macroevolutionary time scales.
format article
author Ben Thuy
Andy S Gale
Andreas Kroh
Michal Kucera
Lea D Numberger-Thuy
Mike Reich
Sabine Stöhr
author_facet Ben Thuy
Andy S Gale
Andreas Kroh
Michal Kucera
Lea D Numberger-Thuy
Mike Reich
Sabine Stöhr
author_sort Ben Thuy
title Ancient origin of the modern deep-sea fauna.
title_short Ancient origin of the modern deep-sea fauna.
title_full Ancient origin of the modern deep-sea fauna.
title_fullStr Ancient origin of the modern deep-sea fauna.
title_full_unstemmed Ancient origin of the modern deep-sea fauna.
title_sort ancient origin of the modern deep-sea fauna.
publisher Public Library of Science (PLoS)
publishDate 2012
url https://doaj.org/article/d775df8e86e149908f930985f0151ea4
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