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Quaternary equatorial Atlantic deep-sea ostracodes: evidence for a distinct tropical fauna in the deep sea

  • Moriaki Yasuhara*
  • , Hisayo Okahashi
  • , Huai-Hsuan May Huang
  • , Yuanyuan Hong
  • , Hokuto Iwatani
  • , Rachel Wai Ching Chu
  • , Gene Hunt
  • *Corresponding author for this work

Research output: Journal Publications and Reviews › RGC 21 - Publication in refereed journal › peer-review

Abstract

Low-latitude, deep-sea faunas remain poorly understood and described. Here, we systematically describe Quaternary deep-sea ostracodes from the Ocean Drilling Program (ODP) Site 925 (Ceara Rise; 4°12.2'N, 43°29.3′W; 3040 m water depth) in the equatorial Atlantic Ocean. Twenty-six genera and 52 species were examined and illustrated with high-resolution scanning electron microscopy images. Six new species are described herein: Pseudocythere spinae, Hemiparacytheridea zarikiani, Pedicythere canis, Xylocythere denticulata, Paracytherois obtusa, and Poseidonamicus sculptus. The results show that deep-sea ostracodes have a tropical faunal element that is distinctive from higher latitude ostracodes, and that is globally distributed in low latitudes. This tropical faunal component is possibly a Tethyan legacy of a fauna that was widely distributed in tropical and extratropical latitudes in deep waters during greenhouse conditions in the Cretaceous and early Cenozoic. Global cooling thereafter shrank its distribution, limiting it to tropical latitudes, perhaps with the relatively warm uppermost bathyal area acting as the source or refuge of this faunal component. Because similar present-day biogeographic patterns (i.e., presence and wide distribution of tropical deep-sea fauna) are known in other deep-sea benthic groups, this scenario might be applicable to the deep-sea benthos more broadly. UUID: http://zoobank.org/552d4cb2-c0db-463a-ae3f-b2efcc0985df. Copyright © The Author(s), 2022. Published by Cambridge University Press on behalf of The Paleontological Society
Original languageEnglish
Pages (from-to)1-41
Number of pages41
JournalJournal of Paleontology
Volume95
Issue numberS86
Online published11 Aug 2021
DOIs
Publication statusPublished - Dec 2021
Externally publishedYes

Funding

The work described in this article was partially supported by grants from the Research Grants Council of the Hong Kong Special Administrative Region, China (project codes HKU 17300720, HKU 17302518), the Seed Funding Programme for Basic Research of the University of Hong Kong (project codes 201811159076, 201711159057), the Small Equipment Grant of the University of Hong Kong, the Faculty of Science RAE Improvement Fund of the University of Hong Kong, the Seed Funding of the HKU-TCL Joint Research Centre for Artificial Intelligence, Smithsonian Postdoctoral Fellowship, and Smithsonian Marine Science Network Postdoctoral Fellowship (to MY); the Peter Buck Postdoctoral Fellowship of the National Museum of Natural History, Smithsonian Institution (to HHMH); and the 45th Round of the Post-doctoral Fellow Scheme of the University of Hong Kong (to YH).

RGC Funding Information

  • RGC-funded

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