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Deep-sea ostracod faunal dynamics in a marginal sea: biotic response to oxygen variability and mid-Pleistocene global changes

Published online by Cambridge University Press:  23 November 2018

Huai-Hsuan May Huang Open the ORCID record for Huai-Hsuan May Huang [Opens in a new window] ,
Moriaki Yasuhara ,
Hokuto Iwatani ,
Tatsuhiko Yamaguchi ,
Katsura Yamada  and
Briony Mamo
Huai-Hsuan May Huang
Affiliation:
Swire Institute of Marine Science and School of Biological Sciences, University of Hong Kong, Pokfulam, Hong Kong. E-mail: [email protected], [email protected], [email protected], [email protected]
Moriaki Yasuhara
Affiliation:
Swire Institute of Marine Science and School of Biological Sciences, University of Hong Kong, Pokfulam, Hong Kong. E-mail: [email protected], [email protected], [email protected], [email protected]
Hokuto Iwatani
Affiliation:
Swire Institute of Marine Science and School of Biological Sciences, University of Hong Kong, Pokfulam, Hong Kong. E-mail: [email protected], [email protected], [email protected], [email protected]
Tatsuhiko Yamaguchi
Affiliation:
Center for Advanced Marine Core Research, Kochi University, Monobe B200, Nankoku, 8 Kochi 783-8502, Japan. E-mail: [email protected].
Katsura Yamada
Affiliation:
Department of Geology, Shinshu University, Matsumoto 390-8621, Japan. E-mail: [email protected]
Briony Mamo
Affiliation:
Swire Institute of Marine Science and School of Biological Sciences, University of Hong Kong, Pokfulam, Hong Kong. E-mail: [email protected], [email protected], [email protected], [email protected]
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Abstract

Deep-sea benthic ostracod assemblages covering the last 2 Myr were investigated in Integrated Ocean Drilling Program Site U1426 (at 903 m water depth) in the southern Sea of Japan. Results show that (1) orbital-scale faunal variability has been influenced by eustatic sea-level fluctuations and oxygen variability and (2) secular-scale faunal transitions are likely associated with the mid-Brunhes event (MBE, ~0.43 Ma) and the onset of the Tsushima Warm Current (TWC, ~1.7 Ma). Krithe, Robertsonites, and Acanthocythereis are the three most abundant genera throughout the core, accounting for 78.5% of total specimens. Multiple-regression tree analysis indicated that the TWC, the MBE, and oxygen content are the significant controlling factors of ostracod dominance. Changes in assemblages exhibit decline and recovery patterns corresponding to orbital-scale cyclicity of sea-level changes. In the Sea of Japan marginal ocean setting, this cyclicity shows a close relationship with bottom-water oxygen variability since the onset of the TWC influx. The MBE amplified the influence of the TWC and oxygen variability to the deep-sea ecosystem through larger sea-level fluctuations. Acanthocythereis dunelmensis, a circumpolar species, dominates before the TWC onset. After the TWC onset and during the mid-Pleistocene transition (MPT, ~1.2–0.7 Ma) Krithe spp., known for their low-oxygen tolerance, substantially increase under moderate oxygen depletion. At the end of the MPT, Krithe dominance diminishes and is replaced by Robertsonites hanaii and Propontocypris spp. after the MBE. The post-MBE assemblage, characterized by R. hanaii, suggests a slightly warmer environment under the development of the TWC. In addition, the post-MBE high-amplitude climate system may have caused the increased abundance of active-swimming Propontocypris spp. due to their superior migration ability. Benthic ecosystems in marginal seas are sensitive and vulnerable to both short- and long-term climatic changes, and the MBE is suggested to be a global biotic event affecting benthic ecosystems substantially.

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Articles
Information
Paleobiology , Volume 45 , Issue 1 , February 2019 , pp. 85 - 97
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Copyright © 2018 The Paleontological Society. All rights reserved 

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Footnotes

*

Present address: 1528-3 Osoneotsu, Nankoku, 783-0005, Japan.

Data available from the Dryad Digital Repository: https://doi.org/10.5061/dryad.43vk5fm

References

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