A review of benthic foraminiferal oxygen and carbon isotopes

被引：1

作者：

Hoogakker, Babette ^{[1
]}

Ishimura, Toyoho ^{[2
]}

de Nooijer, Lennart ^{[3
]}

Rathburn, Anthony ^{[4
]}

Schmiedl, Gerhard ^{[5
]}

机构：

[1] Heriot Watt Univ, Lyell Ctr, Res Ave South, Edinburgh EH14 4B, Scotland

[2] Kyoto Univ, Grad Sch Human & Environm Studies, Yoshida Nihonmatsu Cho,Sakyo Ku, Kyoto 6068501, Japan

[3] Royal Netherlands Inst Sea Res, Yerseke, Netherlands

[4] Calif State Univ Bakersfield, 9001 Stockdale Highway, Bakersfield, CA 93311 USA

[5] Univ Hamburg, Inst Geol, Bundesstr 55, D-20146 Hamburg, Germany

来源：

QUATERNARY SCIENCE REVIEWS | 2024年 / 342卷

关键词：

DEEP-SEA FORAMINIFERA; STABLE CARBON; GROWTH-RATE; PLANKTIC FORAMINIFERS; CONTINENTAL-MARGIN; DELTA-C-13; FRACTIONATION; TEMPERATURE; CALIFORNIA; METHANE;

D O I：

10.1016/j.quascirev.2024.108896

中图分类号：

P9 [自然地理学];

学科分类号：

0705 ; 070501 ;

摘要：

Stable isotopes in the calcium carbonate of benthic foraminifera provide important paleoenvironmental information about seawater/sedimentary porewaters that these foraminifera live in. Oxygen isotopes provide essential insights about variations in deep water temperatures and sea-level/ice volume changes, while carbon isotopes provide information about sea-water carbon/nutrient cycling. In this review we look into detail at the direct and indirect mechanisms that contribute to stable oxygen and carbon isotope signals in Rotaliid benthic foraminifera. This includes effects from ontogenetic- and calcification mechanisms, and the impact of methane seeps and post-depositional diagenesis. We conclude our review with an overview of current challenges and provide recommendations for future research endeavors aimed at outstanding knowledge gaps in understanding how these biomineralizers control their stable isotopes.

引用

页数：14

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