Proxies for paleo-oxygenation: A downcore comparison between benthic foraminiferal surface porosity and I/Ca-Reference-Cited by-同舟云学术

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Proxies for paleo-oxygenation: A downcore comparison between benthic foraminiferal surface porosity and I/Ca

Published:2021-10 Issue: Volume:579 Page:110588
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Lu Wanyi,Barbosa Catia F.,Rathburn Anthony E.,Xavier Priscila da Matta,Cruz Anna P.S.,Thomas Ellen,Rickaby Rosalind E.M.,Zhang Yi Ge,Lu Zunli

Funder

National Science Foundation

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference89 articles.

1. Scaling percentages and distributional patterns of benthic foraminifera with flux rates of organic carbon;Altenbach;J. Foraminiferal Res.,1999

2. Impact of interrelated and interdependent ecological controls on benthic foraminifera: an example from the Gulf of Guinea;Altenbach;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2003

3. Deep-sea oxygen depletion and ocean carbon sequestration during the last ice age;Anderson;Glob. Biogeochem. Cycles,2019

4. A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry;Barker;Geochem. Geophys. Geosyst.,2003

5. Redox-sensitive trace metals as paleoredox proxies: a review and analysis of data from modern sediments;Bennett;Earth Sci. Rev.,2020

Cited by 7 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Paleoenvironmental variations during the Late Cambrian: Implications from Zn isotopes, I/(Ca+Mg) ratios, and other elemental proxies;Marine and Petroleum Geology;2024-07

2. Global oceanic oxygenation controlled by the Southern Ocean through the last deglaciation;Science Advances;2024-01-19

3. Holocene paleo-redox conditions in a microbial dolomitic lake using benthic foraminifera as bioindicators;Marine Micropaleontology;2024-01

4. Expanded marine anoxia at the Cambrian-Ordovician transition: Evidence from lime mudstone I/Ca and δ238U signatures of the GSSP in western Newfoundland, Canada;Marine and Petroleum Geology;2023-09

5. Pore density of the benthic foraminiferal test responded to the hypoxia off the Changjiang estuary in the East China Sea;Frontiers in Marine Science;2023-05-18

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