A New biological proxy for deep-sea paleo-oxygen: Pores of epifaunal benthic foraminifera

Author:

Rathburn Anthony E.,Willingham Jake,Ziebis Wiebke,Burkett Ashley M.ORCID,Corliss Bruce H.

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Reference50 articles.

1. Joos, F., Plattner, G.-K., Stocker, T. F., Körtzinger, A. & Wallace, D. W. R. Trends in marine dissolved oxygen: Implications for ocean circulation changes and the carbon budget. EOS Trans. AGU 84/21, (197–201 (2003).

2. Jaccard, S. L. & Galbraith, E. D. Large climate-driven changes of oceanic oxygen concentration during the last deglaciation. Nature Geosci. 5, 151–156 (2011).

3. Meyer, K. M. & Kump, L. R. Oceanic Euxinia in Earth History: Causes and Consequences. Ann. Rev. Earth Planet. Sci. 36, 251–288 (2008).

4. Jorissen, F. J., Fontanier, C., & Thomas, E. Paleoceanographical proxies based on deep-sea benthic foraminiferal assemblage characteristics, In: Proxies in Late Cenozoic Paleoceanography Volume 1 of Developments in Marine Geology, Hillaire-Marcel, C. & de Vernal, A., eds., Elsevier, p. 263–325 (2007).

5. Giering, S. L. C. et al. Reconciliation of the carbon budget in the ocean’s twilight zone. Nature 507, 480–483, https://doi.org/10.1038/nature13123 (2014).

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