Recent advances in understanding the terminal Ediacaran Earth-life system in South China and Arctic Siberia

Cui, H.; Kaufman, Alan J.; Xiao, S.; Grazhdankin, D. V.; Peek, S.; Martin, A. J.; Bykova, N. V.; Rogov, V. I.; Liu, X. M.; Zhang, F.; Romaniello, S. J.; Anbar, A. D.; Peng, Y.; Cai, Y.; Schiffbauer, J. D.; Meyer, M.; Gilleaudeau, Geoffrey J.; Plummer, Rebecca E.; Sievers, N. E.; Goderis, S.; Claeys, P.

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Date

2019-11-22

Author

Cui, H.

Kaufman, Alan J.

Xiao, S.

Grazhdankin, D. V.

Peek, S.

Martin, A. J.

Bykova, N. V.

Rogov, V. I.

Liu, X. M.

Zhang, F.

Romaniello, S. J.

Anbar, A. D.

Peng, Y.

Cai, Y.

Schiffbauer, J. D.

Meyer, M.

Gilleaudeau, Geoffrey J.

Plummer, Rebecca E.

Sievers, N. E.

Goderis, S.

Claeys, P.

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Abstract

The terminal Ediacaran contains dramatic changes in biogeochemical cycles, many of which are closely coupled with evolutionary transitions in the corresponding fossil records. Dynamic redox conditions may have caused a profound impact on early animal evolution. Our work highlights the significance of integrated bio-, litho-, and chemo-stratigraphy in geobiology research of the deep time.

URI

http://hdl.handle.net/10919/97230

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Scholarly Works, Department of Geosciences [167]
Scholarly Works, NanoEarth [2]

License: Creative Commons CC0 1.0 Universal Public Domain Dedication