Stabilization of the coupled oxygen and phosphorus cycles by the evolution of bioturbation-Reference-Cited by-同舟云学术

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Stabilization of the coupled oxygen and phosphorus cycles by the evolution of bioturbation

Published:2014-08-03 Issue:9 Volume:7 Page:671-676
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Boyle R. A.,Dahl T. W.,Dale A. W.,Shields-Zhou G. A.,Zhu M.,Brasier M. D.,Canfield D. E.,Lenton T. M.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo2213.pdf

Reference30 articles.

1. Liu, A. G., Mcllroy, D. & Brasier, M. D. First evidence for locomotion in the Ediacara biota from the 565 Ma Mistaken Point Formation, Newfoundland. Geology 38, 123–126 (2010).

2. Menon, L., McIlroy, D. & Brasier, M. D. Evidence for Cnidaria-like behavior in ca. 560 Ma Ediacaran Aspidella. Geology 41, 895–898 (2013).

3. Mangano, M & Buatois, L. A. Decoupling of body plan diversification and ecological structuring during the Ediacaran–Cambrian transition: Evolutionary and geobiological feedbacks. Proc. R. Soc. B 281, 20140038 (2014).

4. Buatois, L. A., Narbonne, G. M., Mangano, M. G., Carmona, M. B. & Myrow, P. Ediacaran matground persisted into the earliest Cambrian. Nature Commun. 5, 3544 (2014).

5. Tarhan, L. G. & Droser, M. L. Widespread delayed mixing in early to middle Cambrian marine shelfal settings. Palaeogeogr. Palaeoclimatol. Palaeoecol. 399, 310–322 (2014).

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