Isotopic analyses of Ordovician–Silurian siliceous skeletons indicate silica‐depleted Paleozoic oceans-Reference-Cited by-同舟云学术

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Isotopic analyses of Ordovician–Silurian siliceous skeletons indicate silica‐depleted Paleozoic oceans

Published:2021-05-17 Issue:5 Volume:19 Page:460-472
ISSN:1472-4677
Container-title:Geobiology
language:en
Short-container-title:Geobiology

Author:

Trower Elizabeth J.¹^ORCID,Strauss Justin V.²^ORCID,Sperling Erik A.³^ORCID,Fischer Woodward W.⁴^ORCID

Affiliation:

1. Department of Geological Sciences University of Colorado Boulder Boulder CO USA

2. Department of Earth Sciences Dartmouth College Dartmouth NH USA

3. Department of Geological Sciences Stanford University Stanford CA USA

4. Division of Geological and Planetary Sciences California Institute of Technology Pasadena CA USA

Funder

National Science Foundation

Publisher

Wiley

Subject

General Earth and Planetary Sciences,General Environmental Science,Ecology, Evolution, Behavior and Systematics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/gbi.12449

Reference95 articles.

1. The seasonal sea-ice zone in the glacial Southern Ocean as a carbon sink

2. Late devonian oceanic anoxic events and biotic crises: “rooted” in the evolution of vascular plants;Algeo T. J.;GSA Today,1995

3. Radiolarian Skeletons: Solution at Depths

4. A paired apatite and calcite clumped isotope thermometry approach to estimating Cambro-Ordovician seawater temperatures and isotopic composition

5. Weathering, plants, and the long-term carbon cycle

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