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Global synchronous changes in the carbon isotopic composition of carbonate sediments unrelated to changes in the global carbon cycle

The carbon isotopic (δ(13)C) composition of bulk carbonate sediments deposited off the margins of four carbonate platforms/ramp systems (Bahamas, Maldives, Queensland Plateau, and Great Australian Bight) show synchronous changes over the past 0 to 10 million years. However, these variations are diff...

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Kaydedildi:
Detaylı Bibliyografya
Yazar: Swart, Peter K.
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: National Academy of Sciences 2008
Konular:
Online Erişim:https://ncbi.nlm.nih.gov/pmc/articles/PMC2544524/
https://ncbi.nlm.nih.gov/pubmed/18772393
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0802841105
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