Rise of angiosperms as a factor in long-term climatic cooling

Research output: Contribution to journalArticle

Abstract

By Late Cretaceous or early Tertiary time, the diversification and proliferation of angiosperm-deciduous ecosystems resulted in higher rates of mineral weathering. This increase in the global average weathering rate would have caused a decrease in atmospheric carbon dioxide and, hence, global cooling. This cooling may vary from a few degrees up to 10°C. In this way, deciduous ecosystems with high rates of mineral weathering could have contributed to the evolution during the past 100 m.y. of a cooler Earth and thus were a factor in producing conditions that enhanced their global proliferation. -from Author

Original languageEnglish (US)
Pages (from-to)107-110
Number of pages4
JournalGeology
Volume17
Issue number2
DOIs
StatePublished - 1989

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angiosperm
weathering
cooling
weathering rate
ecosystem
mineral
carbon dioxide
Cretaceous
rate

ASJC Scopus subject areas

  • Geology

Cite this

Rise of angiosperms as a factor in long-term climatic cooling. / Volk, T.

In: Geology, Vol. 17, No. 2, 1989, p. 107-110.

Research output: Contribution to journalArticle

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