Peatmoss (Sphagnum) diversification associated with Miocene Northern Hemisphere climatic cooling?

Shaw, A. J.; Devos, N.; Cox, C. J.; Boles, S. B.; Shaw, B.; Buchanan, A. M.; Cave, L.; Seppelt, R.

http://hdl.handle.net/10400.1/5554

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Resumo(s)

Global climate changes sometimes spark biological radiations that can feed back to effect significant ecological impacts. Northern Hemisphere peatlands dominated by living and dead peatmosses (Sphagnum) harbor almost 30% of the global soil carbon pool and have functioned as a net carbon sink throughout the Holocene, and probably since the late Tertiary. Before that time, northern latitudes were dominated by tropical and temperate plant groups and ecosystems.

Palavras-chave

Bryophyte evolution Sphagnum Miocene Peatmosses Peatlands

URI

http://hdl.handle.net/10400.1/5554

Citação

Shaw, A.J.; Devos, N.; Cox, C.J.; Boles, S.B.; Shaw, B.; Buchanan, A.M.; Cave, L.; Seppelt, R.Peatmoss (Sphagnum) diversification associated with Miocene Northern Hemisphere climatic cooling?, Molecular Phylogenetics and Evolution, 55, 3, 1139-11, 2010.

Editora

Elsevier

DOI

http://dx.doi.org/10.1016/j.ympev.2010.01.020

Coleções

CCM2-Artigos (em revistas ou actas indexadas)

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