Sea ice dynamics across the Mid-Pleistocene transition in the Bering Sea

Modelling studies propose sea ice to be one of the underlying mechanisms for the Mid-Pleistocene transition. Here, the authors show Mid-Pleistocene subarctic North Pacific sea ice dynamics based on biomarkers and biogenic opal accumulation rates, supporting the importance of sea ice for climate chan...

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Autores principales: H. Detlef, S. T. Belt, S. M. Sosdian, L. Smik, C. H. Lear, I. R. Hall, P. Cabedo-Sanz, K. Husum, S. Kender
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2018
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Acceso en línea:https://doaj.org/article/2dbe8013d3a1495a81a89ceea3f47533
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Sumario:Modelling studies propose sea ice to be one of the underlying mechanisms for the Mid-Pleistocene transition. Here, the authors show Mid-Pleistocene subarctic North Pacific sea ice dynamics based on biomarkers and biogenic opal accumulation rates, supporting the importance of sea ice for climate change.