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Updated: May 12, 2026

Laboratory Simulation of an Iron(II)-rich Precambrian Marine Upwelling System to Explore the Growth of Photosynthetic Bacteria
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Impulsos deglaciales de silicato del océano profundo en el Océano Atlántico Norte subtropical

A N Meckler1, D M Sigman, K A Gibson

  • 1Geological Institute, ETH Zürich, 8092 Zürich, Switzerland. nele.meckler@erdw.ethz.ch

Nature
|March 30, 2013
PubMed
Resumen

Durante las edades de hielo, el CO2 atmosférico inferior se almacenaba en el océano. La deglaciación liberó este CO2 a través de cambios en la circulación oceánica, particularmente en el Atlántico Norte y el Océano Sur.

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