Mediterranean isolation preconditioning the Earth System for late Miocene climate cooling View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2019-12

AUTHORS

Walter Capella, Rachel Flecker, F. Javier Hernández-Molina, Dirk Simon, Paul Th. Meijer, Mike Rogerson, Francisco J. Sierro, Wout Krijgsman

ABSTRACT

A global Neogene cooling trend culminated ~7 million years ago with the onset of Greenland glaciation. Increased ocean-atmosphere interaction and low- to high-latitude circulation are thought to be key factors in reorganizing late Miocene global temperature and precipitation patterns, but the drivers of this reorganization have yet to be identified. Here, we present new information about the evolution of the Atlantic-Mediterranean gateway that generated Mediterranean overflow. We use sedimentary and palaeogeographic evidence to constrain the timing and dimensions of this gateway and document the initiation of a saline plume of water within the North Atlantic. Today, this saline jet entrains and transports Eastern North Atlantic water and its dissolved inorganic carbon into the interior of the ocean, contributing to the drawdown of CO2 and the sensitivity of the ocean to atmospheric changes. We show that during the Miocene this transport emerged simultaneously with gateway restriction and propose that the resulting interaction of ocean-surface and ocean-interior carbon inventories would have greatly enhanced ocean-atmosphere exchange, preconditioning the Earth System for late Miocene cooling. More... »

PAGES

3795

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/s41598-019-40208-2

DOI

http://dx.doi.org/10.1038/s41598-019-40208-2

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1112605603

PUBMED

https://www.ncbi.nlm.nih.gov/pubmed/30846804


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Download the RDF metadata as:  json-ld nt turtle xml License info

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Turtle is a human-readable linked data format.

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RDF/XML is a standard XML format for linked data.

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