We investigated the biotic response to the Middle Eocene Climatic Optimum (MECO) at Site 1263 (South-Eastern Atlantic), which has a continuous record not affected by carbonate dissolution and well constrained middle-upper Eocene biostratigraphy. We used coupled analysis of micropaleontological, stable isotope and biomarker (GDGTs) proxies across MECO, so we could reconstruct sea surface temperatures (SST) and biotic changes throughout the water column.

Warming, pelagic food webs and deep-sea biota during the Middle Eocene Climatic Optimum in the SE Atlantic (ODP Site 1263).

LUCIANI, Valeria
2014

Abstract

We investigated the biotic response to the Middle Eocene Climatic Optimum (MECO) at Site 1263 (South-Eastern Atlantic), which has a continuous record not affected by carbonate dissolution and well constrained middle-upper Eocene biostratigraphy. We used coupled analysis of micropaleontological, stable isotope and biomarker (GDGTs) proxies across MECO, so we could reconstruct sea surface temperatures (SST) and biotic changes throughout the water column.
2014
Boscolo Galazzo, F.; Thomas, E.; Pagani, M.; Warren, C.; Giusberti, L.; Luciani, Valeria
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11392/2115812
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