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Bibliographic Details
Main Authors: Sangiorgi, Francesca, Quaijtaal, Willemijn, Donders, Timme H, Schouten, Stefan, Louwye, Stephen
Format: Dataset Open Access
Language:en
Published: PANGAEA 2021
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.926326
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author Sangiorgi, Francesca
Quaijtaal, Willemijn
Donders, Timme H
Schouten, Stefan
Louwye, Stephen
author_facet Sangiorgi, Francesca
Quaijtaal, Willemijn
Donders, Timme H
Schouten, Stefan
Louwye, Stephen
collection Datos científicos de ciencias marinas y ambientales
contents Mid-Miocene (16.6 – 12.8 Ma) sea surface ocean temperatures and sea surface productivity are obtained from the sediment record of Integrated Ocean Discovery Program (IODP) Expedition 307, Site U1318 drilled in the Porcupine Basin, north east Atlantic at a water depth of ~ 400m. Seawater temperatures were obtained using both the TEX86 and Uk37 paleothermometers, which document the Miocene Climatic Optimum and a series of cooling events, some correspondent to the Miocene Mi-2, Mi-3 and Mi-4 events. Cooling events are also documented by changes in the dinoflagellate cyst assemblages. Sea surface productivity was reconstructed by means of dinoflagellate cysts, employing the ratio between Protoperidinioid and Gonyalulacoid (P/G) specimens in the assemblages.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_926326
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Middle Miocene temperature and productivity evolution at IODP Site 307-U1318
Sangiorgi, Francesca
Quaijtaal, Willemijn
Donders, Timme H
Schouten, Stefan
Louwye, Stephen
Dinocysts; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; middle Miocene; North Atlantic; Sea Surface Productivity; Sea surface temperature
Mid-Miocene (16.6 – 12.8 Ma) sea surface ocean temperatures and sea surface productivity are obtained from the sediment record of Integrated Ocean Discovery Program (IODP) Expedition 307, Site U1318 drilled in the Porcupine Basin, north east Atlantic at a water depth of ~ 400m. Seawater temperatures were obtained using both the TEX86 and Uk37 paleothermometers, which document the Miocene Climatic Optimum and a series of cooling events, some correspondent to the Miocene Mi-2, Mi-3 and Mi-4 events. Cooling events are also documented by changes in the dinoflagellate cyst assemblages. Sea surface productivity was reconstructed by means of dinoflagellate cysts, employing the ratio between Protoperidinioid and Gonyalulacoid (P/G) specimens in the assemblages.
title Middle Miocene temperature and productivity evolution at IODP Site 307-U1318
topic Dinocysts; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; middle Miocene; North Atlantic; Sea Surface Productivity; Sea surface temperature
url https://doi.org/10.1594/PANGAEA.926326