The Uniqueness of Planktonic Ecosystems in the Mediterranean Sea: The Response to Orbital- and Suborbital-Climatic Forcing over the Last 130,000 Years

The Mediterranean Sea is an ideal location to test the response of organisms to hydrological transformations driven by climate change. Here we review studies carried out on planktonic foraminifera and coccolithophores during the late Quaternary and attempt the comparison of data scattered in time an...

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Main Authors: Incarbona Alessandro, Di Stefano Enrico, Sprovieri Rodolfo, Ferraro Serena
Format: Article
Language:English
Published: De Gruyter 2016-01-01
Series:Open Geosciences
Subjects:
Online Access:https://doi.org/10.1515/geo-2016-0050
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author Incarbona Alessandro
Di Stefano Enrico
Sprovieri Rodolfo
Ferraro Serena
author_facet Incarbona Alessandro
Di Stefano Enrico
Sprovieri Rodolfo
Ferraro Serena
author_sort Incarbona Alessandro
collection DOAJ
description The Mediterranean Sea is an ideal location to test the response of organisms to hydrological transformations driven by climate change. Here we review studies carried out on planktonic foraminifera and coccolithophores during the late Quaternary and attempt the comparison of data scattered in time and space. We highlight the prompt response of surface water ecosystems to both orbital- and suborbital-climatic variations.
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spelling doaj.art-26276694a80c4caaa33622a0eaa479382022-12-21T19:17:27ZengDe GruyterOpen Geosciences2391-54472016-01-018156757810.1515/geo-2016-0050geo-2016-0050The Uniqueness of Planktonic Ecosystems in the Mediterranean Sea: The Response to Orbital- and Suborbital-Climatic Forcing over the Last 130,000 YearsIncarbona Alessandro0Di Stefano Enrico1Sprovieri Rodolfo2Ferraro Serena3Università di Palermo, Dipartimento di Scienze della Terra e del Mare, Via Archirafi 22, 90134 Palermo, ItalyUniversità di Palermo, Dipartimento di Scienze della Terra e del Mare, Via Archirafi 22, 90134 Palermo, ItalyUniversità di Palermo, Dipartimento di Scienze della Terra e del Mare, Via Archirafi 22, 90134 Palermo, ItalyUniversità degli Studi di Urbino “Carlo Bo”, Dipartimento di Scienze della Terra, della Vita e dell’Ambiente, Campus Scientifico Località Crocicchia, 61029 Urbino, ItalyThe Mediterranean Sea is an ideal location to test the response of organisms to hydrological transformations driven by climate change. Here we review studies carried out on planktonic foraminifera and coccolithophores during the late Quaternary and attempt the comparison of data scattered in time and space. We highlight the prompt response of surface water ecosystems to both orbital- and suborbital-climatic variations.https://doi.org/10.1515/geo-2016-0050planktonic foraminiferacoccolithophoresmediterranean sealate quaternary
spellingShingle Incarbona Alessandro
Di Stefano Enrico
Sprovieri Rodolfo
Ferraro Serena
The Uniqueness of Planktonic Ecosystems in the Mediterranean Sea: The Response to Orbital- and Suborbital-Climatic Forcing over the Last 130,000 Years
Open Geosciences
planktonic foraminifera
coccolithophores
mediterranean sea
late quaternary
title The Uniqueness of Planktonic Ecosystems in the Mediterranean Sea: The Response to Orbital- and Suborbital-Climatic Forcing over the Last 130,000 Years
title_full The Uniqueness of Planktonic Ecosystems in the Mediterranean Sea: The Response to Orbital- and Suborbital-Climatic Forcing over the Last 130,000 Years
title_fullStr The Uniqueness of Planktonic Ecosystems in the Mediterranean Sea: The Response to Orbital- and Suborbital-Climatic Forcing over the Last 130,000 Years
title_full_unstemmed The Uniqueness of Planktonic Ecosystems in the Mediterranean Sea: The Response to Orbital- and Suborbital-Climatic Forcing over the Last 130,000 Years
title_short The Uniqueness of Planktonic Ecosystems in the Mediterranean Sea: The Response to Orbital- and Suborbital-Climatic Forcing over the Last 130,000 Years
title_sort uniqueness of planktonic ecosystems in the mediterranean sea the response to orbital and suborbital climatic forcing over the last 130 000 years
topic planktonic foraminifera
coccolithophores
mediterranean sea
late quaternary
url https://doi.org/10.1515/geo-2016-0050
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