Evolutionary Palaeoecological and Morphological Response of Globorotalia menardii to Environmental Stress Conditions Preceding the Tortonian–Messinian Boundary in the Mediterranean Basin

The Tortonian–Messinian transition is associated with important climatic and oceanographic changes in the Mediterranean Basin, which have shaped both the biotic and abiotic nature of this setting. The morphological variability of the planktonic foraminifera Globorotalia menardii, a species that is h...

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Published in:Journal of Marine Science and Engineering
Main Authors: Evangelia Besiou, George Kontakiotis, Iuliana Vasiliev, Pierre Moissette, Jean-Jacques Cornée, Assimina Antonarakou
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
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Online Access:https://doi.org/10.3390/jmse11061228
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spelling ftmdpi:oai:mdpi.com:/2077-1312/11/6/1228/ 2023-08-20T04:09:19+02:00 Evolutionary Palaeoecological and Morphological Response of Globorotalia menardii to Environmental Stress Conditions Preceding the Tortonian–Messinian Boundary in the Mediterranean Basin Evangelia Besiou George Kontakiotis Iuliana Vasiliev Pierre Moissette Jean-Jacques Cornée Assimina Antonarakou agris 2023-06-15 application/pdf https://doi.org/10.3390/jmse11061228 EN eng Multidisciplinary Digital Publishing Institute Geological Oceanography https://dx.doi.org/10.3390/jmse11061228 https://creativecommons.org/licenses/by/4.0/ Journal of Marine Science and Engineering; Volume 11; Issue 6; Pages: 1228 planktonic foraminifera upper Miocene Mediterranean Basin size distribution temperature salinity stratification primary productivity thermocline development habitat tracking Text 2023 ftmdpi https://doi.org/10.3390/jmse11061228 2023-08-01T10:29:15Z The Tortonian–Messinian transition is associated with important climatic and oceanographic changes in the Mediterranean Basin, which have shaped both the biotic and abiotic nature of this setting. The morphological variability of the planktonic foraminifera Globorotalia menardii, a species that is highly sensitive to water column structure, has been investigated from the sedimentary archive of three Cretan sections across a west–east transect covering the Tortonian–Messinian Boundary. The present work explicitly focuses on test-size and coiling direction changes occurring during the 7.36–7.24 Ma time slice. On such a short timescale, the most important morphological differentiation accounts for the average size of G. menardii, which is mostly associated with evolutionary adaptation to new ecological niches during the latest Tortonian as a response to the environmental perturbations and ecological stress conditions preceding the Tortonian–Messinian Boundary. A combined thermal and/or salinity-driven stratification and thermocline development hypothesis has been suggested to explain the observed size variability. To ameliorate the accuracy of the proposed model and further determine which environmental parameter reflects the optimum conditions of the analysed species, additional sea surface temperature and salinity data derived from the same sampling intervals of the studied or additional Mediterranean sites are needed. The coiling direction of this species within the study time interval remained constant and not environmentally controlled. Text Planktonic foraminifera MDPI Open Access Publishing Journal of Marine Science and Engineering 11 6 1228
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic planktonic foraminifera
upper Miocene
Mediterranean Basin
size distribution
temperature
salinity
stratification
primary productivity
thermocline development
habitat tracking
spellingShingle planktonic foraminifera
upper Miocene
Mediterranean Basin
size distribution
temperature
salinity
stratification
primary productivity
thermocline development
habitat tracking
Evangelia Besiou
George Kontakiotis
Iuliana Vasiliev
Pierre Moissette
Jean-Jacques Cornée
Assimina Antonarakou
Evolutionary Palaeoecological and Morphological Response of Globorotalia menardii to Environmental Stress Conditions Preceding the Tortonian–Messinian Boundary in the Mediterranean Basin
topic_facet planktonic foraminifera
upper Miocene
Mediterranean Basin
size distribution
temperature
salinity
stratification
primary productivity
thermocline development
habitat tracking
description The Tortonian–Messinian transition is associated with important climatic and oceanographic changes in the Mediterranean Basin, which have shaped both the biotic and abiotic nature of this setting. The morphological variability of the planktonic foraminifera Globorotalia menardii, a species that is highly sensitive to water column structure, has been investigated from the sedimentary archive of three Cretan sections across a west–east transect covering the Tortonian–Messinian Boundary. The present work explicitly focuses on test-size and coiling direction changes occurring during the 7.36–7.24 Ma time slice. On such a short timescale, the most important morphological differentiation accounts for the average size of G. menardii, which is mostly associated with evolutionary adaptation to new ecological niches during the latest Tortonian as a response to the environmental perturbations and ecological stress conditions preceding the Tortonian–Messinian Boundary. A combined thermal and/or salinity-driven stratification and thermocline development hypothesis has been suggested to explain the observed size variability. To ameliorate the accuracy of the proposed model and further determine which environmental parameter reflects the optimum conditions of the analysed species, additional sea surface temperature and salinity data derived from the same sampling intervals of the studied or additional Mediterranean sites are needed. The coiling direction of this species within the study time interval remained constant and not environmentally controlled.
format Text
author Evangelia Besiou
George Kontakiotis
Iuliana Vasiliev
Pierre Moissette
Jean-Jacques Cornée
Assimina Antonarakou
author_facet Evangelia Besiou
George Kontakiotis
Iuliana Vasiliev
Pierre Moissette
Jean-Jacques Cornée
Assimina Antonarakou
author_sort Evangelia Besiou
title Evolutionary Palaeoecological and Morphological Response of Globorotalia menardii to Environmental Stress Conditions Preceding the Tortonian–Messinian Boundary in the Mediterranean Basin
title_short Evolutionary Palaeoecological and Morphological Response of Globorotalia menardii to Environmental Stress Conditions Preceding the Tortonian–Messinian Boundary in the Mediterranean Basin
title_full Evolutionary Palaeoecological and Morphological Response of Globorotalia menardii to Environmental Stress Conditions Preceding the Tortonian–Messinian Boundary in the Mediterranean Basin
title_fullStr Evolutionary Palaeoecological and Morphological Response of Globorotalia menardii to Environmental Stress Conditions Preceding the Tortonian–Messinian Boundary in the Mediterranean Basin
title_full_unstemmed Evolutionary Palaeoecological and Morphological Response of Globorotalia menardii to Environmental Stress Conditions Preceding the Tortonian–Messinian Boundary in the Mediterranean Basin
title_sort evolutionary palaeoecological and morphological response of globorotalia menardii to environmental stress conditions preceding the tortonian–messinian boundary in the mediterranean basin
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/jmse11061228
op_coverage agris
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_source Journal of Marine Science and Engineering; Volume 11; Issue 6; Pages: 1228
op_relation Geological Oceanography
https://dx.doi.org/10.3390/jmse11061228
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/jmse11061228
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