Landscape Mapping, Ichnological and Benthic Foraminifera Trends in a Deep-Water Gateway, Discovery Gap, NE Atlantic

Multidisciplinary studies have allowed us to describe the abiotic landscapes and, thus, reveal the ichnological and benthic foraminifera trends in a deep-water gateway. Mesoscale landscape mapping is presented based on the bathymetric position index, substrate types and near-bottom water temperature...

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Autores principales: Evgenia V. Dorokhova, Francisco J. Rodríguez-Tovar, Dmitry V. Dorokhov, Liubov A. Kuleshova, Anxo Mena, Tatiana Glazkova, Viktor A. Krechik
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Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:544820b8788443fc9e9ee3fd4b6bb3ff2021-11-25T17:43:14ZLandscape Mapping, Ichnological and Benthic Foraminifera Trends in a Deep-Water Gateway, Discovery Gap, NE Atlantic10.3390/geosciences111104742076-3263https://doaj.org/article/544820b8788443fc9e9ee3fd4b6bb3ff2021-11-01T00:00:00Zhttps://www.mdpi.com/2076-3263/11/11/474https://doaj.org/toc/2076-3263Multidisciplinary studies have allowed us to describe the abiotic landscapes and, thus, reveal the ichnological and benthic foraminifera trends in a deep-water gateway. Mesoscale landscape mapping is presented based on the bathymetric position index, substrate types and near-bottom water temperature. Four sediment cores, retrieved from the entrance, centre and exit of the gap, were subject to computed tomography, ichnological and benthic foraminifera studies. A high diversity of abiotic landscapes in the relatively small area of Discovery Gap is detected and its landscape is characterized by 23 landscape types. The most heterogeneous abiotic factor is a topography that is associated with sediment patchiness and substrate variability. The ichnological and tomographical studies of the sediment cores demonstrate lateral and temporal differences in the macrobenthic tracemaker behaviour. The ichnofossils assemblage of the sediment core can be assigned to the <i>Zoophycos</i> ichnofacies with a higher presence of <i>Zoophycos</i> in the entrance site of the gap and during glacial intervals. Higher benthic foraminifera diversity and species richness during the Holocene are also registered in the southern part of the gap compared to the northern part. The spatial and temporal differences in macro-benthos behavior and benthic foraminifera distribution in the deep-water gateway are proposed to relate to the topographical variations of the Antarctic Bottom Water and its influence on the hydrodynamic regime, nutrient transport, etc.Evgenia V. DorokhovaFrancisco J. Rodríguez-TovarDmitry V. DorokhovLiubov A. KuleshovaAnxo MenaTatiana GlazkovaViktor A. KrechikMDPI AGarticlehabitat mappingbathymetric position indexGIStrace fossilsbenthic foraminiferacomputed tomographyGeologyQE1-996.5ENGeosciences, Vol 11, Iss 474, p 474 (2021)
institution DOAJ
collection DOAJ
language EN
topic habitat mapping
bathymetric position index
GIS
trace fossils
benthic foraminifera
computed tomography
Geology
QE1-996.5
spellingShingle habitat mapping
bathymetric position index
GIS
trace fossils
benthic foraminifera
computed tomography
Geology
QE1-996.5
Evgenia V. Dorokhova
Francisco J. Rodríguez-Tovar
Dmitry V. Dorokhov
Liubov A. Kuleshova
Anxo Mena
Tatiana Glazkova
Viktor A. Krechik
Landscape Mapping, Ichnological and Benthic Foraminifera Trends in a Deep-Water Gateway, Discovery Gap, NE Atlantic
description Multidisciplinary studies have allowed us to describe the abiotic landscapes and, thus, reveal the ichnological and benthic foraminifera trends in a deep-water gateway. Mesoscale landscape mapping is presented based on the bathymetric position index, substrate types and near-bottom water temperature. Four sediment cores, retrieved from the entrance, centre and exit of the gap, were subject to computed tomography, ichnological and benthic foraminifera studies. A high diversity of abiotic landscapes in the relatively small area of Discovery Gap is detected and its landscape is characterized by 23 landscape types. The most heterogeneous abiotic factor is a topography that is associated with sediment patchiness and substrate variability. The ichnological and tomographical studies of the sediment cores demonstrate lateral and temporal differences in the macrobenthic tracemaker behaviour. The ichnofossils assemblage of the sediment core can be assigned to the <i>Zoophycos</i> ichnofacies with a higher presence of <i>Zoophycos</i> in the entrance site of the gap and during glacial intervals. Higher benthic foraminifera diversity and species richness during the Holocene are also registered in the southern part of the gap compared to the northern part. The spatial and temporal differences in macro-benthos behavior and benthic foraminifera distribution in the deep-water gateway are proposed to relate to the topographical variations of the Antarctic Bottom Water and its influence on the hydrodynamic regime, nutrient transport, etc.
format article
author Evgenia V. Dorokhova
Francisco J. Rodríguez-Tovar
Dmitry V. Dorokhov
Liubov A. Kuleshova
Anxo Mena
Tatiana Glazkova
Viktor A. Krechik
author_facet Evgenia V. Dorokhova
Francisco J. Rodríguez-Tovar
Dmitry V. Dorokhov
Liubov A. Kuleshova
Anxo Mena
Tatiana Glazkova
Viktor A. Krechik
author_sort Evgenia V. Dorokhova
title Landscape Mapping, Ichnological and Benthic Foraminifera Trends in a Deep-Water Gateway, Discovery Gap, NE Atlantic
title_short Landscape Mapping, Ichnological and Benthic Foraminifera Trends in a Deep-Water Gateway, Discovery Gap, NE Atlantic
title_full Landscape Mapping, Ichnological and Benthic Foraminifera Trends in a Deep-Water Gateway, Discovery Gap, NE Atlantic
title_fullStr Landscape Mapping, Ichnological and Benthic Foraminifera Trends in a Deep-Water Gateway, Discovery Gap, NE Atlantic
title_full_unstemmed Landscape Mapping, Ichnological and Benthic Foraminifera Trends in a Deep-Water Gateway, Discovery Gap, NE Atlantic
title_sort landscape mapping, ichnological and benthic foraminifera trends in a deep-water gateway, discovery gap, ne atlantic
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/544820b8788443fc9e9ee3fd4b6bb3ff
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