Tore Pool: a singular sediment trap for paleoproductivity in the North Atlantic gyre

International Conference on Paleoceanography (12º. 2016. Utrecht) The Tore pool is a 5.5 km conical deep basin within the Tore seamount, located 300 km off the Iberian margin in the North Atlantic at 40°N of latitude. The vacant Tore seamount acts as a natural, giant sediment trap, and anticipates a...

Full description

Bibliographic Details
Main Authors: Martín Lebreiro, Susana, Antón López, Laura Ángela, Nave, Sílvia, Kissel, Catherine
Format: Conference Object
Language:English
Published: 2022
Subjects:
Online Access:http://hdl.handle.net/10261/273636
id ftcsic:oai:digital.csic.es:10261/273636
record_format openpolar
spelling ftcsic:oai:digital.csic.es:10261/273636 2024-02-11T09:56:44+01:00 Tore Pool: a singular sediment trap for paleoproductivity in the North Atlantic gyre Martín Lebreiro, Susana Antón López, Laura Ángela Nave, Sílvia Kissel, Catherine Atlántico norte 2022-06-28T11:17:14Z http://hdl.handle.net/10261/273636 en eng fdsdfsdf http://hdl.handle.net/10261/273636 open Tore seamount natural sediment-trap ocean productivity deep-sea circulation subtropical gyre comunicación de congreso 2022 ftcsic 2024-01-16T11:26:26Z International Conference on Paleoceanography (12º. 2016. Utrecht) The Tore pool is a 5.5 km conical deep basin within the Tore seamount, located 300 km off the Iberian margin in the North Atlantic at 40°N of latitude. The vacant Tore seamount acts as a natural, giant sediment trap, and anticipates a singular environment where many biogeochemical and physical processes converge into an isolated and confined space from the open deep ocean. Trapped vertical particle flux of surface productivity is deposited without sediment resuspension and erosion by bottom currents. The Tore pool has a restricted gate for exchange of Atlantic deep waters. This implies a potential better preservation of inside deep sea carbonates compared to the North Atlantic open ocean, protected from O-rich Antarctic Bottom Water (AABW) over glacial stages. Additionally, limited O into the pool would favour seldom anoxic conditions by consumption of organic matter. We base our study on the 25 m long Calypso Giant core MD13-3473 taken within the Tore pool, where geochemical and physical analyses are being performed. The sequence covers the last 400 thousand years (down to Marine Isotope Stage 11). Orbital as well as millennial scale climate changes are present in the records. In this case, an accurate stratigraphy is crucial, as it is the identification of occasional gravitational facies, and critical for the purpose of estimation of sedimentation rate and vertical fluxes. Estimation of marine biomass and productivity fluxes in areas of subtropical gyres, contributes to understand capacity of global marine sequestration of atmospheric gases at orbital scale. Instituto Geológico y Minero de España, España Laboratorio Nacional de Energia e Geología, Portugal Laboratoire des Sciences du Climat et de l'Environnement, Centre National de la Recherche Scientifique, France Laboratoire des Sciences du Climat et de l'Environnement, Université Paris-Saclay, France Conference Object Antarc* Antarctic North Atlantic Digital.CSIC (Spanish National Research Council) Antarctic
institution Open Polar
collection Digital.CSIC (Spanish National Research Council)
op_collection_id ftcsic
language English
topic Tore seamount
natural sediment-trap
ocean productivity
deep-sea circulation
subtropical gyre
spellingShingle Tore seamount
natural sediment-trap
ocean productivity
deep-sea circulation
subtropical gyre
Martín Lebreiro, Susana
Antón López, Laura Ángela
Nave, Sílvia
Kissel, Catherine
Tore Pool: a singular sediment trap for paleoproductivity in the North Atlantic gyre
topic_facet Tore seamount
natural sediment-trap
ocean productivity
deep-sea circulation
subtropical gyre
description International Conference on Paleoceanography (12º. 2016. Utrecht) The Tore pool is a 5.5 km conical deep basin within the Tore seamount, located 300 km off the Iberian margin in the North Atlantic at 40°N of latitude. The vacant Tore seamount acts as a natural, giant sediment trap, and anticipates a singular environment where many biogeochemical and physical processes converge into an isolated and confined space from the open deep ocean. Trapped vertical particle flux of surface productivity is deposited without sediment resuspension and erosion by bottom currents. The Tore pool has a restricted gate for exchange of Atlantic deep waters. This implies a potential better preservation of inside deep sea carbonates compared to the North Atlantic open ocean, protected from O-rich Antarctic Bottom Water (AABW) over glacial stages. Additionally, limited O into the pool would favour seldom anoxic conditions by consumption of organic matter. We base our study on the 25 m long Calypso Giant core MD13-3473 taken within the Tore pool, where geochemical and physical analyses are being performed. The sequence covers the last 400 thousand years (down to Marine Isotope Stage 11). Orbital as well as millennial scale climate changes are present in the records. In this case, an accurate stratigraphy is crucial, as it is the identification of occasional gravitational facies, and critical for the purpose of estimation of sedimentation rate and vertical fluxes. Estimation of marine biomass and productivity fluxes in areas of subtropical gyres, contributes to understand capacity of global marine sequestration of atmospheric gases at orbital scale. Instituto Geológico y Minero de España, España Laboratorio Nacional de Energia e Geología, Portugal Laboratoire des Sciences du Climat et de l'Environnement, Centre National de la Recherche Scientifique, France Laboratoire des Sciences du Climat et de l'Environnement, Université Paris-Saclay, France
format Conference Object
author Martín Lebreiro, Susana
Antón López, Laura Ángela
Nave, Sílvia
Kissel, Catherine
author_facet Martín Lebreiro, Susana
Antón López, Laura Ángela
Nave, Sílvia
Kissel, Catherine
author_sort Martín Lebreiro, Susana
title Tore Pool: a singular sediment trap for paleoproductivity in the North Atlantic gyre
title_short Tore Pool: a singular sediment trap for paleoproductivity in the North Atlantic gyre
title_full Tore Pool: a singular sediment trap for paleoproductivity in the North Atlantic gyre
title_fullStr Tore Pool: a singular sediment trap for paleoproductivity in the North Atlantic gyre
title_full_unstemmed Tore Pool: a singular sediment trap for paleoproductivity in the North Atlantic gyre
title_sort tore pool: a singular sediment trap for paleoproductivity in the north atlantic gyre
publishDate 2022
url http://hdl.handle.net/10261/273636
op_coverage Atlántico norte
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
North Atlantic
genre_facet Antarc*
Antarctic
North Atlantic
op_relation fdsdfsdf
http://hdl.handle.net/10261/273636
op_rights open
_version_ 1790605440242941952