Anchovy population and ocean-climatic fluctuations in the Humboldt Current System during the last 700 years and their implications
International audience A marine sedimentary record collected from 87 m water depth in a coastal environment of the Humboldt Current System (Mejillones Bay, 23° S, northern Chile) was used to reconstruct the past 700 years of ocean-climatic conditions and to study the influence of any changes on anch...
Published in: | Palaeogeography, Palaeoclimatology, Palaeoecology |
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Main Authors: | , , , , |
Other Authors: | , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2014
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Subjects: | |
Online Access: | https://hal.science/hal-01139589 https://doi.org/10.1016/j.palaeo.2014.08.026 |
id |
ftunivorleans:oai:HAL:hal-01139589v1 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Université d'Orléans: HAL |
op_collection_id |
ftunivorleans |
language |
English |
topic |
Sedimentary record Anchovy population Gleissberg solar cycle Ocean-climatic conditions [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] |
spellingShingle |
Sedimentary record Anchovy population Gleissberg solar cycle Ocean-climatic conditions [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] Guiñez, Marcos Valdés, Jorge Sifeddine, Abdel Boussafir, Mohammed Dávila, Paola M. Anchovy population and ocean-climatic fluctuations in the Humboldt Current System during the last 700 years and their implications |
topic_facet |
Sedimentary record Anchovy population Gleissberg solar cycle Ocean-climatic conditions [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] |
description |
International audience A marine sedimentary record collected from 87 m water depth in a coastal environment of the Humboldt Current System (Mejillones Bay, 23° S, northern Chile) was used to reconstruct the past 700 years of ocean-climatic conditions and to study the influence of any changes on anchovy population dynamics. We analyzed quartz, organic carbon, total nitrogen, alkenones and fish scales. Four stratigraphic units in the sediment column correspond with fluctuations in these and other proxies. Low Scale Deposition Rate (SDR) values from 1330 to 1420 suggest a low abundance of anchovy in this coastal environment. Three subsequent cycles of ca. 170 years each showed an increase and decrease of anchovy populations, which is in agreement with changes in the wind regime, sea surface temperature and primary productivity.Since ca. 1840, marked fluctuations of SDR have been observed, probably as a consequence of the onset of a different oceanographic regime characterized by intensified southern winds and upwelling, colder surface waters, higher primary productivity, and enhanced “La Niña like” interdecadal variability. An increase of the anchovy population was observed until halfway through the 20th century, followed by a decrease, even though water temperature decreased and primary productivity increased. This situation is likely the consequence of the increased fishery activity that developed in this zone during the last 60 years. After analyzing the results obtained for anchovy SDR, we can determine that there is a relation between the abundance of this species and phases of the Pacific Decadal Oscillation (PDO), in which an increase in the SDR coincides with a PDO cold phase, while a decline coincides with a warm phase.Fast Fourier transformation analysis applied to the time series obtained from the Mejillones sediment core and to the North Atlantic Oscillation (NAO), the PDO, and the solar irradiance index time series shows three different decadal cycles (80–100 years, 61–75 years and 45–48 years ... |
author2 |
Biogéochimie-Traceurs-Paléoclimat (BTP) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO) Bureau de Recherches Géologiques et Minières (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Guiñez, Marcos Valdés, Jorge Sifeddine, Abdel Boussafir, Mohammed Dávila, Paola M. |
author_facet |
Guiñez, Marcos Valdés, Jorge Sifeddine, Abdel Boussafir, Mohammed Dávila, Paola M. |
author_sort |
Guiñez, Marcos |
title |
Anchovy population and ocean-climatic fluctuations in the Humboldt Current System during the last 700 years and their implications |
title_short |
Anchovy population and ocean-climatic fluctuations in the Humboldt Current System during the last 700 years and their implications |
title_full |
Anchovy population and ocean-climatic fluctuations in the Humboldt Current System during the last 700 years and their implications |
title_fullStr |
Anchovy population and ocean-climatic fluctuations in the Humboldt Current System during the last 700 years and their implications |
title_full_unstemmed |
Anchovy population and ocean-climatic fluctuations in the Humboldt Current System during the last 700 years and their implications |
title_sort |
anchovy population and ocean-climatic fluctuations in the humboldt current system during the last 700 years and their implications |
publisher |
HAL CCSD |
publishDate |
2014 |
url |
https://hal.science/hal-01139589 https://doi.org/10.1016/j.palaeo.2014.08.026 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_source |
ISSN: 0031-0182 EISSN: 1872-616X Palaeogeography, Palaeoclimatology, Palaeoecology https://hal.science/hal-01139589 Palaeogeography, Palaeoclimatology, Palaeoecology, 2014, 415, pp.210-224. ⟨10.1016/j.palaeo.2014.08.026⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.palaeo.2014.08.026 hal-01139589 https://hal.science/hal-01139589 doi:10.1016/j.palaeo.2014.08.026 IRD: fdi:010063603 |
op_doi |
https://doi.org/10.1016/j.palaeo.2014.08.026 |
container_title |
Palaeogeography, Palaeoclimatology, Palaeoecology |
container_volume |
415 |
container_start_page |
210 |
op_container_end_page |
224 |
_version_ |
1799485562407616512 |
spelling |
ftunivorleans:oai:HAL:hal-01139589v1 2024-05-19T07:45:29+00:00 Anchovy population and ocean-climatic fluctuations in the Humboldt Current System during the last 700 years and their implications Guiñez, Marcos Valdés, Jorge Sifeddine, Abdel Boussafir, Mohammed Dávila, Paola M. Biogéochimie-Traceurs-Paléoclimat (BTP) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) Institut des Sciences de la Terre d'Orléans - UMR7327 (ISTO) Bureau de Recherches Géologiques et Minières (BRGM)-Observatoire des Sciences de l'Univers en région Centre (OSUC) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS) 2014-12 https://hal.science/hal-01139589 https://doi.org/10.1016/j.palaeo.2014.08.026 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.palaeo.2014.08.026 hal-01139589 https://hal.science/hal-01139589 doi:10.1016/j.palaeo.2014.08.026 IRD: fdi:010063603 ISSN: 0031-0182 EISSN: 1872-616X Palaeogeography, Palaeoclimatology, Palaeoecology https://hal.science/hal-01139589 Palaeogeography, Palaeoclimatology, Palaeoecology, 2014, 415, pp.210-224. ⟨10.1016/j.palaeo.2014.08.026⟩ Sedimentary record Anchovy population Gleissberg solar cycle Ocean-climatic conditions [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] info:eu-repo/semantics/article Journal articles 2014 ftunivorleans https://doi.org/10.1016/j.palaeo.2014.08.026 2024-05-02T00:01:54Z International audience A marine sedimentary record collected from 87 m water depth in a coastal environment of the Humboldt Current System (Mejillones Bay, 23° S, northern Chile) was used to reconstruct the past 700 years of ocean-climatic conditions and to study the influence of any changes on anchovy population dynamics. We analyzed quartz, organic carbon, total nitrogen, alkenones and fish scales. Four stratigraphic units in the sediment column correspond with fluctuations in these and other proxies. Low Scale Deposition Rate (SDR) values from 1330 to 1420 suggest a low abundance of anchovy in this coastal environment. Three subsequent cycles of ca. 170 years each showed an increase and decrease of anchovy populations, which is in agreement with changes in the wind regime, sea surface temperature and primary productivity.Since ca. 1840, marked fluctuations of SDR have been observed, probably as a consequence of the onset of a different oceanographic regime characterized by intensified southern winds and upwelling, colder surface waters, higher primary productivity, and enhanced “La Niña like” interdecadal variability. An increase of the anchovy population was observed until halfway through the 20th century, followed by a decrease, even though water temperature decreased and primary productivity increased. This situation is likely the consequence of the increased fishery activity that developed in this zone during the last 60 years. After analyzing the results obtained for anchovy SDR, we can determine that there is a relation between the abundance of this species and phases of the Pacific Decadal Oscillation (PDO), in which an increase in the SDR coincides with a PDO cold phase, while a decline coincides with a warm phase.Fast Fourier transformation analysis applied to the time series obtained from the Mejillones sediment core and to the North Atlantic Oscillation (NAO), the PDO, and the solar irradiance index time series shows three different decadal cycles (80–100 years, 61–75 years and 45–48 years ... Article in Journal/Newspaper North Atlantic North Atlantic oscillation Université d'Orléans: HAL Palaeogeography, Palaeoclimatology, Palaeoecology 415 210 224 |