Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea

Autores
Molinero, Juan Carlos; Tseng, Li-Chun; López Abbate, María Celeste; Ramirez-Romero, Eduardo; Hwang, Jiang-Shiou
Año de publicación
2018
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Climate variability plays a central role in the dynamics of marine pelagic ecosystems shaping the structure and abundance changes of plankton communities, thereby affecting energy pathways and biogeochemical fluxes in the ocean. Here we have investigated complex interactions driven a climate-hydrology-plankton system in the southern East China Sea over the period 2000 to 2012. In particular, we aimed at quantifying the influence of climate phenomena playing out in tropical (El Nino 3.4) and middle-high latitudes (East Asia Winter Monsoon, EAWM, and Pacific Decadal Oscillation, PDO) on pelagic copepods. We found that the EAWM and El Nino 3.4 showed a non-stationary and non-linear relationship with local temperature variability. In the two cases, the strength of the relationship, as indexed by the wavelet coherence analysis, decreased along with the positive phase of the PDO. Likewise, the influence of EAWM and El Nino3.4 on copepods exhibited a non-stationary link that changed along with the PDO state. Indeed, copepods and EAWM were closely related during the positive phase, while the link copepods–El Nino 3.4 was stronger during the negative phase. Our results pointed out cascading effects from climate to plankton driven by the positive phase of the PDO through its effect on temperature conditions, and likely through a larger southward transport of nutrient-rich water masses to northern Taiwan and the Taiwan Strait. We suggest a chain of mechanisms whereby the PDO shapes interannual dynamics of pelagic copepods and highlight that these results have implications for integrative management measures, as pelagic copepods plays a prominent role in food web dynamics and for harvested fish in the East China Sea.
Fil: Molinero, Juan Carlos. Geomar-Helmholtz Centre for Ocean Research Kiel; Alemania. Université Montpellier II; Francia
Fil: Tseng, Li-Chun. National Taiwan Ocena University; China
Fil: López Abbate, María Celeste. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Argentino de Oceanografía. Universidad Nacional del Sur. Instituto Argentino de Oceanografía; Argentina
Fil: Ramirez-Romero, Eduardo. Consejo Superior de Investigaciones Cientificas. Instituto Mediterraneo de Estudios Avanzados; España
Fil: Hwang, Jiang-Shiou. National Taiwan Ocena University; China
Materia
Zooplankton
Climate Signals
East China Sea
Non-Linear Response
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/91979

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network_name_str CONICET Digital (CONICET)
spelling Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China SeaMolinero, Juan CarlosTseng, Li-ChunLópez Abbate, María CelesteRamirez-Romero, EduardoHwang, Jiang-ShiouZooplanktonClimate SignalsEast China SeaNon-Linear Responsehttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Climate variability plays a central role in the dynamics of marine pelagic ecosystems shaping the structure and abundance changes of plankton communities, thereby affecting energy pathways and biogeochemical fluxes in the ocean. Here we have investigated complex interactions driven a climate-hydrology-plankton system in the southern East China Sea over the period 2000 to 2012. In particular, we aimed at quantifying the influence of climate phenomena playing out in tropical (El Nino 3.4) and middle-high latitudes (East Asia Winter Monsoon, EAWM, and Pacific Decadal Oscillation, PDO) on pelagic copepods. We found that the EAWM and El Nino 3.4 showed a non-stationary and non-linear relationship with local temperature variability. In the two cases, the strength of the relationship, as indexed by the wavelet coherence analysis, decreased along with the positive phase of the PDO. Likewise, the influence of EAWM and El Nino3.4 on copepods exhibited a non-stationary link that changed along with the PDO state. Indeed, copepods and EAWM were closely related during the positive phase, while the link copepods–El Nino 3.4 was stronger during the negative phase. Our results pointed out cascading effects from climate to plankton driven by the positive phase of the PDO through its effect on temperature conditions, and likely through a larger southward transport of nutrient-rich water masses to northern Taiwan and the Taiwan Strait. We suggest a chain of mechanisms whereby the PDO shapes interannual dynamics of pelagic copepods and highlight that these results have implications for integrative management measures, as pelagic copepods plays a prominent role in food web dynamics and for harvested fish in the East China Sea.Fil: Molinero, Juan Carlos. Geomar-Helmholtz Centre for Ocean Research Kiel; Alemania. Université Montpellier II; FranciaFil: Tseng, Li-Chun. National Taiwan Ocena University; ChinaFil: López Abbate, María Celeste. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Argentino de Oceanografía. Universidad Nacional del Sur. Instituto Argentino de Oceanografía; ArgentinaFil: Ramirez-Romero, Eduardo. Consejo Superior de Investigaciones Cientificas. Instituto Mediterraneo de Estudios Avanzados; EspañaFil: Hwang, Jiang-Shiou. National Taiwan Ocena University; ChinaPublic Library of Science2018-05-31info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/91979Molinero, Juan Carlos; Tseng, Li-Chun; López Abbate, María Celeste; Ramirez-Romero, Eduardo; Hwang, Jiang-Shiou; Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea; Public Library of Science; Plos One; 13; 5; 31-5-2018; 1-71932-6203CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0197382info:eu-repo/semantics/altIdentifier/doi/10.1371/journal.pone.0197382info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:35:12Zoai:ri.conicet.gov.ar:11336/91979instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:35:12.35CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea
title Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea
spellingShingle Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea
Molinero, Juan Carlos
Zooplankton
Climate Signals
East China Sea
Non-Linear Response
title_short Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea
title_full Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea
title_fullStr Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea
title_full_unstemmed Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea
title_sort Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea
dc.creator.none.fl_str_mv Molinero, Juan Carlos
Tseng, Li-Chun
López Abbate, María Celeste
Ramirez-Romero, Eduardo
Hwang, Jiang-Shiou
author Molinero, Juan Carlos
author_facet Molinero, Juan Carlos
Tseng, Li-Chun
López Abbate, María Celeste
Ramirez-Romero, Eduardo
Hwang, Jiang-Shiou
author_role author
author2 Tseng, Li-Chun
López Abbate, María Celeste
Ramirez-Romero, Eduardo
Hwang, Jiang-Shiou
author2_role author
author
author
author
dc.subject.none.fl_str_mv Zooplankton
Climate Signals
East China Sea
Non-Linear Response
topic Zooplankton
Climate Signals
East China Sea
Non-Linear Response
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Climate variability plays a central role in the dynamics of marine pelagic ecosystems shaping the structure and abundance changes of plankton communities, thereby affecting energy pathways and biogeochemical fluxes in the ocean. Here we have investigated complex interactions driven a climate-hydrology-plankton system in the southern East China Sea over the period 2000 to 2012. In particular, we aimed at quantifying the influence of climate phenomena playing out in tropical (El Nino 3.4) and middle-high latitudes (East Asia Winter Monsoon, EAWM, and Pacific Decadal Oscillation, PDO) on pelagic copepods. We found that the EAWM and El Nino 3.4 showed a non-stationary and non-linear relationship with local temperature variability. In the two cases, the strength of the relationship, as indexed by the wavelet coherence analysis, decreased along with the positive phase of the PDO. Likewise, the influence of EAWM and El Nino3.4 on copepods exhibited a non-stationary link that changed along with the PDO state. Indeed, copepods and EAWM were closely related during the positive phase, while the link copepods–El Nino 3.4 was stronger during the negative phase. Our results pointed out cascading effects from climate to plankton driven by the positive phase of the PDO through its effect on temperature conditions, and likely through a larger southward transport of nutrient-rich water masses to northern Taiwan and the Taiwan Strait. We suggest a chain of mechanisms whereby the PDO shapes interannual dynamics of pelagic copepods and highlight that these results have implications for integrative management measures, as pelagic copepods plays a prominent role in food web dynamics and for harvested fish in the East China Sea.
Fil: Molinero, Juan Carlos. Geomar-Helmholtz Centre for Ocean Research Kiel; Alemania. Université Montpellier II; Francia
Fil: Tseng, Li-Chun. National Taiwan Ocena University; China
Fil: López Abbate, María Celeste. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Argentino de Oceanografía. Universidad Nacional del Sur. Instituto Argentino de Oceanografía; Argentina
Fil: Ramirez-Romero, Eduardo. Consejo Superior de Investigaciones Cientificas. Instituto Mediterraneo de Estudios Avanzados; España
Fil: Hwang, Jiang-Shiou. National Taiwan Ocena University; China
description Climate variability plays a central role in the dynamics of marine pelagic ecosystems shaping the structure and abundance changes of plankton communities, thereby affecting energy pathways and biogeochemical fluxes in the ocean. Here we have investigated complex interactions driven a climate-hydrology-plankton system in the southern East China Sea over the period 2000 to 2012. In particular, we aimed at quantifying the influence of climate phenomena playing out in tropical (El Nino 3.4) and middle-high latitudes (East Asia Winter Monsoon, EAWM, and Pacific Decadal Oscillation, PDO) on pelagic copepods. We found that the EAWM and El Nino 3.4 showed a non-stationary and non-linear relationship with local temperature variability. In the two cases, the strength of the relationship, as indexed by the wavelet coherence analysis, decreased along with the positive phase of the PDO. Likewise, the influence of EAWM and El Nino3.4 on copepods exhibited a non-stationary link that changed along with the PDO state. Indeed, copepods and EAWM were closely related during the positive phase, while the link copepods–El Nino 3.4 was stronger during the negative phase. Our results pointed out cascading effects from climate to plankton driven by the positive phase of the PDO through its effect on temperature conditions, and likely through a larger southward transport of nutrient-rich water masses to northern Taiwan and the Taiwan Strait. We suggest a chain of mechanisms whereby the PDO shapes interannual dynamics of pelagic copepods and highlight that these results have implications for integrative management measures, as pelagic copepods plays a prominent role in food web dynamics and for harvested fish in the East China Sea.
publishDate 2018
dc.date.none.fl_str_mv 2018-05-31
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/91979
Molinero, Juan Carlos; Tseng, Li-Chun; López Abbate, María Celeste; Ramirez-Romero, Eduardo; Hwang, Jiang-Shiou; Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea; Public Library of Science; Plos One; 13; 5; 31-5-2018; 1-7
1932-6203
CONICET Digital
CONICET
url http://hdl.handle.net/11336/91979
identifier_str_mv Molinero, Juan Carlos; Tseng, Li-Chun; López Abbate, María Celeste; Ramirez-Romero, Eduardo; Hwang, Jiang-Shiou; Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea; Public Library of Science; Plos One; 13; 5; 31-5-2018; 1-7
1932-6203
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0197382
info:eu-repo/semantics/altIdentifier/doi/10.1371/journal.pone.0197382
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Public Library of Science
publisher.none.fl_str_mv Public Library of Science
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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