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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/91979
Ver los metadatos del registro completo
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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 |
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CONICET Digital (CONICET) |
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CONICET Digital (CONICET) |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
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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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13.070432 |