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

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-hydrolo...

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Main Authors: Juan Carlos Molinero, Li-Chun Tseng, Celeste López Abbate, Eduardo Ramirez-Romero, Jiang-Shiou Hwang
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2018-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC5979015?pdf=render
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author Juan Carlos Molinero
Li-Chun Tseng
Celeste López Abbate
Eduardo Ramirez-Romero
Jiang-Shiou Hwang
author_facet Juan Carlos Molinero
Li-Chun Tseng
Celeste López Abbate
Eduardo Ramirez-Romero
Jiang-Shiou Hwang
author_sort Juan Carlos Molinero
collection DOAJ
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.
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spelling doaj.art-cc4b147914b743ff853b23f7ae450b2c2022-12-22T02:02:28ZengPublic Library of Science (PLoS)PLoS ONE1932-62032018-01-01135e019738210.1371/journal.pone.0197382Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea.Juan Carlos MolineroLi-Chun TsengCeleste López AbbateEduardo Ramirez-RomeroJiang-Shiou HwangClimate 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.http://europepmc.org/articles/PMC5979015?pdf=render
spellingShingle Juan Carlos Molinero
Li-Chun Tseng
Celeste López Abbate
Eduardo Ramirez-Romero
Jiang-Shiou Hwang
Interannual changes in zooplankton echo subtropical and high latitude climate effects in the southern East China Sea.
PLoS ONE
title 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_short 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
url http://europepmc.org/articles/PMC5979015?pdf=render
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