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Zooplankton long-term changes in the NW Mediterranean Sea: Decadal periodicity forced by winter hydrographic conditions related to large-scale atmospheric changes?

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Title: Zooplankton long-term changes in the NW Mediterranean Sea: Decadal periodicity forced by winter hydrographic conditions related to large-scale atmospheric changes?
Authors: García-Comas, Carmen1,2,3 carmencomas@gmail.com, Stemmann, Lars1,2 stemmann@obs-vlfr.fr, Ibanez, Frédéric1,2, Berline, Léo1,2,4, Mazzocchi, Maria Grazia3, Gasparini, Stéphane1,2, Picheral, Marc1,2, Gorsky, Gabriel1,2
Source: Journal of Marine Systems. Sep2011, Vol. 87 Issue 3/4, p216-226. 11p.
Subjects: Zooplankton, Hydrography, Climate change, Cold weather conditions, North Atlantic oscillation, Salinity, Principal components analysis, Time series analysis
Geographic Terms: Ligurian Sea, Mediterranean Sea
Abstract: Abstract: Copepod, chaetognath, decapod larva, siphonophore and jellyfish monthly abundances, from 1974 to 2003 at Point B (northwestern Mediterranean), were obtained with the ZooScan. Principal component analysis (PCA) was performed on zooplankton, and another PCA on local environment. Almost-decadal periods (1974–1982, 1983–1991, 1992–1999, and 2000–2003) were distinguished in the 1st PC of zooplankton, and that of local environment (1974–1980, 1981–1991, 1992–1998, and 1999–2003). The 1st PC of local environment was correlated with winter North Atlantic Oscillation (NAO) until early 1990s. In early 1980s, all groups increased and the majority of the decade abundances were above the long-term average for most groups. In the 1990s, all decreased, and in early 2000s they increased. This synchrony suggests bottom-up control as main mechanism structuring these groups. The 1980s were characterized by low winter temperature and high salinity. We hypothesize that phytoplankton production was favored during that decade due to increased nutrient uprise to surface by strong winter vertical mixing. In the 1990s salinity decreased probably to the detriment of vertical mixing and carrying capacity of the system. These results stress the role of salinity as physical forcing on water-column stability, in the NW Mediterranean, and the importance of winter conditions to determine the state of pelagic ecosystems. [Copyright &y& Elsevier]
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Database: Engineering Source
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Abstract:Abstract: Copepod, chaetognath, decapod larva, siphonophore and jellyfish monthly abundances, from 1974 to 2003 at Point B (northwestern Mediterranean), were obtained with the ZooScan. Principal component analysis (PCA) was performed on zooplankton, and another PCA on local environment. Almost-decadal periods (1974–1982, 1983–1991, 1992–1999, and 2000–2003) were distinguished in the 1st PC of zooplankton, and that of local environment (1974–1980, 1981–1991, 1992–1998, and 1999–2003). The 1st PC of local environment was correlated with winter North Atlantic Oscillation (NAO) until early 1990s. In early 1980s, all groups increased and the majority of the decade abundances were above the long-term average for most groups. In the 1990s, all decreased, and in early 2000s they increased. This synchrony suggests bottom-up control as main mechanism structuring these groups. The 1980s were characterized by low winter temperature and high salinity. We hypothesize that phytoplankton production was favored during that decade due to increased nutrient uprise to surface by strong winter vertical mixing. In the 1990s salinity decreased probably to the detriment of vertical mixing and carrying capacity of the system. These results stress the role of salinity as physical forcing on water-column stability, in the NW Mediterranean, and the importance of winter conditions to determine the state of pelagic ecosystems. [Copyright &y& Elsevier]
ISSN:09247963
DOI:10.1016/j.jmarsys.2011.04.003