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• W4281570663 abstract "The Strait of Georgia, Canada, is an important region for numerous commercially and culturally important species (e.g., herring, salmon, and orcas), yet little is known about the links between lower trophic level (e.g. phytoplankton and zooplankton) phenology due to historical sampling gaps. Here, we present fourteen years (2003-2016) of data linking interannual variability in phytoplankton and zooplankton phenology in the Central Strait of Georgia, BC. Satellite-derived chlorophyll a (Chl a ) data were used to calculate spring bloom dynamics (bloom initiation, bloom intensity, and bloom magnitude). Average spring bloom initiation occurred during the last week of March in the Central Strait of Georgia. Bloom initiation occurred in mid-to-late February/early March during “early” Chl a bloom years (2004, 2005, and 2015) whereas initiation did not occur until the end of April during “late” bloom years (2007, 2008). Spring Chl a bloom initiation was significantly correlated with the North Pacific Gyre Oscillation (NPGO; r = 0.75, p &lt; 0.01) and spring sea surface temperature (SST; r = -0.70, p &lt; 0.01); spring blooms occurred earlier during warm years. When all environmental variables were considered together, NPGO best explained variations in spring bloom initiation (Adj R 2 = 0.53, p &lt; 0.01) and bloom magnitude (Adj R 2 = 0.57, p &lt; 0.01), whereas stratification best explained variations in bloom intensity (Adj R 2 = 0.38, p &lt; 0.05). Early Chl a blooms were associated with high crustacean abundance (maximum of &gt; 1000 ind m -3 ) but low biomass (37.5 mg m -3 ). Independent of the Chl a data, hierarchical cluster analysis revealed similar groupings of years for crustacean abundance data. Most notably, community composition in cluster Group 2 (2004, 2005, and 2015; early Chl a bloom years), was comprised of a higher proportion of small crustaceans (e.g. non-calanoid copepods) compared to the other cluster groups. To our knowledge, this study provides the first evidence linking early spring Chl a bloom timing to a shift in the crustacean community towards smaller taxa in response to multiple warm events in the Strait of Georgia. Our results show that early Chl a blooms may potentially result in a mismatch between phytoplankton and large energy-rich crustacean zooplankton, with lower abundances of the latter. In contrast, average Chl a bloom years were optimal for large-bodied euphausiids, whereas late Chl a blooms were a match for some crustaceans (e.g., medium calanoid copepods), but not others (e.g., large calanoid copepods and amphipods). We hypothesize that early bloom years may result in poorer feeding conditions for juvenile salmon and other predators in the region." @default.
• W4281570663 created "2022-05-27" @default.
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• W4281570663 date "2022-05-26" @default.
• W4281570663 modified "2023-10-01" @default.
• W4281570663 title "Match/Mismatch Between Phytoplankton and Crustacean Zooplankton Phenology in the Strait of Georgia, Canada" @default.
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• W4281570663 cites W1979588997 @default.
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• W4281570663 cites W1980886119 @default.
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• W4281570663 cites W1987970633 @default.
• W4281570663 cites W1988619277 @default.
• W4281570663 cites W1997776385 @default.
• W4281570663 cites W2000964330 @default.
• W4281570663 cites W2004030008 @default.
• W4281570663 cites W2007583931 @default.
• W4281570663 cites W2008540455 @default.
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• W4281570663 cites W2049547441 @default.
• W4281570663 cites W2050121222 @default.
• W4281570663 cites W2051652436 @default.
• W4281570663 cites W2051723055 @default.
• W4281570663 cites W2053078449 @default.
• W4281570663 cites W2059923548 @default.
• W4281570663 cites W2063466669 @default.
• W4281570663 cites W2064376512 @default.
• W4281570663 cites W2068122514 @default.
• W4281570663 cites W2068264411 @default.
• W4281570663 cites W2069458725 @default.
• W4281570663 cites W2076556909 @default.
• W4281570663 cites W2089018663 @default.
• W4281570663 cites W2091580811 @default.
• W4281570663 cites W2096911721 @default.
• W4281570663 cites W2097886440 @default.
• W4281570663 cites W2108155376 @default.
• W4281570663 cites W2112304786 @default.
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• W4281570663 doi "https://doi.org/10.3389/fmars.2022.832684" @default.
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