TY - JOUR
T1 - Response of primary producers to the hydrographic variability in the southern region of the California current system
AU - Cepeda-Morales, Jushiro
AU - Durazo, Reginaldo
AU - Millán-Núñez, Eduardo
AU - De la Cruz-Orozco, Martín
AU - Sosa-Avalos, Ramón
AU - Espinosa-Carreón, T. Leticia
AU - Soto-Mardones, Luis
AU - Gaxiola-Castro, Gilberto
N1 - Publisher Copyright:
© 2017, Universidad Autonoma de Baja California. All rights reserved.
PY - 2017
Y1 - 2017
N2 - The response of primary producers to seasonal and interannual variabilities in the hydrographic conditions observed between 1997 and 2012 is analyzed for the southern portion of the California Current System (CCS). The analysis uses the optimum rate of primary productivity (PP) normalized by units of chlorophyll (Chla) in the water column (PoptB) and Chla concentration. In situ PP estimations using the14C method were obtained as part of the seasonal cruises conducted by the Investigaciones Mexicanas de la Corriente de California program. Supplementary data included sea surface temperature (SST) as measured by the AVHRR sensor from 1985-2009. We found the mean value of PoptB to be at 5.1 ± 3.3 mg C·(mg Chla)-1·h-1, with maximum ranges of 0.5 and 17.5 mg C·(mg Chla)-1·h-1. The relationship between and PoptB SST suggested a phytoplankton community change at around 19 °C, which characterized the transitional nature of the southern portion of the CCS. SST data suggested, on the one hand, that on average the 19 °C isotherm is located in the vicinity of Punta Eugenia and, on the other, that its spatial variability defined the alternating cool-warm conditions. At the seasonal scale, this isotherm showed a marked latitudinal displacement (from 24°N to 32°N), which was observed to be even out of this range during interannual events associated wiThel Niño/La Niña. Under both cool-warm hydrographic conditions, the phytoplanktonic community showed large PoptB rates (~6 mg C·(mg Chla)-1·h-1). At the interannual scale PoptB, changes were associated to changes in the abundance and composition of nano-microphytoplankton. Additionally, data suggested that high PP rates during warm periods could be attributed to an enhanced picoplankton contribution.
AB - The response of primary producers to seasonal and interannual variabilities in the hydrographic conditions observed between 1997 and 2012 is analyzed for the southern portion of the California Current System (CCS). The analysis uses the optimum rate of primary productivity (PP) normalized by units of chlorophyll (Chla) in the water column (PoptB) and Chla concentration. In situ PP estimations using the14C method were obtained as part of the seasonal cruises conducted by the Investigaciones Mexicanas de la Corriente de California program. Supplementary data included sea surface temperature (SST) as measured by the AVHRR sensor from 1985-2009. We found the mean value of PoptB to be at 5.1 ± 3.3 mg C·(mg Chla)-1·h-1, with maximum ranges of 0.5 and 17.5 mg C·(mg Chla)-1·h-1. The relationship between and PoptB SST suggested a phytoplankton community change at around 19 °C, which characterized the transitional nature of the southern portion of the CCS. SST data suggested, on the one hand, that on average the 19 °C isotherm is located in the vicinity of Punta Eugenia and, on the other, that its spatial variability defined the alternating cool-warm conditions. At the seasonal scale, this isotherm showed a marked latitudinal displacement (from 24°N to 32°N), which was observed to be even out of this range during interannual events associated wiThel Niño/La Niña. Under both cool-warm hydrographic conditions, the phytoplanktonic community showed large PoptB rates (~6 mg C·(mg Chla)-1·h-1). At the interannual scale PoptB, changes were associated to changes in the abundance and composition of nano-microphytoplankton. Additionally, data suggested that high PP rates during warm periods could be attributed to an enhanced picoplankton contribution.
KW - California Current
KW - Chlorophyll
KW - Phytoplankton community
KW - Primary production
KW - Seasonal variability
UR - http://www.scopus.com/inward/record.url?scp=85021925618&partnerID=8YFLogxK
U2 - 10.7773/cm.v43i2.2752
DO - 10.7773/cm.v43i2.2752
M3 - Artículo
SN - 0185-3880
VL - 43
SP - 123
EP - 135
JO - Ciencias Marinas
JF - Ciencias Marinas
IS - 2
ER -