Diel vertical distribution of the larvacean Oikopleura dioica in a North Patagonian tidal frontal system (42°–45°S) of the SW Atlantic Ocean

Abstract: In frontal systems, larvaceans generally comprise a significant fraction of the mesozooplankton. Given the low mobility of these organisms, their vertical distribution is directly influenced by the physical conditions of the water column. The main goal of this study was to investigate the...

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Autores principales: Spinelli, M., Derisio, C., Martos, P., Pájaro, M., Esnal, G., Mianzán, H., Capitanio, F.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_17451000_v11_n6_p633_Spinelli
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spelling todo:paper_17451000_v11_n6_p633_Spinelli2023-10-03T16:31:52Z Diel vertical distribution of the larvacean Oikopleura dioica in a North Patagonian tidal frontal system (42°–45°S) of the SW Atlantic Ocean Spinelli, M. Derisio, C. Martos, P. Pájaro, M. Esnal, G. Mianzán, H. Capitanio, F. Larvaceans oceanographic conditions SW Atlantic Ocean tidal front vertical distribution estuarine front fractionation front intertidal environment invertebrate larva oceanography spawning stabilization turbulent mixing vertical distribution vertical movement water column Atlantic Ocean Atlantic Ocean (Southwest) Patagonia Appendicularia (class) Oikopleura dioica Abstract: In frontal systems, larvaceans generally comprise a significant fraction of the mesozooplankton. Given the low mobility of these organisms, their vertical distribution is directly influenced by the physical conditions of the water column. The main goal of this study was to investigate the day and night vertical distribution of the larvaceans Oikopleura dioica in the different sectors of the Península Valdés tidal front (42°–45°S; SW Atlantic Ocean), focusing on possible causes such as oceanographic conditions (well-mixed, frontal and stratified), feeding activities, reproductive behaviour and predation risks. Day and night samples were collected with a MultiNet of 67 µm and 300 µm mesh size, from two depth layers. Conductivity-temperature-depth (CTD) profiles were also recorded. In the well-mixed waters, the size structure of O. dioica was similar in the upper and lower layers both in the day and night samples, probably due to the continuous vertical movement caused by the turbulent mixing of waters. In the frontal and stratified areas, mature animals were found in the upper layers during the night, possibly due to their aggregation in surface waters for synchronized spawning. In these areas, a high percentage of well-fed larvaceans was also found. Principal component analysis showed that, at night, the abundance of potential predators such as chaetognaths, ctenophores and anchovy larvae was correlated with the parameter of stability of the water column (Simpson parameter), and that these were more abundant in the upper layers of the stratified area containing larvaceans. Our results suggest that the degree of stratification of the water column was the main factor affecting the vertical distribution of O. dioica. © 2015, Taylor & Francis. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_17451000_v11_n6_p633_Spinelli
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Larvaceans
oceanographic conditions
SW Atlantic Ocean
tidal front
vertical distribution
estuarine front
fractionation
front
intertidal environment
invertebrate
larva
oceanography
spawning
stabilization
turbulent mixing
vertical distribution
vertical movement
water column
Atlantic Ocean
Atlantic Ocean (Southwest)
Patagonia
Appendicularia (class)
Oikopleura dioica
spellingShingle Larvaceans
oceanographic conditions
SW Atlantic Ocean
tidal front
vertical distribution
estuarine front
fractionation
front
intertidal environment
invertebrate
larva
oceanography
spawning
stabilization
turbulent mixing
vertical distribution
vertical movement
water column
Atlantic Ocean
Atlantic Ocean (Southwest)
Patagonia
Appendicularia (class)
Oikopleura dioica
Spinelli, M.
Derisio, C.
Martos, P.
Pájaro, M.
Esnal, G.
Mianzán, H.
Capitanio, F.
Diel vertical distribution of the larvacean Oikopleura dioica in a North Patagonian tidal frontal system (42°–45°S) of the SW Atlantic Ocean
topic_facet Larvaceans
oceanographic conditions
SW Atlantic Ocean
tidal front
vertical distribution
estuarine front
fractionation
front
intertidal environment
invertebrate
larva
oceanography
spawning
stabilization
turbulent mixing
vertical distribution
vertical movement
water column
Atlantic Ocean
Atlantic Ocean (Southwest)
Patagonia
Appendicularia (class)
Oikopleura dioica
description Abstract: In frontal systems, larvaceans generally comprise a significant fraction of the mesozooplankton. Given the low mobility of these organisms, their vertical distribution is directly influenced by the physical conditions of the water column. The main goal of this study was to investigate the day and night vertical distribution of the larvaceans Oikopleura dioica in the different sectors of the Península Valdés tidal front (42°–45°S; SW Atlantic Ocean), focusing on possible causes such as oceanographic conditions (well-mixed, frontal and stratified), feeding activities, reproductive behaviour and predation risks. Day and night samples were collected with a MultiNet of 67 µm and 300 µm mesh size, from two depth layers. Conductivity-temperature-depth (CTD) profiles were also recorded. In the well-mixed waters, the size structure of O. dioica was similar in the upper and lower layers both in the day and night samples, probably due to the continuous vertical movement caused by the turbulent mixing of waters. In the frontal and stratified areas, mature animals were found in the upper layers during the night, possibly due to their aggregation in surface waters for synchronized spawning. In these areas, a high percentage of well-fed larvaceans was also found. Principal component analysis showed that, at night, the abundance of potential predators such as chaetognaths, ctenophores and anchovy larvae was correlated with the parameter of stability of the water column (Simpson parameter), and that these were more abundant in the upper layers of the stratified area containing larvaceans. Our results suggest that the degree of stratification of the water column was the main factor affecting the vertical distribution of O. dioica. © 2015, Taylor & Francis.
format JOUR
author Spinelli, M.
Derisio, C.
Martos, P.
Pájaro, M.
Esnal, G.
Mianzán, H.
Capitanio, F.
author_facet Spinelli, M.
Derisio, C.
Martos, P.
Pájaro, M.
Esnal, G.
Mianzán, H.
Capitanio, F.
author_sort Spinelli, M.
title Diel vertical distribution of the larvacean Oikopleura dioica in a North Patagonian tidal frontal system (42°–45°S) of the SW Atlantic Ocean
title_short Diel vertical distribution of the larvacean Oikopleura dioica in a North Patagonian tidal frontal system (42°–45°S) of the SW Atlantic Ocean
title_full Diel vertical distribution of the larvacean Oikopleura dioica in a North Patagonian tidal frontal system (42°–45°S) of the SW Atlantic Ocean
title_fullStr Diel vertical distribution of the larvacean Oikopleura dioica in a North Patagonian tidal frontal system (42°–45°S) of the SW Atlantic Ocean
title_full_unstemmed Diel vertical distribution of the larvacean Oikopleura dioica in a North Patagonian tidal frontal system (42°–45°S) of the SW Atlantic Ocean
title_sort diel vertical distribution of the larvacean oikopleura dioica in a north patagonian tidal frontal system (42°–45°s) of the sw atlantic ocean
url http://hdl.handle.net/20.500.12110/paper_17451000_v11_n6_p633_Spinelli
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