2022
DOI: 10.1016/j.dsr.2022.103789
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Habitat associations of post-breeding female southern elephant seals (Mirounga leonina) from Península Valdés, Argentina

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Cited by 2 publications
(3 citation statements)
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“…Based on the SESs path, speed, and swimming pattern, Campagna et al [14] suggested that the shelf area is mainly a transit zone and is not the preferred feeding ground of the SESs females of PV. This was recently confirmed by Mc-Govern et al [15]. Here we propose to use T and S data to characterize the oceanographic conditions along the trajectories of the SESs within the continental shelf, taking advantage of the fact that they crossed it very fast.…”
Section: Introductionmentioning
confidence: 53%
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“…Based on the SESs path, speed, and swimming pattern, Campagna et al [14] suggested that the shelf area is mainly a transit zone and is not the preferred feeding ground of the SESs females of PV. This was recently confirmed by Mc-Govern et al [15]. Here we propose to use T and S data to characterize the oceanographic conditions along the trajectories of the SESs within the continental shelf, taking advantage of the fact that they crossed it very fast.…”
Section: Introductionmentioning
confidence: 53%
“…While at sea, the spatial distribution of females and males is quite different [10]. Males forage mostly on the Patagonian shelf [11] and females mainly along the Patagonian shelf slope, shelf break, or Argentine Basin [12][13][14][15]. SESs females breed between late August and November and molt between December and January along ca.…”
Section: Introductionmentioning
confidence: 99%
“…Most of the records are located within the well-known foraging areas of southern elephant seals from the Península Valdés colony. These include the continental shelf, an area of less than 200 m in depth that extends 300-400 km east from the coast and is characterised by mixed coastal and stratified waters ( Campagna et al 2006 ), the shelf break, where the Malvinas Current carry cold sub-Antarctic waters north from the Antarctic Circumpolar Current and the encounter with low-salinity shelf water originates a shelf-break front associated with temperature and salinity gradients and increased primary productivity ( McGovern et al 2022 ), and the deep Argentine Basin (6000 m), where the warm-salty subtropical waters, carried southwards by the Brazil Current, meet the cold-fresh subpolar waters carried northwards by the Malvinas Current, producing the Brazil-Malvinas Confluence, characterised by increased primary productivity, large temperature gradients and intense mesoscale eddy activity ( Campagna et al 2006 , McGovern et al 2022 ).…”
Section: Geographic Coveragementioning
confidence: 99%