2020
DOI: 10.1038/s41598-020-62570-2
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Scavenging crustacean fauna in the Chilean Patagonian Sea

Abstract: The marine ecosystem of the Chilean Patagonia is considered structurally and functionally unique, because it is the transition area between the Antarctic climate and the more temperate Pacific region. However, due to its remoteness, there is little information about Patagonian marine biodiversity, which is a problem in the face of the increasing anthropogenic activity in the area. The aim of this study was to analyze community patterns and environmental characteristics of scavenging crustaceans in the Chilean … Show more

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Cited by 4 publications
(20 citation statements)
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“…The study was carried out in the Magdalena Sound, which is a fjord located in the Puyuhuapi Channel in the Aysén region of Chile (Figure 1). The Magdalena Sound is in front of the town of Puerto Cisnes on Magdalena Island, and is the deepest branch of the Puyuhuapi Channel, approximately 14 km long, 350 m deep and comprised mostly of vertical stone walls [14,15]. The area contains high amounts of dissolved organic matter, both of autochthonous (i.e., primary production) and allochthonous origin (i.e., discharge from rivers and aquaculture activities), and is influenced by the interaction of fresh water and seawater.…”
Section: Study Sitementioning
confidence: 99%
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“…The study was carried out in the Magdalena Sound, which is a fjord located in the Puyuhuapi Channel in the Aysén region of Chile (Figure 1). The Magdalena Sound is in front of the town of Puerto Cisnes on Magdalena Island, and is the deepest branch of the Puyuhuapi Channel, approximately 14 km long, 350 m deep and comprised mostly of vertical stone walls [14,15]. The area contains high amounts of dissolved organic matter, both of autochthonous (i.e., primary production) and allochthonous origin (i.e., discharge from rivers and aquaculture activities), and is influenced by the interaction of fresh water and seawater.…”
Section: Study Sitementioning
confidence: 99%
“…The area contains high amounts of dissolved organic matter, both of autochthonous (i.e., primary production) and allochthonous origin (i.e., discharge from rivers and aquaculture activities), and is influenced by the interaction of fresh water and seawater. This generates estuarine stratification, with the first layer (0-10 m deep) composed of brackish water and the deeper layers composed of seawater of sub-Antarctic origin [14,15]. Data analysis: Bathymetric patterns -The bathymetric patterns of abundance by species were analysed through a correlation analysis between depth strata and abundance of each species and total species [16,17].…”
Section: Study Sitementioning
confidence: 99%
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