Foraging habitats of lactating northern fur seals are structured by thermocline depths and submesoscale fronts in the eastern Bering Sea

被引:50
|
作者
Nordstrom, Chad A. [1 ,2 ]
Battaile, Brian C. [1 ]
Cotte, Cedric [3 ,4 ]
Trites, Andrew W. [1 ,2 ]
机构
[1] Univ British Columbia, Fisheries Ctr, Marine Mammal Res Unit, AERL, Vancouver, BC V6T 1Z4, Canada
[2] Univ British Columbia, Dept Zool, Vancouver, BC V6T 1Z4, Canada
[3] Ctr Natl Rech Sci, Ctr Etud Biol Chize, F-79360 Villiers En Bois, France
[4] Univ Paris 06, Ctr Natl Rech Sci, Lab Oceanog & Climat Experimentat & Approches Num, Inst Pierre Simon Lapl, Paris, France
基金
美国国家科学基金会;
关键词
Habitat selection; First-passage time; Submesoscale features; Finite-size Lyapunov exponent; Cox proportional hazard model; USA; Alaska; Eastern Bering Sea; POLLOCK THERAGRA-CHALCOGRAMMA; AREA-RESTRICTED SEARCH; CALLORHINUS-URSINUS; PRIBILOF ISLANDS; 1ST-PASSAGE TIME; FINE-SCALE; OCEANOGRAPHIC FEATURES; SPATIAL-DISTRIBUTION; VERTICAL MIGRATION; MARINE PREDATOR;
D O I
10.1016/j.dsr2.2012.07.010
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The relationships between fine-scale oceanographic features, prey aggregations, and the foraging behavior of top predators are poorly understood. We investigated whether foraging patterns of lactating northern fur seals (Callorhinus ursinus) from two breeding colonies located in different oceanographic domains of the eastern Bering Sea (St. Paul Island-shelf; Bogoslof Island-oceanic) were a function of submesoscale oceanographic features. We tested this by tracking 87 lactating fur seals instrumented with bio-logging tags (44 St Paul Island, 43 Bogoslof Island) during July-September, 2009. We identified probable foraging hotspots using first-passage time analysis and statistically linked individual areas of high-use to fine-scale oceanographic features using mixed-effects Cox-proportional hazard models. We found no overlap in foraging areas used by fur seals from the two islands, but a difference in the duration of their foraging trips trips from St. Paul Island were twice as long (7.9 d average) and covered 3-times the distance (600 km average) compared to trips from Bogoslof Island. St. Paul fur seals also foraged at twice the scale (mean radius= 12 km) of Bogoslof fur seals (6 km), which suggests that prey were more diffuse near St Paul Island than prey near Bogoslof Island. Comparing first passage times with oceanographic covariates revealed that foraging hotspots were linked to thermocline depth and occurred near submesoscale surface fronts (eddies and filaments). St Paul fur seals that mixed epipelagic (night) and benthic (day) dives primarily foraged on-shelf in areas with deeper thermoclines that may have concentrated prey closer to the ocean floor, while strictly epipelagic (night) foragers tended to use waters with shallower thermodines that may have aggregated prey closer to the surface. Fur seals from Bogoslof Island foraged almost exclusively over the Bering Sea basin and appeared to hunt intensively along submesoscale fronts that may have converged prey within narrow bands near the surface. Bogoslof fur seals also foraged closer to their island which was surrounded by strong surface fronts, while fur seals from St Paul Island traveled > 100 km and extended some trips off-shelf to the basin to forage at similar oceanographic features. The relative distribution and accessibility of prey-concentrating oceanographic features can account for the observed inter-island foraging patterns, which may in turn have population level consequences for the two fur seal colonies. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:78 / 96
页数:19
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