The Impact of a Southern Ocean Cyclonic Eddy on Mesopelagic Micronekton

被引:7
作者
Della Penna, Alice [1 ,2 ]
Llort, Joan [3 ]
Moreau, Sebastien [4 ]
Patel, Ramkrushnbhai [5 ,6 ]
Kloser, Rudy [7 ]
Gaube, Peter [8 ]
Strutton, Peter [5 ,6 ]
Boyd, Philip W. [5 ]
机构
[1] Univ Auckland, Inst Marine Sci, Auckland, New Zealand
[2] Univ Auckland, Sch Biol Sci, Auckland, New Zealand
[3] Barcelona Supercomp Ctr, Barcelona, Spain
[4] Norwegian Polar Res Inst, Fram Ctr, Tromso, Norway
[5] Univ Tasmania UTas, Inst Marine & Antarctic Studies IMAS, Hobart, Tas, Australia
[6] Univ Tasmania, Australian Res Council Ctr Excellence Climate Ext, Hobart, Tas, Australia
[7] CSIRO Oceans & Atmosphere, Hobart, Tas, Australia
[8] Univ Washington, Appl Phys Lab, Seattle, WA 98105 USA
基金
澳大利亚研究理事会; 欧盟地平线“2020”;
关键词
mesoscale; eddies; mesopelagic; Southern Ocean; micronekton; acoustics; DEEP-SCATTERING LAYER; MESOSCALE EDDIES; MARINE PREDATORS; ELEPHANT SEALS; CARBON EXPORT; KING PENGUINS; FISHES; ZOOPLANKTON; TRANSPORT; PATTERNS;
D O I
10.1029/2022JC018893
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Mesoscale eddies shape the foraging ecology of predators such as marine mammals and seabirds. A growing number of animal tracking studies show that predators alter their swimming, diving, and foraging behavior within mesoscale eddies. However, little is known about how Southern Ocean eddies influence the distribution of mesopelagic micronekton (fish, squid, and crustaceans), which are major prey items of megafauna. Studies in other oceanic regions have found that eddies can influence the abundance and community composition of micronekton. Here, we analyze acoustic observations from a 14-day survey of a cyclonic mesoscale eddy, its surrounding waters, and the Polar Frontal Zone (PFZ) waters where the eddy formed. We report and interpret spatial patterns of acoustic backscatter at 18 and 75 kHz, proxies indicating combined changes in species, size, and abundance of micronekton. We find that the vertical distribution of acoustic backscatter matched the underwater light conditions characteristic of the eddy core, periphery, and surrounding waters, at scales smaller than 10 km. The median water-column integrated acoustic backscatter values in the eddy core were only half of those measured in the Sub-Antarctic Zone waters surrounding the eddy, but similar to those measured in the PFZ, where the eddy originated 27 days prior. These results suggest that, as for physical and chemical tracers, the eddy maintained its biological characteristics from its source waters creating a unique habitat compared to its surroundings.
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页数:14
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