scholarly journals Vertical distribution, population structure and developmental characteristics of the less studied but globally distributed mesopelagic copepod Scaphocalanus magnus in the western Arctic Ocean

2020 ◽  
Vol 42 (3) ◽  
pp. 368-377
Author(s):  
Atsushi Yamaguchi ◽  
Carin J Ashjian ◽  
Robert G Campbell ◽  
Yoshiyuki Abe

Abstract Scaphocalanus magnus is a large copepod species with a worldwide distribution. Information on the ecology of this species is scarce. In this study, S. magnus was collected using vertically stratified net sampling from an ice station in the western Arctic Ocean over a year. The vertical distribution differed between periods of polar night and midnight sun, with core depth distributions of 264–381 m for the polar night and 518–745 m for the midnight sun. The shallower distribution during the polar night may have resulted from the animals moving upwards to find sufficient food during the less productive season. The abundance of early copepodite stages showed clear seasonality. The C2 and C3 stages were abundant June–August and August–September, respectively. After C4, seasonality in abundance was not clear. For C4 and C5, body sizes and masses were greater for males than for females while the opposite was the case for C6. Adult males do not feed and thus have shorter life spans than females, skewing the adult sex ratio towards females. For these mesopelagic particle feeding copepods, a long residence time at C6F suggests that in a varying food environment, it is possible to wait to initiate reproduction until favourable food conditions occur.

2020 ◽  
Vol 39 (9) ◽  
pp. 109-114
Author(s):  
Yanpei Zhuang ◽  
Hongliang Li ◽  
Haiyan Jin ◽  
Shengquan Gao ◽  
Jianfang Chen ◽  
...  

Polar Biology ◽  
2018 ◽  
Vol 42 (2) ◽  
pp. 285-305 ◽  
Author(s):  
Takahito Ikenoue ◽  
Kjell R. Bjørklund ◽  
Amane Fujiwara ◽  
Mario Uchimiya ◽  
Katsunori Kimoto ◽  
...  

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Jang-Mu Heo ◽  
Seong-Su Kim ◽  
Sung-Ho Kang ◽  
Eun Jin Yang ◽  
Ki-Tae Park ◽  
...  

AbstractThe western Arctic Ocean (WAO) has experienced increased heat transport into the region, sea-ice reduction, and changes to the WAO nitrous oxide (N2O) cycles from greenhouse gases. We investigated WAO N2O dynamics through an intensive and precise N2O survey during the open-water season of summer 2017. The effects of physical processes (i.e., solubility and advection) were dominant in both the surface (0–50 m) and deep layers (200–2200 m) of the northern Chukchi Sea with an under-saturation of N2O. By contrast, both the surface layer (0–50 m) of the southern Chukchi Sea and the intermediate (50–200 m) layer of the northern Chukchi Sea were significantly influenced by biogeochemically derived N2O production (i.e., through nitrification), with N2O over-saturation. During summer 2017, the southern region acted as a source of atmospheric N2O (mean: + 2.3 ± 2.7 μmol N2O m−2 day−1), whereas the northern region acted as a sink (mean − 1.3 ± 1.5 μmol N2O m−2 day−1). If Arctic environmental changes continue to accelerate and consequently drive the productivity of the Arctic Ocean, the WAO may become a N2O “hot spot”, and therefore, a key region requiring continued observations to both understand N2O dynamics and possibly predict their future changes.


2009 ◽  
Vol 56 (17) ◽  
pp. 1274-1289 ◽  
Author(s):  
Robert G. Campbell ◽  
Evelyn B. Sherr ◽  
Carin J. Ashjian ◽  
Stéphane Plourde ◽  
Barry F. Sherr ◽  
...  

arktos ◽  
2018 ◽  
Vol 4 (1) ◽  
Author(s):  
Henrik Swärd ◽  
Matt O’Regan ◽  
Christof Pearce ◽  
Igor Semiletov ◽  
Christian Stranne ◽  
...  

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