Trophic relationships along a bathymetric gradient at the deep-sea observatory HAUSGARTEN

被引:88
|
作者
Bergmann, Melanie [1 ]
Dannheim, Jennifer [1 ]
Bauerfeind, Eduard [1 ]
Klages, Michael [1 ]
机构
[1] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany
关键词
Arctic; Deep sea; Trophic level; Food web; Megafauna; Nitrogen stable isotope; Deposit feeder; Suspension feeder; ORGANIC-CARBON FLUX; FOOD-WEB STRUCTURE; STABLE-NITROGEN; BENTHIC COMMUNITY; SP-NOV; ICE; WATER; DELTA-N-15; DELTA-C-13; SEDIMENTS;
D O I
10.1016/j.dsr.2008.10.004
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Deep-seafloor communities, especially those from the ice-covered Arctic, are subject to severe food limitation as the amount of particulate organic matter (POM) from the surface is attenuated with increasing depth. Here, we use naturally occurring stable isotope tracers (delta N-15) to broaden our rudimentary knowledge of food web structure and the response of benthic organisms to decreasing food supplies along the bathymetric transect (similar to 1300-5600m water depth) of the deep-sea observatory HAUSGARTEN. Encompassing five trophic levels, the HAUSGARTEN food web is among the longest indicating continuous recycling of organic material typical of food-limited deep-sea ecosystems. The delta N-15 signatures ranged from 3.0 parts per thousand for Foraminifera to 21.4 parts per thousand ( +/- 0.4) for starfish (Poraniomorpha tumida). The majority of organisms occupied the second and third trophic level. Demersal fish fed at the third trophic level, consistent with results from stomach contents analysis. There were significant differences in the delta N-15 signatures of different functional groups with highest delta N-15 values in predators/ scavengers (13.2 +/- 0.29 parts per thousand) followed by suspension feeders (11.2 +/- 0.2 parts per thousand) and deposit feeders (10.2 +/- 0.3 parts per thousand). Depth( = increasing food limitation) affected functional groups in different ways. While the isotopic signatures of predators/scavengers did not change, those of suspension feeders increased with depth, and the reverse was found for deposit feeders. In contrast to the results of other studies, the delta N-15 signatures in POM samples obtained below 800 m did not vary significantly with depth indicating that changes in delta N-15 values are unlikely to be responsible for the depth-related delta N-15 signature changes observed for benthic consumers. However, the delta N-15 signatures of sediments decreased with increasing depth, which also explains the decrease found for deposit feeders. Suspension feeders may rely increasingly on particles trickling down the HAUSGARTEN slope and carrying higher delta N-15 signatures than the decreasing POM supplies, which elevates the delta N-15 value of their tissues. Our results imply that a depth-stratified approach should be taken to avoid a misinterpretation of data obtained at different depths. (c) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:408 / 424
页数:17
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