Reef communities associated with 'dead' cold-water coral framework drive resource retention and recycling in the deep sea

被引:24
|
作者
Maier, Sandra R. [1 ]
Mienis, Furu [2 ]
de Froe, Evert [2 ]
Soetaert, Karline [1 ,3 ]
Lavaleye, Marc [2 ]
Duineveld, Gerard [2 ]
Beauchard, Olivier [1 ]
Kaaden, Anna-Selma van der [1 ]
Koch, Boris P. [4 ,5 ]
van Oevelen, Dick [1 ]
机构
[1] Royal Netherlands Inst Sea Res NIOZ Yerseke, Dept Estuarine & Delta Syst, Yerseke, Netherlands
[2] Royal Netherlands Inst Sea Res NIOZ Texel, Dept Ocean Syst, Den Burg, Netherlands
[3] Univ Ghent, Dept Biol, Marine Biol Res Grp, Ghent, Belgium
[4] Helmholtz Zentrum Polar & Meeresforsch, Alfred Wegener Inst, Bremerhaven, Germany
[5] Univ Appl Sci, Bremerhaven, Germany
关键词
Carbonate mound; Metabolic activity; Rockall bank; Dissolved organic carbon; Dissolved inorganic nitrogen; Suspension feeder; Video transect; ROCKALL TROUGH; LOPHELIA-PERTUSA; NE ATLANTIC; BIOEROSION PATTERNS; PORCUPINE SEABIGHT; NORTHEAST ATLANTIC; TROPHIC STRUCTURE; ORGANIC-MATTER; MOUND; CARBON;
D O I
10.1016/j.dsr.2021.103574
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Cold-water coral (CWC) reefs create hotspots of metabolic activity in the deep sea, in spite of the limited supply of fresh organic matter from the ocean surface (i.e. phytodetritus). We propose that 'dead' coral framework, which harbours diverse faunal and microbial communities, boosts the metabolic activity of the reefs, through enhanced resource retention and recycling. Analysis of a video transect across a 700-540 m-deep CWC mound (Rockall Bank, North-East Atlantic) revealed a high benthic cover of dead framework (64%). Box-cored fragments of dead framework were incubated on-board and showed oxygen consumption rates of 0.078-0.182 mu mol O-2 (mmol organic carbon, i.e. OC)(-1) h(-1), indicating a substantial contribution to the total metabolic activity of the CWC reef. During the incubations, it was shown that the framework degradation stage influences nitrogen (re)cycling, corresponding to differences in community composition. New (less-degraded) framework released ammonium (0.005 +/- 0.001 mu mol NH4+ (mmol OC)(-1) h(-1)), probably due to the activity of ammonotelic macrofauna. In contrast, old (more-degraded) framework released nitrate (0.015 +/- 0.008 mu mol NO3- (mmol OC)(-1) h(-1)), indicating that nitrifying microorganisms recycled fauna-excreted ammonium to nitrate. Furthermore, the framework community removed natural dissolved organic matter (DOM) from the incubation water (0.005-0.122 mu mol C (mmol OC)(-1) h(-1)). Additional feeding experiments showed that all functional groups and macrofauna taxa of the framework community incorporated C-13-enriched ('labelled') DOM, indicating widespread DOM uptake and recycling. Finally, the framework effectively retained C-13-enriched phytodetritus, (a) by physical retention on the biofilm-covered surface and (b) by biological filtration through suspension-feeding fauna. We therefore suggest that the dead framework acts as a 'filtration-recycling factory' that enhances the metabolic activity of CWC reefs. The exposed framework, however, is particularly vulnerable to ocean acidification, jeopardizing this important aspect of CWC reef functioning.
引用
收藏
页数:14
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