In situ studies of megafaunal mounds indicate rapid sediment turnover and community response at the deep-sea floor

Nature ◽  
1986 ◽  
Vol 323 (6085) ◽  
pp. 251-253 ◽  
Author(s):  
Craig R. Smith ◽  
Peter A. Jumars ◽  
David J. DeMaster
2018 ◽  
Vol 27 (0) ◽  
pp. 87-97 ◽  
Author(s):  
Tadashi Maruyama ◽  
Tomo-o Watsuji ◽  
Tomoko Takahashi ◽  
Hiromi Kayama Watanabe ◽  
Yukiko Nagai ◽  
...  
Keyword(s):  
Deep Sea ◽  

1992 ◽  
Vol 103 (1-3) ◽  
pp. 373-380 ◽  
Author(s):  
P. Cochonat ◽  
R. Le Suavé ◽  
C. Charles ◽  
B. Greger ◽  
M. Hoffert ◽  
...  

2018 ◽  
Author(s):  
Ulrike Braeckman ◽  
Felix Janssen ◽  
Gaute Lavik ◽  
Marcus Elvert ◽  
Hannah Marchant ◽  
...  

Abstract. In the Arctic Ocean, increased sea surface temperature and sea ice retreat have triggered shifts in phytoplankton communities. In Fram Strait, coccolithophorids have been occasionally observed to replace diatoms as the dominating taxon of spring blooms. Deep-sea benthic communities depend strongly on such blooms but with a change in quality and quantity of primarily produced organic matter [OM] input, this may likely have implications for deep-sea life. We compared the in situ responses of Arctic deep-sea benthos to input of phytodetritus from a diatom (Thalassiosira sp.) and a coccolithophorid (Emiliania huxleyi) species. We traced the fate of 13C and 15N labelled phytodetritus into respiration, assimilation by bacteria and infauna in a 4 d and 14 d experiment. Bacteria were key assimilators in the Thalassiosira OM degradation whereas Foraminifera and other infauna were at least as important as bacteria in the Emiliania OM assimilation. After 14 d, 5 times less carbon and 3.8 times less nitrogen of the Emiliania detritus was recycled compared to Thalassiosira detritus. This implies that the utilization of Emiliania OM may be less efficient than for Thalassiosira OM. Our results indicate that a shift from diatom-dominated input to a coccolithophorid-dominated pulse could entail a delay in OM cycling, which may affect bentho-pelagic coupling.


2018 ◽  
Vol 15 (21) ◽  
pp. 6537-6557 ◽  
Author(s):  
Ulrike Braeckman ◽  
Felix Janssen ◽  
Gaute Lavik ◽  
Marcus Elvert ◽  
Hannah Marchant ◽  
...  

Abstract. In the Arctic Ocean, increased sea surface temperature and sea ice retreat have triggered shifts in phytoplankton communities. In Fram Strait, coccolithophorids have been occasionally observed to replace diatoms as the dominating taxon of spring blooms. Deep-sea benthic communities depend strongly on such blooms, but with a change in quality and quantity of primarily produced organic matter (OM) input, this may likely have implications for deep-sea life. We compared the in situ responses of Arctic deep-sea benthos to input of phytodetritus from a diatom (Thalassiosira sp.) and a coccolithophorid (Emiliania huxleyi) species. We traced the fate of 13C- and 15N-labelled phytodetritus into respiration, assimilation by bacteria and infauna in a 4-day and 14-day experiment. Bacteria were key assimilators in the Thalassiosira OM degradation, whereas Foraminifera and other infauna were at least as important as bacteria in the Emiliania OM assimilation. After 14 days, 5 times less carbon and 3.8 times less nitrogen of the Emiliania detritus was recycled compared to Thalassiosira detritus. This implies that the utilization of Emiliania OM may be less efficient than for Thalassiosira OM. Our results indicate that a shift from diatom-dominated input to a coccolithophorid-dominated pulse could entail a delay in OM cycling, which may affect benthopelagic coupling.


2017 ◽  
Author(s):  
Eriko Shimada ◽  
Yusuke Tsuruwaka

We recently found Cribrinopsis japonica Tsutsui & Tsuruwaka, 2014 (Shinkai-hakutou-ginchaku in Japanese name) at the depth between 384 and 800 m in Toyama Bay, Sea of Japan. Since then, C. japonica has been reared under atmospheric pressure in the laboratory for seven years. C. japonica may use a fluorescent protein carried in its tentacles to lure shrimp (Tsutsui et al., 2016*1). However, the ecology of C. japonica in the deep-sea is hardly known. To elucidate the unknown ecology, we coupled one of the first long-term in situ studies of deep-sea organisms with complementary laboratory experiments. Our exploration of deep-sea benthos revealed that C. japonica inhabits the deepest areas of the sea floor at 1,960 m. Moreover, 80% of C. japonica in the deep-sea stayed together with the deep-sea shrimp. In the laboratory environment, when we added the same shrimp species which was observed in situ to the rearing tank with C. japonica, C. japonica stayed closer with the shrimp without attacking using the tentacles. It is rare to observe different animals together at one place or space since there are very few animals in the ocean floor at > 1,000 m depth in the Sea of Japan (Motokawa & Kajihara, 2017*2). In such depopulated environment, it is conceivable that C. japonica and the shrimp may receive benefit mutually or one side by establishing a ‘symbiotic relationship.’ We will elucidate their relationship in more details by studying the possible ‘symbiosis’ in the laboratory.


1980 ◽  
Vol 27 (10) ◽  
pp. 867-872 ◽  
Author(s):  
H.W. Jannasch ◽  
R.L. Cuhel ◽  
C.O. Wirsen ◽  
C.D. Taylor
Keyword(s):  
Deep Sea ◽  

1983 ◽  
Vol 78 (1) ◽  
pp. 69-73 ◽  
Author(s):  
C. O. Wirsen ◽  
H. W. Jannasch

2017 ◽  
Author(s):  
Eriko Shimada ◽  
Yusuke Tsuruwaka

We recently found Cribrinopsis japonica Tsutsui & Tsuruwaka, 2014 (Shinkai-hakutou-ginchaku in Japanese name) at the depth between 384 and 800 m in Toyama Bay, Sea of Japan. Since then, C. japonica has been reared under atmospheric pressure in the laboratory for seven years. C. japonica may use a fluorescent protein carried in its tentacles to lure shrimp (Tsutsui et al., 2016*1). However, the ecology of C. japonica in the deep-sea is hardly known. To elucidate the unknown ecology, we coupled one of the first long-term in situ studies of deep-sea organisms with complementary laboratory experiments. Our exploration of deep-sea benthos revealed that C. japonica inhabits the deepest areas of the sea floor at 1,960 m. Moreover, 80% of C. japonica in the deep-sea stayed together with the deep-sea shrimp. In the laboratory environment, when we added the same shrimp species which was observed in situ to the rearing tank with C. japonica, C. japonica stayed closer with the shrimp without attacking using the tentacles. It is rare to observe different animals together at one place or space since there are very few animals in the ocean floor at > 1,000 m depth in the Sea of Japan (Motokawa & Kajihara, 2017*2). In such depopulated environment, it is conceivable that C. japonica and the shrimp may receive benefit mutually or one side by establishing a ‘symbiotic relationship.’ We will elucidate their relationship in more details by studying the possible ‘symbiosis’ in the laboratory.


2017 ◽  
Vol 23 ◽  
pp. 29-37 ◽  
Author(s):  
Thomas Pape ◽  
Hans-Jürgen Hohnberg ◽  
David Wunsch ◽  
Erik Anders ◽  
Tim Freudenthal ◽  
...  

Abstract. Pressure barrels for sampling and preservation of submarine sediments under in situ pressure with the robotic sea-floor drill rig MeBo (Meeresboden-Bohrgerät) housed at the MARUM (Bremen, Germany) were developed. Deployments of the so-called MDP (MeBo pressure vessel) during two offshore expeditions off New Zealand and off Spitsbergen, Norway, resulted in the recovery of sediment cores with pressure stages equaling in situ hydrostatic pressure. While initially designed for the quantification of gas and gas-hydrate contents in submarine sediments, the MDP also allows for analysis of the sediments under in situ pressure with methods typically applied by researchers from other scientific fields (geotechnics, sedimentology, microbiology, etc.). Here we report on the design and operational procedure of the MDP and demonstrate full functionality by presenting the first results from pressure-core degassing and molecular gas analysis.


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