Transport of terrestrial organic matter in the Ogooué deep sea turbidite system (Gabon)

2011 ◽  
Vol 28 (5) ◽  
pp. 1061-1072 ◽  
Author(s):  
Laurie Biscara ◽  
Thierry Mulder ◽  
Philippe Martinez ◽  
François Baudin ◽  
Henri Etcheber ◽  
...  
Author(s):  
Johann Schnyder ◽  
Elsa Stetten ◽  
François Baudin ◽  
Audrey M. Pruski ◽  
Philippe Martinez

2020 ◽  
Vol 23 (1-2) ◽  
pp. xx-xx
Author(s):  
FRANÇOIS BAUDIN ◽  
CHRISTOPHE RABOUILLE ◽  
BERNARD DENNIELOU

We address the role of the Congo River sediment dispersal in exporting and trapping organic carbon into deep offshore sediments. Of particular interest is the Congo submarine canyon, which constitutes a permanent link between the terrestrial sediment sources and the marine sink. The Congo River delivers an annual sediment load of ~40 Tg (including 2 Tg of C) that feed a mud-rich turbidite system. Previous estimates of carbon storage capacity in the Congo turbidite system suggest that the terminal lobe complex accounts for ~12% of the surface area of the active turbidite system and accumulates ~18% of the annual input of terrestrial particulate organic carbon exiting the Congo River. In this paper, we extend the approach to the whole active turbidite depositional system by calculating an average burial of terrestrial organic matter in the different environments: canyon, channel, and levees. We estimate that between 33 and 69% of terrestrial carbon exported by the Congo River is ultimately trapped in the different parts of turbidite system and we evaluate their relative efficiency using a source to sink approach. Our carbon budget approach, which consider annual river discharge versus offshore centennial accumulation rates, indicates that about half of the total particulate organic matter delivered yearly by the Congo River watershed escapes the study area or is not correctly estimated by our deep offshore dataset and calculations.


2021 ◽  
pp. 105101
Author(s):  
Arif Hussain ◽  
Peter D.W. Haughton ◽  
Patrick M. Shannon ◽  
Emma A. Morris ◽  
Colm S. Pierce ◽  
...  

Author(s):  
Michel Praet-Van

This ultrastructural investigation of gametogenesis in a deep-sea anemone of the Bay of Biscay trawled around 2000 m depth, contributes to the knowledge of biology and strategy of reproduction of deep-sea benthos.This sea anemone is dioecious. The sperm appears very similar to those of shallow water sea anemones of the genus, Calliactis. The ultrastructural investigation of oogenesis allows the characteristics of the stages of previtellogenesis and vitellogenesis to be defined. The latter begins with a period of lipogenesis correlated with the formation of a trophonema. Mature oocytes measure up to 180 (im in diameter. Study of spermatogenesis and oogenesis reveals that spawning occurs in April/May. In males, the main area of testicular cysts, full of sperm, reaches maximal development from March to May and, in females, the percentage of mature oocytes decreases from 33% in April to 1% in May.Spawning may be induced by the advent in the deep-sea of the products of the spring phytoplankton bloom. This period of spawning, during the increased deposition of organic matter to the deep-sea floor, may be an advantageous strategy for early development of Paracalliactis.


2008 ◽  
Vol 250 (3-4) ◽  
pp. 180-198 ◽  
Author(s):  
Sébastien Garziglia ◽  
Sébastien Migeon ◽  
Emmanuelle Ducassou ◽  
Lies Loncke ◽  
Jean Mascle

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