Sedimentary Organic Carbon Budget Across the Slope to the Basin in the Southwestern Ulleung (Tsushima) Basin of the East (Japan) Sea

2019 ◽  
Vol 124 (9) ◽  
pp. 2804-2822
Author(s):  
Jae Seong Lee ◽  
Jeong Hee Han ◽  
Sung‐Uk An ◽  
Sung‐Han Kim ◽  
Dhongil Lim ◽  
...  
2014 ◽  
Vol 49 (4) ◽  
pp. 433-447 ◽  
Author(s):  
Jae Seong Lee ◽  
Jeong Hee Han ◽  
Sung-Uk An ◽  
Taehee Na ◽  
Jung No Kwon ◽  
...  

2006 ◽  
Vol 63 (3-4) ◽  
pp. 155-161 ◽  
Author(s):  
Grete Algesten ◽  
Lars Brydsten ◽  
Per Jonsson ◽  
Pirkko Kortelainen ◽  
Stefan Löfgren ◽  
...  

2015 ◽  
Vol 100 (1) ◽  
pp. 476-482 ◽  
Author(s):  
Aurora M. Ricart ◽  
Paul H. York ◽  
Michael A. Rasheed ◽  
Marta Pérez ◽  
Javier Romero ◽  
...  

2007 ◽  
Vol 54 (9) ◽  
pp. 1530-1548 ◽  
Author(s):  
Diana Zúñiga ◽  
Antoni Calafat ◽  
Anna Sanchez-Vidal ◽  
Miquel Canals ◽  
Brian Price ◽  
...  

2008 ◽  
Vol 65 (3) ◽  
pp. 543-548 ◽  
Author(s):  
Yves T Prairie

In this perspective article, I argue that dissolved organic carbon occupies a central role in the functioning of lake ecosystems, comparable in importance to that played by nutrients. Because lakes receive so much dissolved organic carbon from the terrestrial landscape, its accumulation in water bodies usually represents the largest pool of lacustrine organic matter within the water column. The transformation of even a small fraction of this external carbon by the microbial community can alter significantly the metabolic balance of lake ecosystems, simultaneously releasing carbon dioxide to the atmosphere and burying organic carbon in lake sediments. At the landscape level, even if they occupy a small fraction of the landscape, lakes play a surprisingly important role in the regional carbon budget, particularly when considered at the appropriate temporal scale.


2011 ◽  
Vol 8 (11) ◽  
pp. 3219-3230 ◽  
Author(s):  
K. Kuliński ◽  
J. Pempkowiak

Abstract. This paper presents the results of a comprehensive study of the Baltic Sea carbon budget. The Baltic Sea is very much influenced by terrestrial carbon input. Rivers are the largest carbon source, and their input amounts to 10.90 Tg C yr−1 (Tg = 1012 g) with a 37.5% contribution of organic carbon. On the other hand, carbon is effectively exported from the Baltic to the North Sea (7.67 Tg C yr−1) and is also buried in bottom sediments (2.73 Tg C yr−1). The other sources and sinks of carbon are of minor importance. The net CO2 emission (1.05 Tg C yr−1) from the Baltic to the atmosphere was calculated as the closing term of the carbon budget presented here. There is a net loss of organic carbon, which indicates that the Baltic Sea is heterotrophic.


2012 ◽  
Vol 68 (7) ◽  
pp. III_493-III_498
Author(s):  
Megumu FUJIBAYASHI ◽  
Munehiro NOMURA ◽  
Xiaoguang XU ◽  
Xianning LI ◽  
Yoshio AIKAWA ◽  
...  

2016 ◽  
Vol 116 ◽  
pp. 49-76 ◽  
Author(s):  
William Z. Haskell ◽  
Maria G. Prokopenko ◽  
Douglas E. Hammond ◽  
Rachel H.R. Stanley ◽  
William M. Berelson ◽  
...  

2017 ◽  
Vol 14 (2) ◽  
pp. 301-310 ◽  
Author(s):  
Carlos M. Duarte

Abstract. Vegetated coastal habitats, including seagrass and macroalgal beds, mangrove forests and salt marshes, form highly productive ecosystems, but their contribution to the global carbon budget remains overlooked, and these forests remain hidden in representations of the global carbon budget. Despite being confined to a narrow belt around the shoreline of the world's oceans, where they cover less than 7 million km2, vegetated coastal habitats support about 1 to 10 % of the global marine net primary production and generate a large organic carbon surplus of about 40 % of their net primary production (NPP), which is either buried in sediments within these habitats or exported away. Large, 10-fold uncertainties in the area covered by vegetated coastal habitats, along with variability about carbon flux estimates, result in a 10-fold bracket around the estimates of their contribution to organic carbon sequestration in sediments and the deep sea from 73 to 866 Tg C yr−1, representing between 3 % and 1∕3 of oceanic CO2 uptake. Up to 1∕2 of this carbon sequestration occurs in sink reservoirs (sediments or the deep sea) beyond these habitats. The organic carbon exported that does not reach depositional sites subsidizes the metabolism of heterotrophic organisms. In addition to a significant contribution to organic carbon production and sequestration, vegetated coastal habitats contribute as much to carbonate accumulation as coral reefs do. While globally relevant, the magnitude of global carbon fluxes supported by salt-marsh, mangrove, seagrass and macroalgal habitats is declining due to rapid habitat loss, contributing to loss of CO2 sequestration, storage capacity and carbon subsidies. Incorporating the carbon fluxes' vegetated coastal habitats' support into depictions of the carbon budget of the global ocean and its perturbations will improve current representations of the carbon budget of the global ocean.


2018 ◽  
Vol 25 (9) ◽  
pp. 8497-8511 ◽  
Author(s):  
Siyu Huang ◽  
Junbing Pu ◽  
Jianhua Cao ◽  
Jianhong Li ◽  
Tao Zhang ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document