Articles | Volume 10, issue 2
https://doi.org/10.5194/cp-10-569-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/cp-10-569-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
21 Mar 2014
Research article |
| 21 Mar 2014
Towards an improved organic carbon budget for the western Barents Sea shelf
I. Pathirana
University of Tromsø, Department of Geology, 9011 Tromsø, Norway
Geological Survey of Norway, 7491 Trondheim, Norway
J. Knies
Centre for Arctic Gas Hydrate, Environment and Climate, University of Tromsø, 9037 Tromsø, Norway
Geological Survey of Norway, 7491 Trondheim, Norway
M. Felix
SINTEF Basin Modelling Department, 7465 Trondheim, Norway
U. Mann
SINTEF Basin Modelling Department, 7465 Trondheim, Norway
currently at: Statoil Research Center, Arkitekt Ebbells veg 10, 7005 Trondheim, Norway
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Cited
16 citations as recorded by crossref.
- Carbon dioxide sink in the Arctic Ocean from cross-shelf transport of dense Barents Sea water A. Rogge et al. 10.1038/s41561-022-01069-z
- Hot shale in an ice world: Paleoceanographic evolution of the northern Gondwana margin during the early Paleozoic (Tanezzuft Formation, Tunisia) G. Gambacorta et al. 10.1016/j.marpetgeo.2016.02.015
- The influence of paleo-bathymetry on total organic carbon distribution tested in the Cretaceous Hammerfest Basin, Barents Sea B. Emmel et al. 10.1016/j.marpetgeo.2018.09.003
- Distribution Features of 238U, 232Th, and 226Ra in Bottom Sediments of the Shelf and Continental Slope of Svalbard M. Domanov 10.1134/S1066362224010144
- Particle sources and downward fluxes in the eastern Fram strait under the influence of the west Spitsbergen current A. Sanchez-Vidal et al. 10.1016/j.dsr.2015.06.002
- Distribution features of <sup>238</sup>U, <sup>232</sup>Th and <sup>226</sup>Ra in bottom sediments of the shelf and continental slope of Svalbard M. Domanov 10.31857/S0033831124010148
- The Pleistocene contribution to the net erosion and sedimentary conditions in the outer Bear Island Trough, western Barents Sea K. Zieba et al. 10.1007/s41063-016-0022-3
- Postglacial paleoceanography of the western Barents Sea: Implications for alkenone-based sea surface temperatures and primary productivity M. Łącka et al. 10.1016/j.quascirev.2019.105973
- Transformation of organic matter in a Barents Sea sediment profile: coupled geochemical and microbiological processes M. Stevenson et al. 10.1098/rsta.2020.0223
- New evidence for preservation of contemporary marine organic carbon by iron in Arctic shelf sediments J. Faust et al. 10.1088/1748-9326/aca780
- Middle to late Holocene paleoproductivity reconstructions for the western Barents Sea: a model-data comparison I. Pathirana et al. 10.1007/s41063-015-0002-z
- Microbial Communities Involved in Methane, Sulfur, and Nitrogen Cycling in the Sediments of the Barents Sea S. Begmatov et al. 10.3390/microorganisms9112362
- Does Arctic warming reduce preservation of organic matter in Barents Sea sediments? J. Faust et al. 10.1098/rsta.2019.0364
- Structural and stratigraphic controls on subsurface fluid flow at the Veslemøy High, SW Barents Sea S. Chand et al. 10.1016/j.marpetgeo.2014.06.004
- Benthic macrofaunal bioturbation activities from shelf to deep basin in spring to summer transition in the Arctic Ocean B. Oleszczuk et al. 10.1016/j.marenvres.2019.06.008
- Brine formation in relation to climate changes and ice retreat during the last 15,000 years in Storfjorden, Svalbard, 76–78°N T. Rasmussen & E. Thomsen 10.1002/2014PA002643
14 citations as recorded by crossref.
- Carbon dioxide sink in the Arctic Ocean from cross-shelf transport of dense Barents Sea water A. Rogge et al. 10.1038/s41561-022-01069-z
- Hot shale in an ice world: Paleoceanographic evolution of the northern Gondwana margin during the early Paleozoic (Tanezzuft Formation, Tunisia) G. Gambacorta et al. 10.1016/j.marpetgeo.2016.02.015
- The influence of paleo-bathymetry on total organic carbon distribution tested in the Cretaceous Hammerfest Basin, Barents Sea B. Emmel et al. 10.1016/j.marpetgeo.2018.09.003
- Distribution Features of 238U, 232Th, and 226Ra in Bottom Sediments of the Shelf and Continental Slope of Svalbard M. Domanov 10.1134/S1066362224010144
- Particle sources and downward fluxes in the eastern Fram strait under the influence of the west Spitsbergen current A. Sanchez-Vidal et al. 10.1016/j.dsr.2015.06.002
- Distribution features of <sup>238</sup>U, <sup>232</sup>Th and <sup>226</sup>Ra in bottom sediments of the shelf and continental slope of Svalbard M. Domanov 10.31857/S0033831124010148
- The Pleistocene contribution to the net erosion and sedimentary conditions in the outer Bear Island Trough, western Barents Sea K. Zieba et al. 10.1007/s41063-016-0022-3
- Postglacial paleoceanography of the western Barents Sea: Implications for alkenone-based sea surface temperatures and primary productivity M. Łącka et al. 10.1016/j.quascirev.2019.105973
- Transformation of organic matter in a Barents Sea sediment profile: coupled geochemical and microbiological processes M. Stevenson et al. 10.1098/rsta.2020.0223
- New evidence for preservation of contemporary marine organic carbon by iron in Arctic shelf sediments J. Faust et al. 10.1088/1748-9326/aca780
- Middle to late Holocene paleoproductivity reconstructions for the western Barents Sea: a model-data comparison I. Pathirana et al. 10.1007/s41063-015-0002-z
- Microbial Communities Involved in Methane, Sulfur, and Nitrogen Cycling in the Sediments of the Barents Sea S. Begmatov et al. 10.3390/microorganisms9112362
- Does Arctic warming reduce preservation of organic matter in Barents Sea sediments? J. Faust et al. 10.1098/rsta.2019.0364
- Structural and stratigraphic controls on subsurface fluid flow at the Veslemøy High, SW Barents Sea S. Chand et al. 10.1016/j.marpetgeo.2014.06.004
2 citations as recorded by crossref.
- Benthic macrofaunal bioturbation activities from shelf to deep basin in spring to summer transition in the Arctic Ocean B. Oleszczuk et al. 10.1016/j.marenvres.2019.06.008
- Brine formation in relation to climate changes and ice retreat during the last 15,000 years in Storfjorden, Svalbard, 76–78°N T. Rasmussen & E. Thomsen 10.1002/2014PA002643
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