Zobrazeno 1 - 10
of 110
pro vyhledávání: '"Bernard P. Boudreau"'
Publikováno v:
Nature Communications, Vol 7, Iss 1, Pp 1-8 (2016)
Anthropogenic CO2is acidifying the Arctic Ocean surface, with current models predicting downward penetration to deep waters. Here, based on an alternative model supported by available saturation data, the authors show simultaneous acidification of bo
Externí odkaz:
https://doaj.org/article/e1b6ba1730fe4ff295795d0f51d8533b
Publikováno v:
Paleoceanography and Paleoclimatology. 37
Publikováno v:
Paleoceanography and Paleoclimatology. 37
Publikováno v:
Geophysical Research Letters. 49
Autor:
Andrea J. Fassbender, David S. Trossman, Bernard P. Boudreau, Alfonso Mucci, Carolina O. Dufour, Olivier Sulpis, John P. Dunne, Brian K. Arbic
Publikováno v:
Global Biogeochemical Cycles. 33:1654-1673
Publikováno v:
Paleoceanography and Paleoclimatology. 36
Publikováno v:
Geoscientific Model Development, Vol 12, Pp 4469-4496 (2019)
Seawater–sediment interaction is a crucial factor in carbon and nutrient cycling on a wide range of spatial and temporal scales. This interaction is mediated not just through geochemistry but also via biology. Infauna vigorously mix sediment partic
Publikováno v:
Earth and Planetary Science Letters. 492:112-120
Substantial and correlated changes in marine carbonate (CaCO3) content of oceanic sediments commonly accompany the transitions from cold glacial periods to warm interglacial periods. The South China Sea (SCS) is said to be ocean-dominated at depth, a
Autor:
Bernard P. Boudreau, Yiming Luo
Publikováno v:
Earth and Planetary Science Letters. 474:1-12
Deep-sea sediments record changes in oceanic carbonate chemistry and CaCO 3 sedimentation rate through temporal variations in the total burial of CaCO 3 and the position of the carbonate snowline, i.e., the ocean depth at which CaCO 3 -free sediments
Publikováno v:
Nature Communications, Vol 7, Iss 1, Pp 1-8 (2016)
Nature Communications
Nature Communications
The Arctic Ocean is acidifying from absorption of man-made CO2. Current predictive models of that acidification focus on surface waters, and their results argue that deep waters will acidify by downward penetration from the surface. Here we show, wit