76 research outputs found
Dissolved nitrogen in West Greenland waters
The nitrogen tension in several water masses in the West Greenland coastal region departs only about 5% from the value of the atmosphere. Significantly higher values of nitrogen tension were found in the upper layers of waters near glacier fronts. These values are attributed to the solution of gases trapped in the glacier ice and released to the water under considerable hydrostatic pressure
Sea ice dynamics across the Mid-Pleistocene transition in the Bering Sea.
Sea ice and associated feedback mechanisms play an important role for both long- and short-term climate change. Our ability to predict future sea ice extent, however, hinges on a greater understanding of past sea ice dynamics. Here we investigate sea ice changes in the eastern Bering Sea prior to, across, and after the Mid-Pleistocene transition (MPT). The sea ice record, based on the Arctic sea ice biomarker IP25 and related open water proxies from the International Ocean Discovery Program Site U1343, shows a substantial increase in sea ice extent across the MPT. The occurrence of late-glacial/deglacial sea ice maxima are consistent with sea ice/land ice hysteresis and land-glacier retreat via the temperature-precipitation feedback. We also identify interactions of sea ice with phytoplankton growth and ocean circulation patterns, which have important implications for glacial North Pacific Intermediate Water formation and potentially North Pacific abyssal carbon storage
Planktic foraminifera in Holocene sediments from the Laptev Sea and the central Arctic Ocean : species distribution and paleobiogeographical implication
Sources of dissolved inorganic carbon to the Canada Basin halocline: A multitracer study
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