Dune Lake, Alaska 12,000 Year Multiproxy Sediment Data
This dataset contains opal, organic carbon and nitrogen contents, and organic δ13C (carbon-13) and δN15 (nitrogen-15) stable isotopes that were analyzed on a sedimentary sequence spanning the past ~12,000 years from Dune Lake, a shallow groundwater-fed lake in the boreal forest region of central interior Alaska. The unusual hydrology of this system relative to most other lakes studied for paleoclimate in this region provides a novel insight into different seasonal aspects of Alaskan paleoclimatology. The record is consistent with a general long-term decrease in wintertime precipitation, possibly accompanied by an increase in permafrost extent, over the Holocene.
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|Begin datetime||1000-01-01 00:00:00|
|End datetime||2014-06-11 00:00:00|
Map data from IBCSO, IBCAO, and Global Topography.
Maximum (North) Latitude:
Minimum (South) Latitude:
Minimum (West) Longitude: -149.9043, Maximum (East) Longitude: -149.9043
Additional contact information
- author: Bruce P. Finney <firstname.lastname@example.org>
- author: Nancy H. Bigelow <email@example.com>
- author: Valerie A. Barber <firstname.lastname@example.org>
- author: Mary E. Edwards <M.E.Edwards@soton.ac.uk>
- principalInvestigator: Bruce P. Finney <email@example.com>
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