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Arctic Holocene proxy climate database - new approaches to assessing geochronological accuracy and encoding climate variables

Sundqvist, Hanna S. (author)
Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK)
Kaufman, D. S. (author)
McKay, N. P. (author)
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Balascio, N. L. (author)
Briner, J. P. (author)
Cwynar, L. C. (author)
Sejrup, H. P. (author)
Seppa, H. (author)
Subetto, D. A. (author)
Andrews, J. T. (author)
Axford, Y. (author)
Bakke, J. (author)
Birks, H. J. B. (author)
Brooks, S. J. (author)
de Vernal, A. (author)
Jennings, A. E. (author)
Charpentier Ljungqvist, Fredrik (author)
Stockholms universitet,Historiska institutionen
Ruehland, K. M. (author)
Saenger, C. (author)
Smol, J. P. (author)
Viau, A. E. (author)
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 (creator_code:org_t)
2014-08-29
2014
English.
In: Climate of the Past. - : Copernicus GmbH. - 1814-9324 .- 1814-9332. ; 10:4, s. 1605-1631
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • We present a systematic compilation of previously published Holocene proxy climate records from the Arctic. We identified 170 sites from north of 58 degrees N latitude where proxy time series extend back at least to 6 cal ka (all ages in this article are in calendar years before present - BP), are resolved at submillennial scale (at least one value every 400 +/- 200 years) and have age models constrained by at least one age every 3000 years. In addition to conventional meta-data for each proxy record (location, proxy type, reference), we include two novel parameters that add functionality to the database. First, climate interpretation is a series of fields that logically describe the specific climate variable(s) represented by the proxy record. It encodes the proxy-climate relation reported by authors of the original studies into a structured format to facilitate comparison with climate model outputs. Second, geochronology accuracy score (chron score) is a numerical rating that reflects the overall accuracy of C-14-based age models from lake and marine sediments. Chron scores were calculated using the original author-reported C-14 ages, which are included in this database. The database contains 320 records (some sites include multiple records) from six regions covering the circumpolar Arctic: Fennoscandia is the most densely sampled region (31% of the records), whereas only five records from the Russian Arctic met the criteria for inclusion. The database contains proxy records from lake sediment (60 %), marine sediment (32 %), glacier ice (5 %), and other sources. Most (61 %) reflect temperature (mainly summer warmth) and are primarily based on pollen, chironomid, or diatom assemblages. Many (15 %) reflect some aspect of hydroclimate as inferred from changes in stable isotopes, pollen and diatom assemblages, humification index in peat, and changes in equilibrium-line altitude of glaciers. This comprehensive database can be used in future studies to investigate the spatio-temporal pattern of Arctic Holocene climate changes and their causes. The Arctic Holocene data set is available from NOAA Paleoclimatology.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)

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