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Pollen-based quantitative land-cover reconstruction for northern Asia covering the last 40 ka cal BP

Cao, Xianyong (författare)
Helmholtz Ctr Polar & Marine Res, Germany;Chinese Acad Sci, China
Tian, Fang (författare)
Helmholtz Ctr Polar & Marine Res, Germany
Li, Furong (författare)
Linnéuniversitetet,Institutionen för biologi och miljö (BOM)
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Gaillard, Marie-José, 1953- (författare)
Linnéuniversitetet,Institutionen för biologi och miljö (BOM)
Rudaya, Natalia (författare)
Helmholtz Ctr Polar & Marine Res, Germany;Russian Acad Sci, Russia;Univ Potsdam, Germany
Xu, Qinghai (författare)
Hebei Normal Univ, China
Herzschuh, Ulrike (författare)
Helmholtz Ctr Polar & Marine Res, Germany;Univ Potsdam, Germany
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 (creator_code:org_t)
2019-08-08
2019
Engelska.
Ingår i: Climate of the Past. - : Copernicus Gesellschaft MBH. - 1814-9324 .- 1814-9332. ; 15:4, s. 1503-1536
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • We collected the available relative pollen productivity estimates (PPEs) for 27 major pollen taxa from Eurasia and applied them to estimate plant abundances during the last 40 ka cal BP (calibrated thousand years before present) using pollen counts from 203 fossil pollen records in northern Asia (north of 40 degrees N). These pollen records were organized into 42 site groups and regional mean plant abundances calculated using the REVEALS (Regional Estimates of Vegetation Abundance from Large Sites) model. Time-series clustering, constrained hierarchical clustering, and detrended canonical correspondence analysis were performed to investigate the regional pattern, time, and strength of vegetation changes, respectively. Reconstructed regional plant functional type (PFT) components for each site group are generally consistent with modern vegetation in that vegetation changes within the regions are characterized by minor changes in the abundance of PFTs rather than by an increase in new PFTs, particularly during the Holocene. We argue that pollen-based REVEALS estimates of plant abundances should be a more reliable reflection of the vegetation as pollen may overestimate the turnover, particularly when a high pollen producer invades areas dominated by low pollen producers. Comparisons with vegetation-independent climate records show that climate change is the primary factor driving land-cover changes at broad spatial and temporal scales. Vegetation changes in certain regions or periods, however, could not be explained by direct climate change, e.g. inland Siberia, where a sharp increase in evergreen conifer tree abundance occurred at ca. 7-8 ka cal BP despite an unchanging climate, potentially reflecting their response to complex climate-permafrost-fire-vegetation interactions and thus a possible long-term lagged climate response.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)
NATURVETENSKAP  -- Biologi -- Ekologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences -- Ecology (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Naturgeografi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Physical Geography (hsv//eng)

Nyckelord

Paleoecology
Paleoekologi

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