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Steffen Holzkämper

Datos Biográficos

ID6571441
NOMBRESteffen Holzkämper
NOMBRESSteffen
APELLIDOHolzkämper
FIRMAHOLZKÄMPER S
AFILIACIONESStockholm University
ORCID0000-0001-8487-2532
VERIFICADOSí
TOTAL DE OBRAS4
TOTAL DE CITAS5
TOTAL COMO AUTOR4
TOTAL COMO EDITOR0
PRIMER AÑO DE PUBLICACIÓN2012
AÑO MÁS RECIENTE DE PUBLICACIÓN2019
ÍNDICE H2
  • Last Interglacial Climate in Northern Sweden—Insights from a Speleothem Record

    Open Access•Martin Finné, J Sakari Salonen et al.•ARTICLE•Quaternary•2019

    Continental records with absolute dates of the timing and progression of climatic conditions during the Last Interglacial (LIG) from northern Europe are rare. Speleothems from northern Europe have a large potential as archives for LIG environmental conditions since they were formed in sheltered environments and may be preserved beneath ice sheets. Here, we present δ13C and δ18O values from speleothem Kf-21, from Korallgrottan in Jämtland (northwe…

  • A 2000-year record of lake ontogeny and climate variability from the north-eastern European Russian Arctic

    Open Access•Tomi P Luoto, Peter Kuhry et al.•ARTICLE•The Holocene•2016•Citada por: 3•Referencias: 11

    A lake sediment record from the north-eastern European Russian Arctic was examined using palaeolimnological methods, including subfossil chironomid and diatom analysis. The objective of this study is to disentangle environmental history of the lake and climate variability during the past 2000 years. The sediment profile was divided into two main sections following changes in the lithology, separating the limno-telmatic phase between ~2000 and 120…

  • Stable isotopes in Sphagnum fuscum peat as late-Holocene climate proxies in northeastern European Russia

    Open Access•Päivi Kaislahti Tillman, Steffen Holzkämper et al.•ARTICLE•The Holocene•2013•Citada por: 2•Referencias: 11

    The environment of the northern taiga to tundra transition is highly sensitive to climate fluctuations. In this study from northeastern European Russia, stable carbon and oxygen isotope ratios (δ 13 C, δ 18 O) in α-cellulose of Sphagnum fuscum stems subsampled from hummocks and peat plateau profiles have been used as climate proxies. The entire isotope time series, dated by lead ( 210 Pb), caesium ( 137 Cs) and AMS-radiocarbon ( 14 C) dating, spa…

  • Comparison of stable carbon and oxygen isotopes in Picea glauca tree rings and Sphagnum fuscum moss remains from subarctic Canada

    Open Access•Steffen Holzkämper, Päivi Kaislahti Tillman et al.•ARTICLE•Quaternary Research•2012

    Stable isotope ratios from tree rings and peatland mosses have become important proxies of past climate variations. We here compare recent stable carbon and oxygen isotope ratios in cellulose of tree rings from white spruce ( Picea glauca ), growing near the arctic tree line; and cellulose of Sphagnum fuscum stems, growing in a hummock of a subarctic peatland, in west-central Canada. Results show that carbon isotopes in S. fuscum correlate signif…

  • A 2000-year record of lake ontogeny and climate variability from the north-eastern European Russian Arctic

    Open Access•Tomi P Luoto, Peter Kuhry et al.•ARTICLE•The Holocene•2016•Citada por: 3•Referencias: 11

    A lake sediment record from the north-eastern European Russian Arctic was examined using palaeolimnological methods, including subfossil chironomid and diatom analysis. The objective of this study is to disentangle environmental history of the lake and climate variability during the past 2000 years. The sediment profile was divided into two main sections following changes in the lithology, separating the limno-telmatic phase between ~2000 and 120…

  • Stable isotopes in Sphagnum fuscum peat as late-Holocene climate proxies in northeastern European Russia

    Open Access•Päivi Kaislahti Tillman, Steffen Holzkämper et al.•ARTICLE•The Holocene•2013•Citada por: 2•Referencias: 11

    The environment of the northern taiga to tundra transition is highly sensitive to climate fluctuations. In this study from northeastern European Russia, stable carbon and oxygen isotope ratios (δ 13 C, δ 18 O) in α-cellulose of Sphagnum fuscum stems subsampled from hummocks and peat plateau profiles have been used as climate proxies. The entire isotope time series, dated by lead ( 210 Pb), caesium ( 137 Cs) and AMS-radiocarbon ( 14 C) dating, spa…

  • Comparison of stable carbon and oxygen isotopes in Picea glauca tree rings and Sphagnum fuscum moss remains from subarctic Canada

    Open Access•Steffen Holzkämper, Päivi Kaislahti Tillman et al.•ARTICLE•Quaternary Research•2012

    Stable isotope ratios from tree rings and peatland mosses have become important proxies of past climate variations. We here compare recent stable carbon and oxygen isotope ratios in cellulose of tree rings from white spruce ( Picea glauca ), growing near the arctic tree line; and cellulose of Sphagnum fuscum stems, growing in a hummock of a subarctic peatland, in west-central Canada. Results show that carbon isotopes in S. fuscum correlate signif…

  • Stable isotopes in Sphagnum fuscum peat as late-Holocene climate proxies in northeastern European Russia

    Open Access•Päivi Kaislahti Tillman, Steffen Holzkämper et al.•ARTICLE•The Holocene•2013•Citada por: 2•Referencias: 11

    The environment of the northern taiga to tundra transition is highly sensitive to climate fluctuations. In this study from northeastern European Russia, stable carbon and oxygen isotope ratios (δ 13 C, δ 18 O) in α-cellulose of Sphagnum fuscum stems subsampled from hummocks and peat plateau profiles have been used as climate proxies. The entire isotope time series, dated by lead ( 210 Pb), caesium ( 137 Cs) and AMS-radiocarbon ( 14 C) dating, spa…

  • A 2000-year record of lake ontogeny and climate variability from the north-eastern European Russian Arctic

    Open Access•Tomi P Luoto, Peter Kuhry et al.•ARTICLE•The Holocene•2016•Citada por: 3•Referencias: 11

    A lake sediment record from the north-eastern European Russian Arctic was examined using palaeolimnological methods, including subfossil chironomid and diatom analysis. The objective of this study is to disentangle environmental history of the lake and climate variability during the past 2000 years. The sediment profile was divided into two main sections following changes in the lithology, separating the limno-telmatic phase between ~2000 and 120…

  • Last Interglacial Climate in Northern Sweden—Insights from a Speleothem Record

    Open Access•Martin Finné, J Sakari Salonen et al.•ARTICLE•Quaternary•2019

    Continental records with absolute dates of the timing and progression of climatic conditions during the Last Interglacial (LIG) from northern Europe are rare. Speleothems from northern Europe have a large potential as archives for LIG environmental conditions since they were formed in sheltered environments and may be preserved beneath ice sheets. Here, we present δ13C and δ18O values from speleothem Kf-21, from Korallgrottan in Jämtland (northwe…

Geology and Paleoclimatology Research (4 obras) · Climate change (3 obras) · Geography (3 obras) · Geology (3 obras) · Holocene (3 obras) · Oceanography (3 obras) · Paleontology (3 obras) · Physical geography (3 obras) · Stable isotope ratio (3 obras) · Archaeology (2 obras)

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