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Adam Hölzer

Biographic Data

ID5599277
NAMEAdam Hölzer
GIVEN NAMESAdam
FAMILY NAMEHölzer
SIGNATUREHOLZER A
AFFILIATIONSState Museum of Natural History Karlsruhe
VERIFIEDNo
TOTAL WORKS3
TOTAL CITATIONS11
AUTHOR COUNT3
EDITOR COUNT0
FIRST PUBLICATION YEAR1998
LATEST PUBLICATION YEAR2007
H-INDEX2
  • Late Holocene Natural and Human-Induced Environmental Change Reconstructed from Peat Records in Eastern Central China

    Open Access•Yan Zhao, Adam Hölzer et al.•ARTICLE•Radiocarbon•2007•Cited by: 3•References: 15

    We present a high-resolution multiproxy record (geochemistry, macrofossil, and pollen) from a peatland in the Dajiuhu Basin in eastern central China. The chronology of the 120-cm peat profile was controlled by 6 accelerator mass spectrometry (AMS) 14 C dates on plant remains, including 2 post-bomb dates. The age model was based on linear interpolations of calibrated ages. Plant macrofossil results indicate a major transition around 3600 cal BP fr…

  • Botanical macro-remains and insects from the Eemian and Weichselian site of Oerel (northwest Germany) and their evidence for the history of climate

    Open Access•Karl‐Ernst Behre, Karl-Ernst Behre et al.•ARTICLE•Vegetation History and…•2005•Cited by: 1•References: 2

  • Silicon and titanium in peat profiles as indicators of human impact

    Open Access•Adam Hölzer, Amal Hölzer•ARTICLE•The Holocene•1998•Cited by: 7•References: 4

    A close correlation exists at four peat sites between pollen indicators of human impact, especially Plantago lanceolata and Cerealia, and the elements silicon and especially titanium as indicators of erosion. Pollen of plants with a short life cycle occur at the peak of silicon or titanium or shortly after, and a tree-pollen response follows later. Short disturbances of the vegetation or very early human impact can be detected and delimited even …

  • Silicon and titanium in peat profiles as indicators of human impact

    Open Access•Adam Hölzer, Amal Hölzer•ARTICLE•The Holocene•1998•Cited by: 7•References: 4

    A close correlation exists at four peat sites between pollen indicators of human impact, especially Plantago lanceolata and Cerealia, and the elements silicon and especially titanium as indicators of erosion. Pollen of plants with a short life cycle occur at the peak of silicon or titanium or shortly after, and a tree-pollen response follows later. Short disturbances of the vegetation or very early human impact can be detected and delimited even …

  • Late Holocene Natural and Human-Induced Environmental Change Reconstructed from Peat Records in Eastern Central China

    Open Access•Yan Zhao, Adam Hölzer et al.•ARTICLE•Radiocarbon•2007•Cited by: 3•References: 15

    We present a high-resolution multiproxy record (geochemistry, macrofossil, and pollen) from a peatland in the Dajiuhu Basin in eastern central China. The chronology of the 120-cm peat profile was controlled by 6 accelerator mass spectrometry (AMS) 14 C dates on plant remains, including 2 post-bomb dates. The age model was based on linear interpolations of calibrated ages. Plant macrofossil results indicate a major transition around 3600 cal BP fr…

  • Botanical macro-remains and insects from the Eemian and Weichselian site of Oerel (northwest Germany) and their evidence for the history of climate

    Open Access•Karl‐Ernst Behre, Karl-Ernst Behre et al.•ARTICLE•Vegetation History and…•2005•Cited by: 1•References: 2

  • Silicon and titanium in peat profiles as indicators of human impact

    Open Access•Adam Hölzer, Amal Hölzer•ARTICLE•The Holocene•1998•Cited by: 7•References: 4

    A close correlation exists at four peat sites between pollen indicators of human impact, especially Plantago lanceolata and Cerealia, and the elements silicon and especially titanium as indicators of erosion. Pollen of plants with a short life cycle occur at the peak of silicon or titanium or shortly after, and a tree-pollen response follows later. Short disturbances of the vegetation or very early human impact can be detected and delimited even …

  • Botanical macro-remains and insects from the Eemian and Weichselian site of Oerel (northwest Germany) and their evidence for the history of climate

    Open Access•Karl‐Ernst Behre, Karl-Ernst Behre et al.•ARTICLE•Vegetation History and…•2005•Cited by: 1•References: 2

  • Late Holocene Natural and Human-Induced Environmental Change Reconstructed from Peat Records in Eastern Central China

    Open Access•Yan Zhao, Adam Hölzer et al.•ARTICLE•Radiocarbon•2007•Cited by: 3•References: 15

    We present a high-resolution multiproxy record (geochemistry, macrofossil, and pollen) from a peatland in the Dajiuhu Basin in eastern central China. The chronology of the 120-cm peat profile was controlled by 6 accelerator mass spectrometry (AMS) 14 C dates on plant remains, including 2 post-bomb dates. The age model was based on linear interpolations of calibrated ages. Plant macrofossil results indicate a major transition around 3600 cal BP fr…

Ecology (3 works) · Geography (3 works) · Geology (3 works) · Geology and Paleoclimatology Research (3 works) · Macrofossil (3 works) · Paleontology (3 works) · Peat (3 works) · Physical geography (3 works) · Pollen (3 works) · Archaeology and ancient environmental studies (2 works)

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