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Rolf Zale

Biographic Data

ID6375680
NAMERolf Zale
GIVEN NAMESRolf
FAMILY NAMEZale
SIGNATUREZALE R
AFFILIATIONSUmeå University
VERIFIEDNo
TOTAL WORKS3
TOTAL CITATIONS1
AUTHOR COUNT3
EDITOR COUNT0
FIRST PUBLICATION YEAR1991
LATEST PUBLICATION YEAR2023
H-INDEX1
  • Landscape of ice and fire – uniquely well-preserved Scots pine trunks reveal forest fires near the retreating Weichselian ice margin

    Open Access•Jonatan Klaminder, Magdalena Fassl et al.•ARTICLE•Vegetation History and…•2023•References: 8

    Environmental conditions for trees that established in central Fennoscandia shortly after the final retreat of the Weichselian ice sheet remain poorly understood. In this study we examine tree rings of five well-preserved Pinus sylvestris (Scots pines) that grew in the area in front of the retreating ice sheet in northern Sweden. They became buried in flood sediments deposited by a glacial outburst flood (jökulhlaup) about 9.5–9.9 kyr cal bp and …

  • Holocene development of the fauna of Lake Boeckella, northern Antarctic Peninsula

    Open Access•John A E Gibson, Rolf Zale•ARTICLE•The Holocene•2006•Cited by: 1

    The origins of the freshwater fauna that inhabits Antarctic lakes are poorly known. The species present today could be relict species that have survived Quaternary glaciations on the continent, or Holocene migrants from more temperate regions. One approach to investigating these questions is to study faunal microfossils in lake sediment. This approach was applied to a 293 cm sediment core from Lake Boeckella, located at the northern tip of the An…

  • Late Holocene tephrochronology of the northern Antarctic Peninsula

    Open Access•Svante Björck, Per Sandgren et al.•ARTICLE•Quaternary Research•1991

    Andesitic and basaltic andesitic tephra layers are abundant in Holocene deposits from the Antarctic Peninsula. Visually discernible tephra horizons occur in three lakes on Livingston Island. Tephra in two other lakes and in a moss bank on Elephant Island, with very low ash concentrations, were detected magnetically. Deception Island is the most likely volcanic source for the tephra. With direct 14 C dating, age/depth curves, and cross-correlation…

  • Holocene development of the fauna of Lake Boeckella, northern Antarctic Peninsula

    Open Access•John A E Gibson, Rolf Zale•ARTICLE•The Holocene•2006•Cited by: 1

    The origins of the freshwater fauna that inhabits Antarctic lakes are poorly known. The species present today could be relict species that have survived Quaternary glaciations on the continent, or Holocene migrants from more temperate regions. One approach to investigating these questions is to study faunal microfossils in lake sediment. This approach was applied to a 293 cm sediment core from Lake Boeckella, located at the northern tip of the An…

  • Late Holocene tephrochronology of the northern Antarctic Peninsula

    Open Access•Svante Björck, Per Sandgren et al.•ARTICLE•Quaternary Research•1991

    Andesitic and basaltic andesitic tephra layers are abundant in Holocene deposits from the Antarctic Peninsula. Visually discernible tephra horizons occur in three lakes on Livingston Island. Tephra in two other lakes and in a moss bank on Elephant Island, with very low ash concentrations, were detected magnetically. Deception Island is the most likely volcanic source for the tephra. With direct 14 C dating, age/depth curves, and cross-correlation…

  • Holocene development of the fauna of Lake Boeckella, northern Antarctic Peninsula

    Open Access•John A E Gibson, Rolf Zale•ARTICLE•The Holocene•2006•Cited by: 1

    The origins of the freshwater fauna that inhabits Antarctic lakes are poorly known. The species present today could be relict species that have survived Quaternary glaciations on the continent, or Holocene migrants from more temperate regions. One approach to investigating these questions is to study faunal microfossils in lake sediment. This approach was applied to a 293 cm sediment core from Lake Boeckella, located at the northern tip of the An…

  • Landscape of ice and fire – uniquely well-preserved Scots pine trunks reveal forest fires near the retreating Weichselian ice margin

    Open Access•Jonatan Klaminder, Magdalena Fassl et al.•ARTICLE•Vegetation History and…•2023•References: 8

    Environmental conditions for trees that established in central Fennoscandia shortly after the final retreat of the Weichselian ice sheet remain poorly understood. In this study we examine tree rings of five well-preserved Pinus sylvestris (Scots pines) that grew in the area in front of the retreating ice sheet in northern Sweden. They became buried in flood sediments deposited by a glacial outburst flood (jökulhlaup) about 9.5–9.9 kyr cal bp and …

Holocene (3 works) · Archaeology (2 works) · Geography (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Oceanography (2 works) · Paleontology (2 works) · Peninsula (2 works) · Physical geography (2 works) · Polar Research and Ecology (2 works)

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