The pollen stratigraphy of late Quaternary lake sediments of South-West Greenland

Research output: Chapter in Book/Report/Conference proceeding › Report chapter › Research

Standard

The pollen stratigraphy of late Quaternary lake sediments of South-West Greenland. / Kelly, Michael; Funder, Svend Visby.

The Geological Survey of Greenland Report . Vol. 64 1974. p. 1-26 (The Geological Survey of Greenland Report , Vol. 64).

Research output: Chapter in Book/Report/Conference proceeding › Report chapter › Research

Harvard

Kelly, M & Funder, SV 1974, The pollen stratigraphy of late Quaternary lake sediments of South-West Greenland. in The Geological Survey of Greenland Report . vol. 64, The Geological Survey of Greenland Report , vol. 64, pp. 1-26.

APA

Kelly, M., & Funder, S. V. (1974). The pollen stratigraphy of late Quaternary lake sediments of South-West Greenland. In The Geological Survey of Greenland Report (Vol. 64, pp. 1-26). The Geological Survey of Greenland Report Vol. 64

Vancouver

Kelly M, Funder SV. The pollen stratigraphy of late Quaternary lake sediments of South-West Greenland. In The Geological Survey of Greenland Report . Vol. 64. 1974. p. 1-26. (The Geological Survey of Greenland Report , Vol. 64).

Author

Kelly, Michael ; Funder, Svend Visby. / The pollen stratigraphy of late Quaternary lake sediments of South-West Greenland. The Geological Survey of Greenland Report . Vol. 64 1974. pp. 1-26 (The Geological Survey of Greenland Report , Vol. 64).

Bibtex

@inbook{7bc916696ccf441485197e8f5e741086,
title = "The pollen stratigraphy of late Quaternary lake sediments of South-West Greenland",
abstract = "Pollen analysis and radiocarbon dating of lake sediment cores from four localities in the Frederikshab district, South-West Greenland, provide a chronology of vegetation changes in the area since c. 10000 B.P. An initial pioneer phase with the early development of some heath communities is followed by a mid postglacial phase in which there is the successive appearance of woody scrub species. A final phase shows the decline of some of these. This is interpreted as a general response to a broad amplitude fluctuation in climate, with its optimal period lying between c. 7600 and 3200 B.P. The detailed composition of the vegetation however is influenced by immigration phenomena, with the appearance of many species lagging behind the attainment of their climatic thresholds. Detailed consideration is given to the possibility of Alnus crispa being present as a scrub component during the climatic optimum.",
author = "Michael Kelly and Funder, {Svend Visby}",
year = "1974",
language = "Dansk",
volume = "64",
series = "The Geological Survey of Greenland Report ",
pages = "1--26",
booktitle = "The Geological Survey of Greenland Report",

}

RIS

TY - GEN

T1 - The pollen stratigraphy of late Quaternary lake sediments of South-West Greenland

AU - Kelly, Michael

AU - Funder, Svend Visby

PY - 1974

Y1 - 1974

N2 - Pollen analysis and radiocarbon dating of lake sediment cores from four localities in the Frederikshab district, South-West Greenland, provide a chronology of vegetation changes in the area since c. 10000 B.P. An initial pioneer phase with the early development of some heath communities is followed by a mid postglacial phase in which there is the successive appearance of woody scrub species. A final phase shows the decline of some of these. This is interpreted as a general response to a broad amplitude fluctuation in climate, with its optimal period lying between c. 7600 and 3200 B.P. The detailed composition of the vegetation however is influenced by immigration phenomena, with the appearance of many species lagging behind the attainment of their climatic thresholds. Detailed consideration is given to the possibility of Alnus crispa being present as a scrub component during the climatic optimum.

AB - Pollen analysis and radiocarbon dating of lake sediment cores from four localities in the Frederikshab district, South-West Greenland, provide a chronology of vegetation changes in the area since c. 10000 B.P. An initial pioneer phase with the early development of some heath communities is followed by a mid postglacial phase in which there is the successive appearance of woody scrub species. A final phase shows the decline of some of these. This is interpreted as a general response to a broad amplitude fluctuation in climate, with its optimal period lying between c. 7600 and 3200 B.P. The detailed composition of the vegetation however is influenced by immigration phenomena, with the appearance of many species lagging behind the attainment of their climatic thresholds. Detailed consideration is given to the possibility of Alnus crispa being present as a scrub component during the climatic optimum.

M3 - Bidrag til rapport

VL - 64

T3 - The Geological Survey of Greenland Report

SP - 1

EP - 26

BT - The Geological Survey of Greenland Report

ER -

ID: 35115457