Holocene climate and environmental history of Brurskardstjørni, a lake in the catchment of Øvre Heimdalsvatn, south-central Norway

2010 ◽  
pp. 13-34
Author(s):  
Gaute Velle ◽  
Anne E. Bjune ◽  
Jorunn Larsen ◽  
H. John B. Birks
Keyword(s):  
Environmental History ◽  
Holocene Climate ◽  
South Central ◽  
History Of

Holocene climate and environmental history of Brurskardstjørni, a lake in the catchment of Øvre Heimdalsvatn, south-central Norway

Hydrobiologia ◽  
2010 ◽  
Vol 642 (1) ◽  
pp. 13-34 ◽  
Author(s):  
Gaute Velle ◽  
Anne E. Bjune ◽  
Jorunn Larsen ◽  
H. John B. Birks
Keyword(s):  
Environmental History ◽  
Holocene Climate ◽  
South Central ◽  
History Of

Lateglacial and early Flandrian environmental history of the Isle of Mull, Inner Hebrides, Scotland

1986 ◽  
Vol 77 (1) ◽  
pp. 1-20 ◽  
Author(s):  
J. J. Lowe ◽  
M. J. C. Walker
Keyword(s):  
Environmental History ◽  
Polar Front ◽  
Climatic Conditions ◽  
Plant Succession ◽  
Ice Cap ◽  
South Central ◽  
Tundra Vegetation ◽  
Loch Lomond ◽  
Thermal Maximum ◽  
History Of

ABSTRACTPollen-stratigraphic data, supported by lithological, geochemical and radiocarbon evidence are described from two Late Devensian Lateglacial sites on the Isle of Mull, Inner Hebrides, Scotland. The data suggest that, following the wastage of the Late Devensian ice sheet some time prior to 13,000 BP, an open grass- and sedge-dominated landscape was colonised first by juniper scrub and subsequently by Empetrum heaths. Tree birch development was limited principally, it would seem, by exposure to strong westerly winds, although some scattered birch woodland did become established in more sheltered localities. The thermal maximum of the Lateglacial Interstadial appears to have occurred from c. 13,000 to 12,000 BP after which climate began to deteriorate as the atmospheric Polar Front migrated southwards. The harsh climatic conditions of the Loch Lomond Stadial, the full effects of which were experienced after c. 10,700 BP, led to the break-up of the Interstadial vegetation cover, the development of an ice cap and several smaller cirque and valley glaciers in the hills of south-central Mull, and the establishment of a periglacial regime throughout the island. By c. 10,200 BP, however, climatic amelioration was underway once more, the Loch Lomond Advance glaciers had wasted completely, and a plant succession was initiated which led to the replacement of tundra vegetation communities by Empetrum heath, juniper scrub and eventually hazel-birch woodland within the space of c. 1500 years.

Middle and Late Pleistocene environmental history of the Marsworth area, south-central England

2015 ◽  
Vol 126 (1) ◽  
pp. 18-49 ◽  
Author(s):  
Julian B. Murton ◽  
David Q. Bowen ◽  
Ian Candy ◽  
John A. Catt ◽  
Andrew Currant ◽  
...  
Keyword(s):  
Environmental History ◽  
Late Pleistocene ◽  
South Central ◽  
History Of ◽  
Middle And Late Pleistocene

Holocene climate and environmental history of East Greenland inferred from lake sediments

2017 ◽  
Vol 57 (4) ◽  
pp. 321-341 ◽  
Author(s):  
Amanda R. Lusas ◽  
Brenda L. Hall ◽  
Thomas V. Lowell ◽  
Meredith A. Kelly ◽  
Ole Bennike ◽  
...  
Keyword(s):  
Lake Sediments ◽  
Environmental History ◽  
Holocene Climate ◽  
East Greenland ◽  
History Of
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