Soils and vegetation in abandoned penguin rookeries (maritime Antarctic
Abstract: Occurrence of abandoned ornithogenic soils resulted from the changing of nesting places due to recent geological events in this region. During the Holocene period King George Island has been lifted up to more than 50 m high as an effect of isostatic movement. At the same time penguin rooke...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.627.3201 2023-05-15T14:06:21+02:00 Soils and vegetation in abandoned penguin rookeries (maritime Antarctic Andrzej Tatur Andrzej Myrcha The Pennsylvania State University CiteSeerX Archives 1989 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.627.3201 http://polaris.nipr.ac.jp/~penguin/polarbiosci/issues/pdf/1989-Tatur.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.627.3201 http://polaris.nipr.ac.jp/~penguin/polarbiosci/issues/pdf/1989-Tatur.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://polaris.nipr.ac.jp/~penguin/polarbiosci/issues/pdf/1989-Tatur.pdf text 1989 ftciteseerx 2016-01-08T15:16:57Z Abstract: Occurrence of abandoned ornithogenic soils resulted from the changing of nesting places due to recent geological events in this region. During the Holocene period King George Island has been lifted up to more than 50 m high as an effect of isostatic movement. At the same time penguin rookeries have been shifted down onto the newly emerged rocks and new beaches, whereas the higher nesting areas have been abandoned. In several points dramatic changes in local environmental condition forced the penguins to abandon their nesting places totally. The areas deserted by penguins have been colonized by the vegetation. Ornithogenic soils have been hidden from view under a dense carpet of lichens, mosses and grasses. Rich in nutrients, phosphatic clays forming these soils proved to be relatively long-lasting in the climatic conditions of maritime Antarctic, because after many hundreds and thousands of years they have retained specific chemical and mineral properties. Thus the ancient ornithogenic soils of abandoned rookeries have been a valuable source of easily available nutrients for the formation of ter-restrial ecosystems during the Holocene period. Our survey has found this problem to be common and important in this region. 1. Text Antarc* Antarctic King George Island Unknown Antarctic King George Island |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
Abstract: Occurrence of abandoned ornithogenic soils resulted from the changing of nesting places due to recent geological events in this region. During the Holocene period King George Island has been lifted up to more than 50 m high as an effect of isostatic movement. At the same time penguin rookeries have been shifted down onto the newly emerged rocks and new beaches, whereas the higher nesting areas have been abandoned. In several points dramatic changes in local environmental condition forced the penguins to abandon their nesting places totally. The areas deserted by penguins have been colonized by the vegetation. Ornithogenic soils have been hidden from view under a dense carpet of lichens, mosses and grasses. Rich in nutrients, phosphatic clays forming these soils proved to be relatively long-lasting in the climatic conditions of maritime Antarctic, because after many hundreds and thousands of years they have retained specific chemical and mineral properties. Thus the ancient ornithogenic soils of abandoned rookeries have been a valuable source of easily available nutrients for the formation of ter-restrial ecosystems during the Holocene period. Our survey has found this problem to be common and important in this region. 1. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Andrzej Tatur Andrzej Myrcha |
spellingShingle |
Andrzej Tatur Andrzej Myrcha Soils and vegetation in abandoned penguin rookeries (maritime Antarctic |
author_facet |
Andrzej Tatur Andrzej Myrcha |
author_sort |
Andrzej Tatur |
title |
Soils and vegetation in abandoned penguin rookeries (maritime Antarctic |
title_short |
Soils and vegetation in abandoned penguin rookeries (maritime Antarctic |
title_full |
Soils and vegetation in abandoned penguin rookeries (maritime Antarctic |
title_fullStr |
Soils and vegetation in abandoned penguin rookeries (maritime Antarctic |
title_full_unstemmed |
Soils and vegetation in abandoned penguin rookeries (maritime Antarctic |
title_sort |
soils and vegetation in abandoned penguin rookeries (maritime antarctic |
publishDate |
1989 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.627.3201 http://polaris.nipr.ac.jp/~penguin/polarbiosci/issues/pdf/1989-Tatur.pdf |
geographic |
Antarctic King George Island |
geographic_facet |
Antarctic King George Island |
genre |
Antarc* Antarctic King George Island |
genre_facet |
Antarc* Antarctic King George Island |
op_source |
http://polaris.nipr.ac.jp/~penguin/polarbiosci/issues/pdf/1989-Tatur.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.627.3201 http://polaris.nipr.ac.jp/~penguin/polarbiosci/issues/pdf/1989-Tatur.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766278056538800128 |