Past Antarctica - Paleoclimatology and Climate Change CHAPTER 11 Geoecological responses

Organisms living in polar regions are subject to some of the most extreme environmental conditions on Earth. Antarctic vegetation is mainly composed of non-vascular cryptogams, with bryophytes and mosses, in particular, being the dominant terrestrial flora with lichens and algae (e.g., Øvstedal and...

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Main Author: N. Cannone
Other Authors: M. Oliva, J. Ruiz-Fernandez, Cannone, N.
Format: Book Part
Language:English
Published: Elsevier 2020
Subjects:
Online Access:http://hdl.handle.net/11383/2101266
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spelling ftuninsubriairis:oai:irinsubria.uninsubria.it:11383/2101266 2024-01-28T09:59:36+01:00 Past Antarctica - Paleoclimatology and Climate Change CHAPTER 11 Geoecological responses N. Cannone N. Cannone M. Oliva, J. Ruiz-Fernandez Cannone, N. 2020 STAMPA http://hdl.handle.net/11383/2101266 eng eng Elsevier country:GBR place:London info:eu-repo/semantics/altIdentifier/isbn/978-0-12-817925-3 ispartofbook:Past Antarctica Paleoclimatology and Climate Change volume:1 firstpage:201 lastpage:216 numberofpages:16 alleditors:M. Oliva, J. Ruiz-Fernandez http://hdl.handle.net/11383/2101266 Biodiversity biogeography geoecological responses climate change Antarctica info:eu-repo/semantics/bookPart 2020 ftuninsubriairis 2024-01-03T17:53:21Z Organisms living in polar regions are subject to some of the most extreme environmental conditions on Earth. Antarctic vegetation is mainly composed of non-vascular cryptogams, with bryophytes and mosses, in particular, being the dominant terrestrial flora with lichens and algae (e.g., Øvstedal and Smith, 2001; Ochyra et al., 2008). Survival in Antarctic terrestrial ecosystems is based on the capability to withstand cold temperatures, low and irregular water availability, scarce nutrients, unstable substrata, prolonged snow cover, low radiation receipt, wide seasonal variations in photoperiod and strong winds (e.g., Kennedy, 1993, 1995). In Antarctica growth conditions are extreme and plants exist at the physiological limits of survival, with abiotic factors considered to be responsible for the restrictions imposed upon the distributions of plant populations (Longton, 1988; Davey, 1997). In this harsh context, even slight changes to growth conditions are likely to have a large impact, rendering Antarctic terrestrial communities sensitive to climate change (Robinson et al., 2003). As a consequence of these severe conditions, Antarctic flora is almost entirely cryptogamic. Only two vascular species, Deschampsia antarctica Desv. and Colobanthus quitensis (Kunth) Bartl., occur, both of which are restricted to the Antarctic Peninsula. Biodiversity patterns of the extant Antarctic biota are the result of a complex and long biogeographical and climatic history. Knowledge of these patterns, with special reference to past, present and future geoecological responses of these ecosystems, allows for facing and preventing, when possible, threats to the continent’s biodiversity deriving from climate change, biological invasions and anthropogenic impacts. Book Part Antarc* Antarctic Antarctic Peninsula Antarctica IRInSubria - Institutional Repository Insubria (Università degli Studi dell’Insubria) Antarctic Antarctic Peninsula Davey ENVELOPE(-58.567,-58.567,-61.967,-61.967) The Antarctic
institution Open Polar
collection IRInSubria - Institutional Repository Insubria (Università degli Studi dell’Insubria)
op_collection_id ftuninsubriairis
language English
topic Biodiversity
biogeography
geoecological responses
climate change
Antarctica
spellingShingle Biodiversity
biogeography
geoecological responses
climate change
Antarctica
N. Cannone
Past Antarctica - Paleoclimatology and Climate Change CHAPTER 11 Geoecological responses
topic_facet Biodiversity
biogeography
geoecological responses
climate change
Antarctica
description Organisms living in polar regions are subject to some of the most extreme environmental conditions on Earth. Antarctic vegetation is mainly composed of non-vascular cryptogams, with bryophytes and mosses, in particular, being the dominant terrestrial flora with lichens and algae (e.g., Øvstedal and Smith, 2001; Ochyra et al., 2008). Survival in Antarctic terrestrial ecosystems is based on the capability to withstand cold temperatures, low and irregular water availability, scarce nutrients, unstable substrata, prolonged snow cover, low radiation receipt, wide seasonal variations in photoperiod and strong winds (e.g., Kennedy, 1993, 1995). In Antarctica growth conditions are extreme and plants exist at the physiological limits of survival, with abiotic factors considered to be responsible for the restrictions imposed upon the distributions of plant populations (Longton, 1988; Davey, 1997). In this harsh context, even slight changes to growth conditions are likely to have a large impact, rendering Antarctic terrestrial communities sensitive to climate change (Robinson et al., 2003). As a consequence of these severe conditions, Antarctic flora is almost entirely cryptogamic. Only two vascular species, Deschampsia antarctica Desv. and Colobanthus quitensis (Kunth) Bartl., occur, both of which are restricted to the Antarctic Peninsula. Biodiversity patterns of the extant Antarctic biota are the result of a complex and long biogeographical and climatic history. Knowledge of these patterns, with special reference to past, present and future geoecological responses of these ecosystems, allows for facing and preventing, when possible, threats to the continent’s biodiversity deriving from climate change, biological invasions and anthropogenic impacts.
author2 N. Cannone
M. Oliva, J. Ruiz-Fernandez
Cannone, N.
format Book Part
author N. Cannone
author_facet N. Cannone
author_sort N. Cannone
title Past Antarctica - Paleoclimatology and Climate Change CHAPTER 11 Geoecological responses
title_short Past Antarctica - Paleoclimatology and Climate Change CHAPTER 11 Geoecological responses
title_full Past Antarctica - Paleoclimatology and Climate Change CHAPTER 11 Geoecological responses
title_fullStr Past Antarctica - Paleoclimatology and Climate Change CHAPTER 11 Geoecological responses
title_full_unstemmed Past Antarctica - Paleoclimatology and Climate Change CHAPTER 11 Geoecological responses
title_sort past antarctica - paleoclimatology and climate change chapter 11 geoecological responses
publisher Elsevier
publishDate 2020
url http://hdl.handle.net/11383/2101266
long_lat ENVELOPE(-58.567,-58.567,-61.967,-61.967)
geographic Antarctic
Antarctic Peninsula
Davey
The Antarctic
geographic_facet Antarctic
Antarctic Peninsula
Davey
The Antarctic
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
op_relation info:eu-repo/semantics/altIdentifier/isbn/978-0-12-817925-3
ispartofbook:Past Antarctica Paleoclimatology and Climate Change
volume:1
firstpage:201
lastpage:216
numberofpages:16
alleditors:M. Oliva, J. Ruiz-Fernandez
http://hdl.handle.net/11383/2101266
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