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The greening of Western Australian landscapes: the Phanerozoic plant record

Peyrot, Daniel (författare)
The University of Western Australia
Playford, Geoffrey (författare)
The University of Queensland
Mantle, Daniel J. (författare)
MGPalaeo, 1/5 Arvida St Malaga, Western Australia
visa fler...
Backhouse, John (författare)
The University of Western Australia
Milne, Lynne A. (författare)
Curtin University
Carpenter, Raymond J. (författare)
University of Adelaide
Foster, Clinton (författare)
The University of Western Australia; Australian National University
Mory, Arthur, J. (författare)
Geological Survey and Resource Strategy, 100 Plain Street, East Perth WA
McLoughlin, Stephen, 1964- (författare)
Naturhistoriska riksmuseet,Enheten för paleobiologi
Vitacca, Jesse (författare)
The University of Western Australia
Scibiorski, Joe (författare)
The University of Western Australia
Mack, Charlotte L. (författare)
Curtin University
Bevan, Jenny (författare)
The University of Western Australia
visa färre...
 (creator_code:org_t)
Perth : Royal Society of Western Australia, 2019
2019
Engelska.
Ingår i: Journal of the Royal Society of Western Australia. - Perth : Royal Society of Western Australia. - 0035-922X. ; 102, s. 52-82
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Western Australian terrestrial floras first appeared in the Middle Ordovician (c. 460 Ma) and developed Gondwanan affinities in the Permian. During the Mesozoic, these floras transitioned to acquire a distinctly austral character in response to further changes in the continent’s palaeolatitude and its increasing isolation from other parts of Gondwana. This synthesis of landscape evolution is based on palaeobotanical and palynological evidence mostly assembled during the last 60 years. The composition of the plant communities and the structure of vegetation changed markedly through the Phanerozoic. The Middle Ordovician –Middle Devonian was characterised by diminutive vegetation in low-diversity communities. An increase in plant size is inferred from the Devonian record, particularly from that of the Late Devonian when a significant part of the flora was arborescent. Changes in plant growth-forms accompanied a major expansion of vegetation cover to episodically or permanently flooded lowland settings and, from the latest Mississippian onwards, to dry hinterland environments. Wetter conditions during the Permian yielded waterlogged environments with complex swamp communities dominated by Glossopteris. In response to the Permian–Triassic extinction event, a transitional vegetation characterised by herbaceous lycopsids became dominant but was largely replaced by the Middle Triassic with seed ferns and shrubs or trees attributed to Dicroidium. Another floristic turnover at the Triassic–Jurassic boundary introduced precursors of Australia’s modern vegetation and other southern hemisphere regions. Most importantly, flowering plants gained ascendancy during the Late Cretaceous. Characteristics of the state’s modern vegetation, such as sclerophylly and xeromorphy, arose during the Late Cretaceous and Paleogene. The vegetation progressively developed its present-day structure and composition in response to the increasing aridity during the Neogene–Quaternary.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Annan geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Other Earth and Related Environmental Sciences (hsv//eng)

Nyckelord

palaeobotany
palynology
vegetation
palaeoclimate
Western Australia
The changing Earth
Den föränderliga jorden
Ecosystems and species history
Ekosystem och arthistoria
Diversity of life
Livets mångfald

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ref (ämneskategori)
art (ämneskategori)

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