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Sökning: onr:"swepub:oai:DiVA.org:nrm-3839" > The Coal Farms of t...

The Coal Farms of the Late Paleozoic

Gastaldo, Robert (författare)
Colby College, Maine
Bamford, Marion (författare)
University of the Witwatersrand, South Africa
Calder, John (författare)
Geological Survey Division, Nova Scotia Department of Energy and Mines
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DiMichele, William (författare)
Smithsonian Institution, United States National Museum, Washington, DC,
Iannuzzi, Roberto (författare)
Universidade Federal do Rio Grande do Sul, Porto Alegre
Jasper, André (författare)
Universidade do Vale do Taquari - Univates, Lajeado
Kerp, Hans (författare)
University of Münster
McLoughlin, Stephen, 1964- (författare)
Naturhistoriska riksmuseet,Enheten för paleobiologi
Opluštil, Stanislav (författare)
Charles University in Prague
Pfefferkorn, Hermann (författare)
University of Pennsylvania, Philadelphia
Rößler,, Ronny (författare)
Museum für Naturkunde, Chemnitz
Wang, Jun (författare)
Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing
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 (creator_code:org_t)
1
Cham, Switzerland : Springer Nature, 2020
2020
Engelska.
Ingår i: Nature Through Time. - Cham, Switzerland : Springer Nature. - 9783030350574 ; , s. 317-343
  • Bokkapitel (refereegranskat)
Abstract Ämnesord
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  • The assembly of the supercontinent Pangea resulted in a paleoequatorial region known as Euramerica, a northern mid-to-high latitude region called Angara, and a southern high paleolatitudinal region named Gondwana. Forested peat swamps, extending over hundreds of thousands of square kilometers, grew across this supercontinent during the Mississippian, Pennsylvanian, and Permian in response to changes in global climate. The plants that accumulated as peat do not belong to the plant groups prominent across today’s landscapes. Rather, the plant groups of the Late Paleozoic that are responsible for most of the biomass in these swamps belong to the fern and fern allies: club mosses, horsetails, and true ferns.  Gymnosperms of various systematic affinity play a subdominant role in these swamps, and these plants were more common outside of wetland settings. It is not until the Permian when these seed-bearing plants become more dominant. Due to tectonic activity associated with assembling the supercontinent, including earthquakes and volcanic ashfall, a number of these forests were buried in their growth positions. These instants in time, often referred to as T0 assemblages, provide insight into the paleoecological relationships that operated therein. Details of T0 localities through the Late Paleozoic demonstrate that the plants, and plant communities, of the coal forests are non-analogs to our modern world. Analysis of changing vegetational patterns from the Mississippian into the Permian documents the response of landscapes to overall changes in Earth Systems under icehouse to hothouse conditions.

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

Vegetation
palaeobotany
mires
greenhouse
icehouse
Carboniferous
Permian
Diversity of life
Livets mångfald
Ecosystems and species history
Ekosystem och arthistoria
The changing Earth
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