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Sökning: L773:0016 7606 OR L773:1943 2674 > Refined Permian-Tri...

Refined Permian-Triassic floristic timeline reveals early collapse and delayed recovery of south polar terrestrial ecosystems

Mays, Chris, 1983- (författare)
Naturhistoriska riksmuseet,Enheten för paleobiologi
Vajda, Vivi (författare)
Naturhistoriska riksmuseet,Enheten för paleobiologi,Department of Geology, Lund University, Sweden
Frank, Tracy (författare)
University of Nebraska
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Fielding, Christopher (författare)
University of Nebraska
Nicoll, Robert (författare)
Geoscience Australia
Tevyaw, Allen (författare)
University of Nebraska
McLoughlin, Stephen, 1964- (författare)
Naturhistoriska riksmuseet,Enheten för paleobiologi
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 (creator_code:org_t)
Boulder : Geological Society of America, 2020
2020
Engelska.
Ingår i: Geological Society of America Bulletin. - Boulder : Geological Society of America. - 0016-7606 .- 1943-2674. ; 132, s. 1489-1513
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • The collapse of late Permian (Lopingian) Gondwanan floras, characterized by the extinction of glossopterid gymnosperms, heralded the end of one of the most enduring and extensive biomes in Earth’s history. The Sydney Basin, Australia, hosts a near continuous, age-constrained succession of high southern paleolatitude (∼65–75°S) terrestrial strata spanning the end-Permian extinction (EPE) interval. Sedimentological, stable carbon isotopic, palynological, and macrofloral data were collected from two cored coal-exploration wells and correlated. Six palynostratigraphic zones, supported by ordination analyses, were identified within the uppermost Permian to Lower Triassic succession, corresponding to discrete vegetation stages before, during, and after the EPE interval. Collapse of the glossopterid biome marked the onset of the terrestrial EPE and may have significantly predated the marine mass extinctions and conodont-defined Permian–Triassic Boundary. Apart from extinction of the dominant Permian plant taxa, the EPE was characterized by a reduction in primary productivity, and the immediate aftermath was marked by high abundances of opportunistic fungi, algae, and ferns. This transition is coeval with the onset of a gradual global decrease in δ13Corg and the primary extrusive phase of Siberian Traps Large Igneous Province magmatism. The dominant gymnosperm groups of the Gondwanan Mesozoic (peltasperms, conifers, and corystosperms) all appeared soon after the collapse but remained rare throughout the immediate post-EPE succession. Faltering recovery was due to a succession of rapid and severe climatic stressors until at least the late Early Triassic. Immediately prior to the Smithian–Spathian boundary (ca. 249 Ma), indices of increased weathering, thick redbeds, and abundant pleuromeian lycophytes likely signify marked climate change and intensification of the Gondwanan monsoon climate system. This is the first record of the Smithian–Spathian floral overturn event in high southern latitudes.

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

Permian
Triassic
extinction
fossil flora
palynology
Gondwana
Australia
Smithian-Spathian
Diversity of life
Livets mångfald
Ecosystems and species history
Ekosystem och arthistoria
The changing Earth
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ref (ämneskategori)
art (ämneskategori)

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