2001
DOI: 10.1006/bojl.2000.0409
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Plant assemblages from the Silurian of southern Bolivia and their palaeogeographic significance

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Cited by 10 publications
(14 citation statements)
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“…This is in agreement with data from Ludlow, Pridoli and earliest Lochkovian plant localities all over the world (Edwards, 1979;Tims and Chambers, 1984;Cai et al, 1993;Edwards et al, 2001;Gerrienne et al, 2001;Kotyk et al, 2002). The early flora of the South China block was mainly comprised of early lycophytes and plants with rhyniophytoid architecture and reniform sporangia.…”
Section: Discussionsupporting
confidence: 90%
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“…This is in agreement with data from Ludlow, Pridoli and earliest Lochkovian plant localities all over the world (Edwards, 1979;Tims and Chambers, 1984;Cai et al, 1993;Edwards et al, 2001;Gerrienne et al, 2001;Kotyk et al, 2002). The early flora of the South China block was mainly comprised of early lycophytes and plants with rhyniophytoid architecture and reniform sporangia.…”
Section: Discussionsupporting
confidence: 90%
“…The Wutubulake flora is coeval to that of the Van Canh Formation at Dô Son. However Wutubulake was part of the Khazakhstanian block (Edwards, 1990;Edwards et al, 2001). Khazakhstania was located on the equatorial belt of the Gondwana (Scotese, 2010).…”
Section: Stratigraphic Bearings Of the Plant Findingsmentioning
confidence: 99%
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“…As this supercontinent straddled the South Pole in MidPalaeozoic times, it has the potential to provide information on high-latitude vegetation, to some extent realized by descriptions of Silurian plants from Bolivia (Edwards et al 2001a) and Lochkovian and later assemblages from Brazil and Argentina (Edwards et al 2001b). …”
mentioning
confidence: 99%
“…Probable Ludlow examples from the Kirusillas Formation exposed at Sella in theTarija area of southern Bolivia (Figs 1 & 2) include taxa (e.g. Cooksonia) at a similar grade of organization to those found in coeval strata of Laurussia (Edwards et al 2001), but a more reliably dated and far more diverse Ludlow assemblage (Toro et al 1996) from the more northerly Cochabamba region of central Bolivia is reported to include taxa such as Rhynia, Zosterophyllum and Drepanophycus that occur much later at lower palaeolatitudes. Such a discrepancy in this latter report demanded further investigation and, as part of a collaborative multidisciplinary venture between palaeobotanists and sedimentologists from La Plata, Argentina and Cardiff, UK, new collections of both plant and animal fossils were made at a number of localities to the east of Cochabamba.…”
mentioning
confidence: 99%