1983
DOI: 10.1086/337376
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Megagametophyte Development in the Chaloneriaceae Fam. Nov., Permineralized Paleozoic Isoetales (Lycopsida)

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Cited by 37 publications
(10 citation statements)
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“…This can be seen most clearly in the Isoetales, where the rhizomorph displays a variety of forms, from the small rhizomorph of Oxroadia (Long, ; Bateman, ) and Paurodendron (Phillips & Leisman, ; Rothwell & Erwin, ; Fig. g), to the cormose rhizomorphs of groups such as the Chaloneriaceae (Pigg & Rothwell, ,b); Pleuromeiaceae (Grauvogel‐Stamm, ) and Isoetaceae (Paolillo, ; Retallack, ), to the giant rhizomorph axes known as stigmarian axes (Stewart & Rothwell, ), which extended up to 15 m and occasionally further from the trunks of large trees (Fig. h).…”
Section: Disparity In the Structures From Which Lycopsid Roots Developmentioning
confidence: 99%
“…This can be seen most clearly in the Isoetales, where the rhizomorph displays a variety of forms, from the small rhizomorph of Oxroadia (Long, ; Bateman, ) and Paurodendron (Phillips & Leisman, ; Rothwell & Erwin, ; Fig. g), to the cormose rhizomorphs of groups such as the Chaloneriaceae (Pigg & Rothwell, ,b); Pleuromeiaceae (Grauvogel‐Stamm, ) and Isoetaceae (Paolillo, ; Retallack, ), to the giant rhizomorph axes known as stigmarian axes (Stewart & Rothwell, ), which extended up to 15 m and occasionally further from the trunks of large trees (Fig. h).…”
Section: Disparity In the Structures From Which Lycopsid Roots Developmentioning
confidence: 99%
“…Based on material from North American coal balls, Pigg & Rothwell (1983a) subsequently showed that some plants with the same distinctive and widely distributed spores as Polysporia mirabilis had fertile zones, rather than terminal cones. They named the reconstructed whole plant Chaloneria cormosa , as the basis for recognizing a new family of isoetalean lycopsids, the Chaloneriaceae (Pigg & Rothwell 1983b).…”
Section: Carboniferous Fossil Plants and Sporesmentioning
confidence: 99%
“…Thus, Retallack (1997, pp. 515–516) suggested that it ‘seems more likely that subarborescent Triassic lycopsids evolved from herbaceous Isoetes , and these from subarborescent Palaeozoic lycopsids such as Chaloneria (Pigg and Rothwell 1983 a , b ), rather than from arborescent Palaeozoic lycopsids such as Sigillaria (Mägdefrau 1931, p. 133)’. Although Isoetes beestonii appears very early after the Permian/Triassic boundary, this does not necessarily mean that it is the linking group between the Palaeozoic and Mesozoic arborescent to subarborescent lycophytes.…”
Section: Evolutionary Considerationsmentioning
confidence: 99%