2006
DOI: 10.1666/0022-3360(2006)80[447:ecftlm]2.0.co;2
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Eocene Conchostracans From the Laney Member of the Green River Formation, Wyoming, Usa

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Cited by 20 publications
(2 citation statements)
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“…Recent studies (Martin & Davis 2001) based on molecular and morphological analyses, indicate a nonmonophyletic status for 'Conchostraca', hence this group is no longer considered a strict taxonomic unit (Fryer 1987, Olesen 1998, Stenderup et al 2006, Li et al ALCHERINGA PERMO-TRIASSIC SPINICAUDATANS FROM ARGENTINA 2009a, b, c). According to Martin & Davis (2001), Diplostraca is now divided into four extant suborders (Laevicaudata, Spinicaudata, Cyclestherida and Cladocera); however, Shen (2003Shen ( , 2011, Shen et al (2006), andHuang (2008) proposed the incorporation of two extinct suborders (Leaiina and Estheriellina). The terms 'clam-shrimp' and 'conchostraca' are still useful to make reference to laevicaudatans, spinicaudatans, leaiids, estherielliids and cyclestherids in non-technical publications.…”
Section: Systematic Palaeontologymentioning
confidence: 99%
“…Recent studies (Martin & Davis 2001) based on molecular and morphological analyses, indicate a nonmonophyletic status for 'Conchostraca', hence this group is no longer considered a strict taxonomic unit (Fryer 1987, Olesen 1998, Stenderup et al 2006, Li et al ALCHERINGA PERMO-TRIASSIC SPINICAUDATANS FROM ARGENTINA 2009a, b, c). According to Martin & Davis (2001), Diplostraca is now divided into four extant suborders (Laevicaudata, Spinicaudata, Cyclestherida and Cladocera); however, Shen (2003Shen ( , 2011, Shen et al (2006), andHuang (2008) proposed the incorporation of two extinct suborders (Leaiina and Estheriellina). The terms 'clam-shrimp' and 'conchostraca' are still useful to make reference to laevicaudatans, spinicaudatans, leaiids, estherielliids and cyclestherids in non-technical publications.…”
Section: Systematic Palaeontologymentioning
confidence: 99%
“…Analyses of spore-pollen assemblages suggest a Lower Tertiary age but this does not exclude the possibility of a Late Cretaceous age (Nanjing Institute of Geology and Palaeontology et al, 1975). An early Eocene age (Ypresian) is more convincing on the basis of the study of the conchostracan Paraleptestheria menglaensis (Chen and Shen, 1980;Shen et al, 2006).…”
Section: Introductionmentioning
confidence: 99%