2011
DOI: 10.1016/j.gr.2010.11.008
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Glaciation and ~770Ma Ediacara (?) Fossils from the Lesser Karatau Microcontinent, Kazakhstan

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Cited by 60 publications
(33 citation statements)
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“…Large carbon negative anomalies (Shuram excursion) are found in most Ediacaran sediments (e.g. Meert et al, 2011). the combination of δ 13 C and δ 18 O profiles is limited in the Neoproterozoic Era, because oxygen isotopes are relatively mobile during post-depositional alteration (Banner and Hanson, 1990) and have only been used to identify altered samples (e.g. Kaufman and Knoll, 1995;Kaufman et al, 2006;Zhu et al, 2007).…”
Section: Introductionmentioning
confidence: 99%
“…Large carbon negative anomalies (Shuram excursion) are found in most Ediacaran sediments (e.g. Meert et al, 2011). the combination of δ 13 C and δ 18 O profiles is limited in the Neoproterozoic Era, because oxygen isotopes are relatively mobile during post-depositional alteration (Banner and Hanson, 1990) and have only been used to identify altered samples (e.g. Kaufman and Knoll, 1995;Kaufman et al, 2006;Zhu et al, 2007).…”
Section: Introductionmentioning
confidence: 99%
“…Meert et al, 2011). Nimbia has been reported from Ediacaran localities such as the Krol-Tal Belt (India), West Africa, the Flinders Ranges (Australia), the Great Basin (Western U.S.A.), the Digermul Peninsula (Norway), the Avalonian blocks of Newfoundland and the White Sea Region (Russia) (Hofmann et al, 1990;Crimes et al, 1995;Crimes and McIlroy, 1999;Gehling et al, 2000;Fedonkin, 2003;Shanker et al, 2004;Bertrand-Sarfati et al, 1995;Meert et al, 2011).…”
Section: Discussionmentioning
confidence: 99%
“…However the segmentation that is found in the Sonia structures is absent in Nimbia occlusa. Aspidella terranovica has been described from the Podolia, Ukraine, the Ural Mountains, NW Canada, the Avalon Peninsula, Newfoundland, Namibia and Kazakhstan (Gehling et al, 2000;Meert et al, 2011). The structure of the Sonia Sandstone is dissimilar to Aspidella terranovica in many aspects.…”
Section: Discussionmentioning
confidence: 99%
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“…A combination of simple morphology and indifferent preservation of most softbodied Ediacaran and Cryogenian fossils has com poun ded the mystery: none can be unequivocally attributed to metazoans (Antcliffe & Brasier 2008, Antcliffe et al 2011, Erwin et al 2011, Meert et al 2011). Some of these Sun et al 1986;Meert et al 2011 un skeletonized Ediacaran organisms lived on dry land (Retallack 2013 a). Skeletonized and phosphatic Cryogenian and Ediacaran fossils including Cloudina and Corumbella are more convincing as animals, but difficult to assign to modern animal groups (Fedonkin et al 2008.…”
Section: Acritarch Diversification Reconsideredmentioning
confidence: 99%