Carbon isotope (δ13Ccarb) stratigraphy of the Lower–Middle Ordovician (Tremadocian–Darriwilian) in the Great Basin, western United States: Implications for global correlation

Edwards, Cole T.; Saltzman, Matthew R.

doi:10.1016/j.palaeo.2014.02.005

Cited by 62 publications

(52 citation statements)

References 66 publications

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“…13 C carb excursions resulting from sea level change have few contributions to global comparison (Edwards and Saltzman 2014). Therefore, the relationship between three d 13 C carb -positive excursions shown in Figs.…”

Section: Positive Carbon Isotope Excursions and Sea Level Changementioning

confidence: 99%

“…2) of the Tahe oil-gas field in the northern Tarim Basin can be compared or partly compared with that of the Argentine Precordillera (Sial et al 2013;Albanesi et al 2013;Edwards and Saltzman 2014), Oklahoma and Virginia, USA (Young et al 2008), Cincinnati region, USA (Bergström et al 2010), Sweden (Wu et al 2015), and O carb for well S112-1 and well S114 in the Tahe oil-gas field Pet. Sci.…”

Section: Correlation Of Dmentioning

confidence: 99%

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Positive carbon isotope excursions: global correlation and genesis in the Middle–Upper Ordovician in the northern Tarim Basin, Northwest China

Cunge

Liu

et al. 2016

Pet. Sci.

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Section: Positive Carbon Isotope Excursions and Sea Level Changementioning

confidence: 99%

Section: Correlation Of Dmentioning

confidence: 99%

Positive carbon isotope excursions: global correlation and genesis in the Middle–Upper Ordovician in the northern Tarim Basin, Northwest China

Cunge

Liu

et al. 2016

Pet. Sci.

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“…Two detailed ␦ 13 C records exist for the Lower and Middle Ordovician of the Great Basin, USA (Edwards and Saltzman, 2014). An increasing trend in ␦ 13 C is observed during the late Tremadocian to early Floian (Diaphorodus deltatus and Oepikodus communis conodont zones) that probably corresponds to a similar increase in the Latorp Limestone in the Brunflo 2 core (Fig.…”

Section: North Americamentioning

confidence: 99%

“…8. Correlation of ␦ 13 C carb curve from the Brunflo 2 core with those from the Precordillera (Argentina; Buggisch et al, 2003), Shingle Pass (Nevada) and Ibex sections (Utah) in North America (Edwards and Saltzman, 2014). in the upper Lehman Formation, which is interpreted to represent the rising limb of MDICE.…”

Section: North Americamentioning

confidence: 99%

“…These ␦ 13 C excursions are fairly well constrained by means of biostratigraphy and have been formally named, usually from sections in North America (Bergström et al, 2009). In comparison, very few studies have been undertaken in the Lower and Middle Ordovician strata (Buggisch et al, 2003;Ainsaar et al, 2007Ainsaar et al, , 2010Munnecke et al, 2011;Edwards and Saltzman, 2014). The result is that this part of the Ordovician history is far less understood in terms of carbon isotope chemostratigraphy.…”

Section: Introductionmentioning

confidence: 99%

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Lower–Middle Ordovician δ13C chemostratigraphy of western Baltica (Jämtland, Sweden)

Calner

Lehnert

et al. 2015

Palaeoworld

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Middle to Late Ordovician carbon isotope chemostratigraphy of the Lower Yangtze Platform: Implications for global correlation

et al. 2021

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Middle to Late Ordovician carbonates were collected in South China (Anhui Province) from the Kuniutan, Datianba, and Pagoda formations in the Dingxiang and Daling sections and analysed for high-resolution carbon isotope chemostratigraphy. An increase by 0.4‰ in δ 13 C carb is observed in the upper part of the Kuniutan Formation (Eoplacognathus pseudoplanus Biozone), representing the rising limb of the Middle Darriwilian Isotopic Carbon Excursion (MDICE). In the upper part of the Datianba Formation, positive shifts of ca. 1‰ are recorded in the studied section which compare with the carbon shifts reported in North America and Baltoscandia. A pronounced positive δ 13 C carb excursion of ca. 1.5‰ from the lower part of the Pagoda Formation can be correlated with the global Guttenberg Isotopic Carbon Excursion (GICE). The documentation of three carbon isotope shifts in this study provides new evidence for changes in the global carbon cycle from Darriwilian to Early Katian which could have been influenced by changes in global climate and primary productivity.

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Carbon isotope (δ13Ccarb) stratigraphy of the Lower–Middle Ordovician (Tremadocian–Darriwilian) in the Great Basin, western United States: Implications for global correlation

Cited by 62 publications

References 66 publications

Positive carbon isotope excursions: global correlation and genesis in the Middle–Upper Ordovician in the northern Tarim Basin, Northwest China

Positive carbon isotope excursions: global correlation and genesis in the Middle–Upper Ordovician in the northern Tarim Basin, Northwest China

Lower–Middle Ordovician δ13C chemostratigraphy of western Baltica (Jämtland, Sweden)

Middle to Late Ordovician carbon isotope chemostratigraphy of the Lower Yangtze Platform: Implications for global correlation

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