Coal facies studies in Canada

Kalkreuth, W.

doi:10.1016/j.coal.2003.06.001

Cited by 10 publications

(2 citation statements)

References 36 publications

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“…Multiple lines of evidence support the notion that a wet Arctic became wetter during the PETM (Carmichael et al, 2017). Abundant Paleocene coal deposits in Northern Canada, Alaska, and Spitsbergen provide evidence for a wet climate in the Arctic (Kalkreuth, 2004;Lüthje, 2008;McIver & Basinger, 1999;Mull et al, 2003). Warmer air masses in the early Eocene can hold more water vapor and their movement would have carried more moisture poleward (Fricke, 2003;Fricke et al, 1998), resulting in more precipitation locally (Sloan et al, 1995).…”

Section: Did Carbon Isotope Fractionation For C 3 Land Plant Leaf Lipids Increase In Spitsbergen During the Petm?mentioning

confidence: 87%

Synchronous Marine and Terrestrial Carbon Cycle Perturbation in the High Arctic During the PETM

Cui

Diefendorf

Kump

et al. 2021

Paleoceanog and Paleoclimatol

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This climate anomaly has attracted much attention since it is perhaps the best analog for the climate response to greenhouse gas emissions from fossil fuel combustion (Dunkley Jones et al., 2010;Haywood et al., 2011), although the PETM occurred at a rate that is at least an order of magnitude slower than the rate of anthropogenic carbon release (Cui et al., 2011;Zeebe et al., 2016). The PETM is associated with drastic and transient environmental change, including marine and terrestrial ecosystem reorganization (

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Section: Did Carbon Isotope Fractionation For C 3 Land Plant Leaf Lipids Increase In Spitsbergen During the Petm?mentioning

confidence: 87%

Synchronous Marine and Terrestrial Carbon Cycle Perturbation in the High Arctic During the PETM

Cui

Diefendorf

Kump

et al. 2021

Paleoceanog and Paleoclimatol

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“…No anthropogenic activities or historical accidental spills have been recorded in this area. However, Ellesmere Island is known for its numerous coal deposits (Ricketts and Embry, 1984;Kalkreuth, 2004;Harrison et al, 2011). Coal layers outcrop along the Stenkul Fiord, literally meaning the Coal Fiord, which is part of the Eureka Sound Group coals and occurs approximately 60 km north of the Grise Fiord (Kalkreuth et al, 1996).…”

Section: Distribution Of the Pahs In Recent Sedimentsmentioning

confidence: 99%

Spatial and Temporal Distributions of Polycyclic Aromatic Hydrocarbons in Sediments from the Canadian Arctic Archipelago

Corminboeuf¹,

Montero‐Serrano²,

St‐Louis³

2021

Preprint

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<p>The concentrations of 23 polycyclic aromatic hydrocarbons (PAHs; 16 parent and 7 alkylated PAHs) in 113 surface marine sediment samples, 13 on-land sediment samples and 8 subsampled push cores retrieved from the Canadian Arctic Archipelago (CAA) were calculated. PAHs were extracted via accelerated solvent extraction (ASE) and quantified via gas chromatography-mass spectrometry (GC-MS). The sums of the concentrations 16 PAHs in the surface sediments ranged from 7.8 to 247.7 ng g<sup>-1</sup> (dry weight [dw]) basis). The PAH inputs to the sediments have remained constant during the last century and agree with the results obtained for the surface sediments. Diagnostic ratios indicated that the PAHs in the CAA mainly originate from natural petrogenic sources, with some pyrogenic sources. Temporal trends did not indicate major source shifts and largely indicated petrogenic inputs. Overall, the sediments retrieved from the CAA have low PAH concentrations that are mainly natural.</p>

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The evaporite–coal transition: Chemical, mineralogical and organic composition of the Late Triassic Abu Ruweis Formation, NW Jordan—Reference type of the “Arabian Keuper”

et al. 2012

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Coal facies studies in Canada

Cited by 10 publications

References 36 publications

Synchronous Marine and Terrestrial Carbon Cycle Perturbation in the High Arctic During the PETM

Synchronous Marine and Terrestrial Carbon Cycle Perturbation in the High Arctic During the PETM

Spatial and Temporal Distributions of Polycyclic Aromatic Hydrocarbons in Sediments from the Canadian Arctic Archipelago

The evaporite–coal transition: Chemical, mineralogical and organic composition of the Late Triassic Abu Ruweis Formation, NW Jordan—Reference type of the “Arabian Keuper”

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