2016
DOI: 10.1016/j.palaeo.2016.09.003
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Nearshore euxinia in the photic zone of an ancient sea: Part II – The bigger picture and implications for understanding ocean anoxia

Abstract: University of Bristol -Explore Bristol Research General rightsThis document is made available in accordance with publisher policies. Please cite only the published version using the reference above.

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Cited by 17 publications
(12 citation statements)
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“…7) can be utilized to differentiate between oxic and reducing palaeodepositional environments, but the distributions can be affected by maturity 287 and secondary alteration (Peters and Moldowan, 1991). The distribution for oils from NE (Słowakiewicz et al, 2016a). 301 All oil samples are characterised by the dominance of C30 17α-hopane over lower or 302 higher homologues in many oil samples (Fig.…”
mentioning
confidence: 99%
“…7) can be utilized to differentiate between oxic and reducing palaeodepositional environments, but the distributions can be affected by maturity 287 and secondary alteration (Peters and Moldowan, 1991). The distribution for oils from NE (Słowakiewicz et al, 2016a). 301 All oil samples are characterised by the dominance of C30 17α-hopane over lower or 302 higher homologues in many oil samples (Fig.…”
mentioning
confidence: 99%
“…In addition, comparisons are made in this paper to previously published and reported herein biomarker data from fourteen samples of KAF dolomite lagoonal facies (onshore equivalent of the Innes Carbonate Member of the NPB) of the Malton 4 well (Słowakiewicz et al, 2016), and typical carbon isotopic values for saturated and aromatic fractions of Jurassic, Permian and Devonian oil from the SPB and North Sea areas.…”
Section: Sample Collectionmentioning
confidence: 95%
“…In addition, the Toarcian Whitby Mudstone Formation is in the early oil window (French et al, 2014), but the Carboniferous Bowland Shale-Hodder Mudstone shales are thermally mature for gas (Haarhoff et al, 2018). Higher thermal maturity (R o ~0.8-0.9 %) has also been noted in Lockton 2a KAF limestone slope facies, revealed by negative δ 18 O values (-2 to -14 ‰), the presence of saddle dolomite and increased abundance of tricyclic and tetracyclic terpenoids (Słowakiewicz et al, 2016). 4) from the roof of the Boulby Mine at workings (2000 West Salt) at a depth of 1100 m subsurface were collected by hand into pre-furnaced glass jars.…”
Section: Distribution and Perception Of Thermal Maturitymentioning
confidence: 95%
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“…12), as well as the observed slightly marked unresolved complex mixture in the aliphatic compounds of one particular sample (not shown), are a reflection of the clay-minerals present at this depth (3229.5 m), where partial microbial reworking of the deposited algal OM took place. This is probably the result of episodic suboxic conditions in the shallow-water column (Słowakiewicz et al 2015(Słowakiewicz et al , 2016 around the Zielin-3Kbis well area. The cross-plot developed by Hughes et al (1995) for a wide maturity range of hydrocarbons, expressed as the dependence of dibenzothiophene/phenanthrene ratio (DBT/P) vs. Pr/Ph ratio, is useful in determining the depositional environment of a source rock and the lithology in which it was generated.…”
Section: Molecular Composition Of Hydrocarbons and Dibenzothiophenesmentioning
confidence: 99%