2020
DOI: 10.1016/j.marpetgeo.2020.104434
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The geneses of sedimentary organic matter with anomalous 13C-enriched isotopic composition in saline and freshwater lakes: A case study of lacustrine source rocks from Dongpu and Qikou sags, Bohai Bay Basin, eastern China

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Cited by 11 publications
(6 citation statements)
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“…Moreover, The HI values in the sediment corers of LM and HZ increased with the upcore profile, as shown in Figure S4 in Supporting Information . S2 has been used as a good proxy of algal organic matter because algal organic matter is more resistant than any other organic components during the early diagenesis process (D. Duan et al., 2015; Z. Chen et al., 2020). Thus, the increase of algal organic matter indicates the gradual increase of lacustrine primary productivity.…”
Section: Discussionmentioning
confidence: 99%
“…Moreover, The HI values in the sediment corers of LM and HZ increased with the upcore profile, as shown in Figure S4 in Supporting Information . S2 has been used as a good proxy of algal organic matter because algal organic matter is more resistant than any other organic components during the early diagenesis process (D. Duan et al., 2015; Z. Chen et al., 2020). Thus, the increase of algal organic matter indicates the gradual increase of lacustrine primary productivity.…”
Section: Discussionmentioning
confidence: 99%
“…The residual marine brine of the Jiamuhe Formation under the Fengcheng Formation invaded [48], bringing abundant elements such as Fe, Mn, and Mg [49]. (2) Meanwhile, the various microorganisms in the Fengcheng Formation are beneficial for the enrichment of iron elements [17,24]. (3) Fe elements contributed with medium basic volcanic ash.…”
Section: Indicative Significance Of Iron Dolomite Ringmentioning
confidence: 99%
“…For example, mica interlaminar pores and albite pores formed under the action of alkaline fluids are good oil storage spaces. The diagenetic phenomena of alkaline diagenesis are diverse, including alkali lacustrine salt rocks [16], alkaline evaporative salt minerals [17], and quartz dissolution under the action of alkaline groundwater [18]. In addition, alkaline diagenesis may also provide a new explanation for the silicification of metal deposits, the origin of siliceous cementation, and the reddening and fragmentation of rocks [11][12][13][14][15][16][17][18][19].…”
Section: Introductionmentioning
confidence: 99%
“…S2 represents higher molecular weight algae-derived aliphatic hydrocarbons. It has been applied in the pyrolysis of algal macromolecular organic matter because this material degrades less easily than other organic components in early diagenesis (Chen et al, 2020;Duan et al, 2015). Moreover, photosynthesis could fractionate the isotopic values of CO 2 .…”
Section: Om Input and Variation In The Sediment Coresmentioning
confidence: 99%
“…Algae prefer lighter CO 2 when high biological productivity and dissolved CO 2 are insufficient. Plankton consumes more bicarbonate ions in water because the carbon isotopic composition of bicarbonate is 7-10‰ heavier than that of dissolved CO 2 (Chen et al, 2020), which leads to enrichment of 13 C in these organisms.…”
Section: Om Input and Variation In The Sediment Coresmentioning
confidence: 99%