2015
DOI: 10.1016/j.sedgeo.2015.04.003
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Soils, slopes and source rocks: Application of a soil chemistry model to nutrient delivery to rift lakes

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Cited by 4 publications
(2 citation statements)
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“…Previous studies have shown that OC and SR accumulation are controlled by the complex interplay of primary productivity, dilution and preservation of OM, which are further influenced by a number of factors such as lake level fluctuations, changes in hinterland and basin slope angles and inorganic sediment and terrestrial OM input 3,6,7,[10][11][12][50][51][52][53][54] . Despite recent progress in understanding these processes (e.g., Bohacs et al 55 , Ellis et al 6 ), SR accumulation in rift-lake systems is particularly complex and therefore remains hard to generalize 3 .…”
Section: Discussionmentioning
confidence: 99%
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“…Previous studies have shown that OC and SR accumulation are controlled by the complex interplay of primary productivity, dilution and preservation of OM, which are further influenced by a number of factors such as lake level fluctuations, changes in hinterland and basin slope angles and inorganic sediment and terrestrial OM input 3,6,7,[10][11][12][50][51][52][53][54] . Despite recent progress in understanding these processes (e.g., Bohacs et al 55 , Ellis et al 6 ), SR accumulation in rift-lake systems is particularly complex and therefore remains hard to generalize 3 .…”
Section: Discussionmentioning
confidence: 99%
“…These studies have revealed the importance of factors such as width-depth ratio on the lake’s mixing potential, primary productivity and anoxia 10 . In addition to internal nutrient recycling, hinterland derived nutrient supply can be important for productivity, and depend on evolution of the hinterland topography 3 , 12 . Several studies have also documented the sensitivity of lake levels for high-frequency climatic changes 5 , 11 , 13 , a feature that is less straightforward to reconstruct from ancient sediment series.…”
Section: Introductionmentioning
confidence: 99%