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Zhang Liping, Huang Difan, Liao Zhiqin. Gammacerane —Geochemical Indicator of Water Column Stratification[J]. Acta Sedimentologica Sinica, 1999, 17(1): 136-140.
Citation: Zhang Liping, Huang Difan, Liao Zhiqin. Gammacerane —Geochemical Indicator of Water Column Stratification[J]. Acta Sedimentologica Sinica, 1999, 17(1): 136-140.

Gammacerane —Geochemical Indicator of Water Column Stratification

  • Received Date: 1998-06-08
  • Rev Recd Date: 1998-07-20
  • Publish Date: 1999-03-10
  • Distribution of gammacerane in some marine evapo ritic environments such as Michigan basin shows that gammacerane, a hy persaline biomarker, is not absolutely associated with hy persaline envi ronment ;Relative higher concent ration of g ammacerane in Song liao fresh-brackish lacustrine envi ronment is connected w ith water column stratification caused by event of linking between lacust rine and sea. Both stable carbon isotopic compositions of gammacerane and microbiology indicate that the formation of gammacerane is related to water column strat if ication.Since water columns in hypersaline depositional environments are of ten density st ratified, it explains w hy g ammacerane is of ten found in sediments deposi ted under hypersaline conditions but is not necessarily restricted in this type of deposits.
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  • Received:  1998-06-08
  • Revised:  1998-07-20
  • Published:  1999-03-10

Gammacerane —Geochemical Indicator of Water Column Stratification

Abstract: Distribution of gammacerane in some marine evapo ritic environments such as Michigan basin shows that gammacerane, a hy persaline biomarker, is not absolutely associated with hy persaline envi ronment ;Relative higher concent ration of g ammacerane in Song liao fresh-brackish lacustrine envi ronment is connected w ith water column stratification caused by event of linking between lacust rine and sea. Both stable carbon isotopic compositions of gammacerane and microbiology indicate that the formation of gammacerane is related to water column strat if ication.Since water columns in hypersaline depositional environments are of ten density st ratified, it explains w hy g ammacerane is of ten found in sediments deposi ted under hypersaline conditions but is not necessarily restricted in this type of deposits.

Zhang Liping, Huang Difan, Liao Zhiqin. Gammacerane —Geochemical Indicator of Water Column Stratification[J]. Acta Sedimentologica Sinica, 1999, 17(1): 136-140.
Citation: Zhang Liping, Huang Difan, Liao Zhiqin. Gammacerane —Geochemical Indicator of Water Column Stratification[J]. Acta Sedimentologica Sinica, 1999, 17(1): 136-140.
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