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Late Palaeozoic palynomorph assemblages from the Karoo Supergroup and their potential for biostratigraphic correlation, Kalahari Karoo Basin, Botswana

机译:博茨瓦纳卡拉哈里卡鲁盆地,来自卡鲁超群的晚古生古孢粉组合及其生物地层相关性的潜力

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LateCarbonifeoustoPermiancoresamplesfromtwoboreholesections,STRAT1andCKP6,thatpenetratetheglacialtopostglacialandcoal-bearingLowerKaroosequence,KalahariKarooBasin,Botswana,containwellpreservedpollenandsporepalynomorphs.Thepalynomorphassemblagescomprise165speciesofsporesandpollen,andfewacritarchsandchlorophyceanalgae.Thispaperpresentsalocalbiozonationofthreesucceedingassemblagezones,recognisableineachboreholesection.Theassemblagezonesarenamed:theHamiapollenitesbullaeformisBiozone,theCyclogranisporitesgondwanensisBiozoneandthePlatysaccuspapilionis-StriatopodocarpitesfususBiozone,inascendingorderofstratigraphy.AssemblagesarecomparedandcorrelatedwithassemblagesdescribedfromotherGondwanaareasofAfrica,Australia,Arabia,SouthAmericaandAntarctica.AgeneralanalysisoftaxafromtheKalahariKarooBasinindicatesadistinctsimilaritywithassemblagesfromtheParan??BasinofSouthAmerica.TheHamiapollenitesbullaeformisBiozoneiscomparablewiththeVittatinacostabilisIntervalZoneoftheParan??Basin.AssemblagesfromtheCyclogranisporitesgondwanensisandthePlatysaccuspapilionis-StriatopodocarpitesfususzonesarecomparablewiththeLueckisporitesvirkkiaeIntervalZone.AgedeterminationfortheassemblagesintheKalahariKarooBasinisinferredfromcomparisonwithsimilarassemblagesfrompreviousGondwanastudies,andrangesfromtheLateCarboniferous(Kasimovian-Gzhelian)tolatestEarlyorpossiblyearliestMiddlePermian(LateCisulariantoEarlyGuadalupian).
机译:LateCarbonifeoustoPermiancoresamplesfromtwoboreholesections,STRAT1andCKP6,thatpenetratetheglacialtopostglacialandcoal-bearingLowerKaroosequence,KalahariKarooBasin,博茨瓦纳,containwellpreservedpollenandsporepalynomorphs.Thepalynomorphassemblagescomprise165speciesofsporesandpollen,andfewacritarchsandchlorophyceanalgae.Thispaperpresentsalocalbiozonationofthreesucceedingassemblagezones,recognisableineachboreholesection.Theassemblagezonesarenamed:theHamiapollenitesbullaeformisBiozone,theCyclogranisporitesgondwanensisBiozoneandthePlatysaccuspapilionis-StriatopodocarpitesfususBiozone,inascendingorderofstratigraphy.AssemblagesarecomparedandcorrelatedwithassemblagesdescribedfromotherGondwanaareasofAfrica,澳大利亚,沙特阿拉伯,SouthAmericaandAntarctica.AgeneralanalysisoftaxafromtheKalahariKarooBasinindicatesadistinctsimilaritywithassemblagesfromtheParan ?? BasinofSouthAmerica.TheHamiapollenitesbullaeformisBiozoneiscomparablewiththeVittatinacostabilisIntervalZoneoftheParan ??盆地。自行车组合granisporitesgondwanensisandthePlatysaccuspapilionis-StriatopodocarpitesfususzonesarecomparablewiththeLueckisporitesvirkkiaeIntervalZone.AgedeterminationfortheassemblagesintheKalahariKarooBasinisinferredfromcomparisonwithsimilarassemblagesfrompreviousGondwanastudies,andrangesfromtheLateCarboniferous(Kasimovian-Gzhelian)tolatestEarlyorpossiblyearliestMiddlePermian(LateCisulariantoEarlyGuadalupian)。

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