{"refrec":{"BRefID":303224,"RR":"<b>Kerney, M.P.; Preece, R.C.; Turner, C.</b> (1980). Molluscan and plant biostratigraphy of some Late Devensian and Flandrian deposits in Kent. <i>Philosophical Transactions of the Royal Society of London Series B-Biological Sciences 291(1044)</i>: 1-43. <a href=\"https://dx.doi.org/10.1098/rstb.1980.0126\" target=\"_blank\">https://dx.doi.org/10.1098/rstb.1980.0126</a>","BEntID":295518,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Philosophical Transactions of the Royal Society of London Series B-Biological Sciences 291(1044)</i>: 1-43. <a href=\"https://dx.doi.org/10.1098/rstb.1980.0126\" target=\"_blank\">https://dx.doi.org/10.1098/rstb.1980.0126</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Kerney, M.P.; Preece, R.C.; Turner, C.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Kerney, M.P. <i>et al.</i>","Englishabstract":"Sequences of calcareous slope and spring deposits (mainly tufa) are described from two localities in Kent (Folkestone and Wateringbury). They contain rich faunas of terrestrial Mollusca, allowing a detailed reconstruction of the local environments. The faunal changes also reveal an underlying common pattern, ascribed largely to the effects of climate and migration. Eight biostratigraphical assemblage zones are proposed, applicable to deposits of this general character in the area of southern England. The base of each zone is defined as follows: zone y first appearance of a molluscan fauna, dominantly of <i>Pupilla, Vallonia</i> and <i>Vitrina</i>; zone z expansion of Abida and <i>Trichia</i>; zone a decline of <i>Pupilla</i>, appearance of <i>Carychium</i> and <i>Aegopinella</i>; zone b expansion of <i>Carychium</i> and <i>Aegopinella</i>, occurrence of Discus ruderatus; zone c expansion of <i>Discus rotundatus</i>, suppression of <i>Discus ruderatus</i>; zone d expansion of <i>Oxychilus cellarius</i>; zone e re-expansion of <i>Vallonia</i>; zone f appearance of <i>Helix aspersa</i>. Botanical evidence (pollen and seeds) and some radiocarbon dates allow a partial correlation of the zones with the standard Godwin pollen zones of the Late Devensian (late-glacial) and the Flandrian.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Molluscan and plant biostratigraphy of some Late Devensian and Flandrian deposits in Kent","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1980,"MonPub":null,"DateUpdate":"2018-11-26","DateCreate":"2018-11-26","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:A1980KS11000001","VABBcode":null,"OpenAcc":0,"DOI":"10.1098/rstb.1980.0126"},"refs":null,"anarec":{"AnaID":303224,"PubliDate":1980,"Pagination":"1-43","XtraPublOfAnaID":null,"ISBN":null,"Volume":"291","Issue":"1044","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":276311,"SerRR":"Philosophical Transactions of the Royal Society of London Series B-Biological Sciences. 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