{"title":"The Aragonian type area revisited; comments on paleontology and stratigraphy","authors":"M. Freudenthal, E. Martín-Suárez","doi":"10.1344/GEOLOGICAACTA2018.16.2.3","DOIUrl":null,"url":null,"abstract":"In a recent study of van der Meulen and coauthors, the fossil rodents Fahlbuschia , Pseudofahlbuschia and Renzimys from the Aragonian type area (Calatayud Basin, Spain) were synonimized with Democricetodon . On the basis of the relative chronology provided by Daams and coauthors in an earlier study, these authors construed two evolutionary lineages, distinguished by size. One of these lineages contains Fahlbuschia koenigswaldi (Freudenthal, 1963) and the other one Democricetodon moralesi van der Meulen et al. (2004) but, in view of their great similarity, we consider D. moralesi to be a synonym of F. koenigswaldi . The relative stratigraphic position of some fossil mammal localities is difficult to establish in the Aragonian type area because it is affected by folds and faults. Early studies of Daams and Freudenthal subdivided the local zone D into D1, D2, D3 and gave a scheme of the stratigraphy in which the fossiliferous locality Valdemoros 1A is considered to be older than Valdemoros 3B. But Daams and coauthors came to the opposite interpretation in a later study, and divided zone D in Da, Db, Dc, Dd. But, new field data presented here enforce the original interpretation in which Valdemoros 1A is older than Valdemoros 3B. This leads to the conclusion that the division of local zone D into Da to Dd has to be discarded, and substituted by the formerly proposed zonation D1-D3.","PeriodicalId":55107,"journal":{"name":"Geologica Acta","volume":null,"pages":null},"PeriodicalIF":1.3000,"publicationDate":"2018-06-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geologica Acta","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1344/GEOLOGICAACTA2018.16.2.3","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOLOGY","Score":null,"Total":0}
引用次数: 1
Abstract
In a recent study of van der Meulen and coauthors, the fossil rodents Fahlbuschia , Pseudofahlbuschia and Renzimys from the Aragonian type area (Calatayud Basin, Spain) were synonimized with Democricetodon . On the basis of the relative chronology provided by Daams and coauthors in an earlier study, these authors construed two evolutionary lineages, distinguished by size. One of these lineages contains Fahlbuschia koenigswaldi (Freudenthal, 1963) and the other one Democricetodon moralesi van der Meulen et al. (2004) but, in view of their great similarity, we consider D. moralesi to be a synonym of F. koenigswaldi . The relative stratigraphic position of some fossil mammal localities is difficult to establish in the Aragonian type area because it is affected by folds and faults. Early studies of Daams and Freudenthal subdivided the local zone D into D1, D2, D3 and gave a scheme of the stratigraphy in which the fossiliferous locality Valdemoros 1A is considered to be older than Valdemoros 3B. But Daams and coauthors came to the opposite interpretation in a later study, and divided zone D in Da, Db, Dc, Dd. But, new field data presented here enforce the original interpretation in which Valdemoros 1A is older than Valdemoros 3B. This leads to the conclusion that the division of local zone D into Da to Dd has to be discarded, and substituted by the formerly proposed zonation D1-D3.
在van der Meulen及其合著者最近的一项研究中,来自Aragonian类型地区(西班牙卡拉塔尤德盆地)的啮齿类化石Fahlbuschia、Pseudofahlbushia和Renzimys与Democricetodon同义。根据Daams和合著者在早期研究中提供的相对年表,这些作者解释了两个按大小区分的进化谱系。其中一个谱系包含Fahlbuschia koenigswaldi(Freudenthal,1963)和另一个谱系Democricetodon moralesi van der Meulen等人(2004),但鉴于它们的巨大相似性,我们认为D.moralesi是F.koenigswalldi的同义词。由于受到褶皱和断层的影响,在Aragonian型地区很难确定一些哺乳动物化石所在地的相对地层位置。Daams和Freudenthal的早期研究将当地的D带细分为D1、D2和D3,并给出了一个地层学方案,其中化石产地Valdemoros 1A被认为比Valdemoros 3B更古老。但Daams和合著者在后来的一项研究中得出了相反的解释,并将D区划分为Da、Db、Dc、Dd。但是,这里提供的新现场数据加强了最初的解释,即瓦尔迪摩罗斯1A比瓦尔迪摩洛斯3B更古老。这导致了这样的结论,即必须放弃将局部区域D划分为Da到Dd,并由先前提出的分区D1-D3代替。
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