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Morphometric And Stratophenetic Basis For Phytogeny And Taxonomy In Late Cretaceous Gublerinid Planktonic Foraminifera

机译:晚白垩世粗斜纹浮游有孔虫的植物学和分类学的形态学和地层学基础

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Taxonomic revision of the gublerinid serial planktonic foraminifera of the Late Cretaceous (late Campanian-Maastrichtian) reveals that the group consists of two genera, Gublerina Kikoiene 1948 and Praegublerina gen. nov., which evolved from the finely costate, biserial species Heterohelixplanata (Cushman 1938). Three species are included within Praegublerina: P. pseudotessera (Cushman 1938), P. acuta (de Klasz 1953) and P. robusta (de Klasz 1953), the first being the oldest of the genus and a descendant of Heterohelix planata (Cushman 1938). Gublerina cuvillieri Kikoine 1948 and G. rajagopalani Govindan 1972 are retained within Gublerina. The two lineages are recognized based on gross test architecture, test ornamentation, pore size and internal test morphology. Our study reveals the existence of an evolutionary continuum between lineages in which the gublerinid-type chamber proliferation is independently developed in Gublerina and Praegublerina. The new taxonomic framework reflects the iterative pattern of planktonic foraminiferal evolution and it results in a better understanding of the stratigraphic and geographic distribution of the gublerinid taxa. Stable isotopic comparison of G. rajagopalani and G. cuvillieri with co-occurring late Maastrichtian benthic and planktonic species indicates that the two Gublerina species shared the same depth habitat near the thermocline.
机译:对晚白垩世(Campanian-Maastrichtian晚期)的古柏列尼特连续浮游有孔虫的分类学修订显示,该组由两个属组成,古柏瑞娜·基科伊内(Gublerina Kikoiene)1948年和古柏瑞娜(Praegublerina gen)。十一月,这是从精细的双齿双异种Heterohelixplanata(Cushman 1938)演变而来。 Praegublerina中有3种:P。pseudotessera(Cushman 1938),P。acuta(de Klasz 1953)和P.robasta(de Klasz 1953),第一个是该属的最老,是Heterohelix planata的后代(Cushman 1938) )。 Gublerina cuvillieri Kikoine 1948和G. rajagopalani Govindan 1972被保留在Gublerina内。可以根据总体测试架构,测试装饰,孔径和内部测试形态来识别这两个谱系。我们的研究揭示了在血统之间存在进化连续体的情况,其中在古布雷利那和普拉古布雷里那独立地发展了古勃氏蛋白型腔增殖。新的分类学框架反映了浮游有孔虫进化的迭代模式,并且可以更好地了解古柏林类生物群的地层和地理分布。与共同出现的马斯特里赫特底栖和浮游物种同时发生的罗汉果G. cuvillieri和稳定的同位素比较表明,两种古布利特里娜物种在温跃层附近共有相同深度的栖息地。

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