High-diversity larger foraminiferal assemblages calibrated with calcareous nannoplankton biozones in the aftermath of EECO (Collio, Friuli-Venezia Giulia, northeastern Italy)

IF 1.7 3区 地球科学 Q2 PALEONTOLOGY Palaeoworld Pub Date : 2024-04-01 DOI:10.1016/j.palwor.2023.01.013
Andrea Benedetti , Cesare Andrea Papazzoni , Francesca Bosellini , Luca Giusberti , Eliana Fornaciari
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Abstract

The Eocene of Collio (easternmost Friuli-Venezia Giulia, northeastern Italy) contains rich larger foraminiferal assemblages mainly dominated by nummulitids of genera Nummulites and Assilina. Herein, we document, by typological and biometric approaches, upper Ypresian to lower Lutetian taxa, dated by an integrated biostratigraphy combining the Shallow Benthic Zones (SBZ) with the nannofossil biozones. A total of seven species of Alveolina, 12 species of Assilina and 33 of Nummulites are described (in Appendix A), some of them left in open nomenclature. The larger foraminiferal assemblages indicate that all the collected samples are assignable to SBZ12 and SBZ13 and their high diversity suggests high resilience of these shallow-water taxa after the Early Eocene Climate Optimum warming event. The occurrence of the calcareous nannofossil Blackites inflatus together with Alveolina violae Nummulites friulanus, N. campesinus, N. quasilaevigatus, Assilina maior maior and A. cuvillieri, typical SBZ12 markers, suggests that SBZ12 extends at least to the basal Lutetian, thus the SBZ12/13 boundary occurs in the lowermost Lutetian instead of at the Ypresian/Lutetian transition.

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EECO后高多样性大型有孔虫组合与钙质纳米浮游生物带校准(科利奥,弗鲁利-威尼斯朱利亚,意大利东北部)
科利奥(意大利东北部弗留利-威尼斯朱利亚省最东端)始新世包含丰富的大型有孔虫集合体,主要以Nummulites和Assilina属的有孔虫为主。在这里,我们通过类型学和生物计量学方法记录了上伊普雷期至下卢特泰期的类群,并通过浅海底带(SBZ)与化石生物带相结合的综合生物地层学进行了年代测定。共描述了 7 个 Alveolina 种类、12 个 Assilina 种类和 33 个 Nummulites 种类(见附录 A),其中一些种类的命名尚未确定。较大的有孔虫集合体表明,所有采集到的样本都可归入 SBZ12 和 SBZ13,其较高的多样性表明这些浅水类群在早始新世气候最适变暖事件后具有较强的恢复能力。钙质化石 Blackites inflatus 与 Alveolina violae Nummulites friulanus、N. campesinus、N. quasilaevigatus、Assilina maior maior 和 A. cuvillieri(典型的 SBZ12 标记)一起出现,表明 SBZ12 至少延伸到了下部的卢特陶统,因此 SBZ12/13 边界出现在最下部的卢特陶统,而不是在伊普雷先/卢特陶过渡带。
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来源期刊
Palaeoworld
Palaeoworld PALEONTOLOGY-
CiteScore
4.00
自引率
5.90%
发文量
95
期刊介绍: Palaeoworld is a peer-reviewed quarterly journal dedicated to the study of past life and its environment. We encourage submission of original manuscripts on all aspects of palaeontology and stratigraphy, comparisons of regional and global data in time and space, and results generated by interdisciplinary investigations in related fields. Some issues will be devoted entirely to a special theme whereas others will be composed of contributed articles. Palaeoworld is dedicated to serving a broad spectrum of geoscientists and palaeobiologists as well as serving as a resource for students in fields as diverse as palaeobiology, evolutionary biology, taxonomy and phylogeny, geobiology, historical geology, and palaeoenvironment. Palaeoworld publishes original articles in the following areas: •Phylogeny and taxonomic studies of all fossil groups •Biostratigraphy, chemostratigraphy, chronostratigraphy •Palaeoecology, palaeoenvironment and global changes throughout Earth history •Tempo and mode of biological evolution •Biological events in Earth history (e.g., extinctions, radiations) •Ecosystem evolution •Geobiology and molecular palaeobiology •Palaeontological and stratigraphic methods •Interdisciplinary studies focusing on fossils and strata
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