CHRONOSTRATIGRAPHIC FRAMEWORK OF THE EXTERNAL LIGURIAN UNITS (LATE CRETACEOUS, NORTHERN APENNINES, ITALY) BASED ON CALCAREOUS NANNOFOSSILS

IF 1.2 4区 地球科学 Q2 GEOLOGY
Ofioliti Pub Date : 2011-01-03 DOI:10.4454/OFIOLITI.V36.I1.2
R. Catanzariti, N. Perilli
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引用次数: 4

Abstract

The study of calcareous nannofossil assemblages recovered from the External Ligurian Units allows us (1) to reconstruct the distribution patterns of selected Late Cretaceous taxa; (2) to identify the biohorizons helpful in recognizing and characterizing the standard zones of Sissingh (1977); some of which have been grouped; and (3) to propose a synthesis of the ages achieved until now for the External Ligurian Units. According to the available dataset; rooted on published and unpublished data; the here proposed biostratigraphic scheme is based on 24 age-indicative taxa and 16 first occurrences; and its biostratigraphic resolution is comparable with the resolution of the scheme of Sissingh (1977); only considering FOs. Calcareous nannofossils are hence a fossil group useful to furnish a new and more complete chronostratigraphic framework of the main External Ligurian Units; helpful to better constrain the tectono-sedimentary and the geodynamic evolution of the Western Tethys Domain.
基于钙质纳米化石的外利古里亚单元(晚白垩世,意大利亚平宁山脉北部)年代地层格架
通过对外利古里亚单元钙质纳米化石组合的研究,我们(1)重建了选定的晚白垩世分类群的分布格局;(2)确定有助于识别和描述Sissingh标准带的生物层位(1977);其中一些已经分组;(3)综合迄今为止所取得的外部利古里亚单位的年龄。根据现有数据集;基于已发表和未发表的数据;本文提出的生物地层方案基于24个指示年龄的分类群和16个首次地;其生物地层分辨率与Sissingh(1977)方案的分辨率相当;只考虑FOs。因此,钙质纳米化石是一个化石群,有助于提供一个新的、更完整的外利古里亚主要单元的年代地层格架;有助于更好地约束西特提斯域的构造-沉积和地球动力学演化。
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来源期刊
Ofioliti
Ofioliti 地学-地质学
CiteScore
2.40
自引率
7.70%
发文量
1
期刊介绍: Since 1976, Ofioliti provides an international forum for original contributions and reviews in the field of the geodynamics, petrology, geochemistry, biostratigraphy, stratigraphy, tectonics and paleogeography applied to ophiolitic terrains and modern oceanic lithosphere, including their sedimentary cover. Studies of topics such as geodynamics of the mantle, the evolution of orogens including ophiolites and paleoceanography are also welcome
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