Oligocene-Pliocene taxonomy and stratigraphy of the genus Sphenolithus in the circum North Atlantic Basin: Gulf of Mexico and ODP Leg 154.

J. Bergen, E. de Kaenel, S. A. Blair, T. Boesiger, E. Browning
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引用次数: 22

Abstract

Sphenolithus is secondary only to the genusDiscoaster in Cenozoic nannofossil biostratigraphy, notably of primary importance for the Oligocene to Early Miocene. The research presented herein provides a framework for Oligocene to Middle Pliocene Sphenolithus, where gradations between individual taxa and their stratigraphic ranges are presented. Integration of schemes from BP, Amoco and Arco Vastar, to form a single composite Neogene calcareous nannofossil framework for the Gulf of Mexico basin, began around the turn of the century with focus on refining taxonomic concepts to solve stratigraphic discrepancies between the heritage schemes. Further study and bioevent calibration was accomplished through analyses of deep-water wells in the Gulf of Mexico along with research grounding the integrated framework to the “astronomical clock” of ODP Leg 154 back into the middle Early Oligocene at an average sample resolution of 21 kyr. Forty-two species are considered herein, in addition to the morphologically-similar Ilselithina fusa. Thirteen new species are introduced. Sphenolithus peartiae and Sphenolithus distentus are emended. Clarification of taxonomic concepts by the use of morphologic groups is supplemented with identification tables, drawings, and light photomicrographs. Iterative processes, in terms of size, are stressed.
北大西洋盆地环缘蝶石属的渐新世-上新世分类和地层学:墨西哥湾和ODP Leg 154。
Sphenolithus在新生代纳米化石生物地层学中仅次于disaster属,在渐新世至早中新世具有重要意义。本文的研究为渐新世至中上新世的蝶石群提供了一个框架,其中个别分类群及其地层范围之间存在等级关系。整合BP、Amoco和Arco Vastar的方案,形成墨西哥湾盆地单一的复合新近系钙质纳米化石框架,始于世纪之交,重点是完善分类概念,以解决遗产方案之间的地层差异。进一步的研究和生物事件校准是通过对墨西哥湾深水井的分析完成的,同时研究将ODP Leg 154的“天文钟”集成框架建立在早渐新世中期,平均样品分辨率为21 kyr。这里考虑了42种,除了形态相似的Ilselithina fusa。引进了13个新物种。修订了泛凤梨和大凤梨。通过使用形态学组来澄清分类概念,并辅以识别表、图纸和光学显微照片。就规模而言,强调迭代过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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