New larger benthic foraminifera from the subsurface Lower to Middle Eocene Oldsmar Formation of southeastern Florida (USA)

IF 1.5 4区 地球科学 Q2 GEOLOGY
E. Robinson, K. Cunningham
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引用次数: 0

Abstract

We describe two larger benthic foraminiferal taxa collected from wells drilled in the subsurface Eocene rocks of southeastern Florida that are new to peninsular Florida and the Caribbean region. Saudia floridana n.sp. is characteristic of a foraminiferal assemblage, along with Helicostegina gyralis, wide forms of the Cushmania americana group, and Gunteria floridana, in an upper part of the Oldsmar Formation. Globogypsinoides browardensis n.gen. n.sp. occurs in a second foraminiferal assemblage, along with Borelis cf. floridanus, Coskinolina cf. yucatanensis, and as-yet undescribed large rotaliids, in a middle part of the Oldsmar Formation. The foraminiferal assemblage of the middle Oldsmar unit is ascribed an Ypresian age and the assemblage of the upper Oldsmar unit a Lutetian age. These two assemblages indicate inner shelf water depths of 40 m or less on the Florida Platform during the Early to Middle Eocene deposition of the middle to upper part of the Oldsmar Formation.
美国佛罗里达东南部下始新世至中始新世Oldsmar组地下新的大型底栖有孔虫
我们描述了两个较大的底栖有孔虫分类群,这些分类群是从佛罗里达东南部始新世地下岩石中钻探的井中收集的,它们是佛罗里达半岛和加勒比地区的新物种。佛罗里达州的沙特阿拉伯是一个有孔虫组合的特征,与美国库什马尼亚群的广泛形式的Helicostegina gyralis和佛罗里达的Gunteria一起,在Oldsmar组的上部。天牛属植物。n.sp。与Borelis cf. floridanus, Coskinolina cf. yucatanensis和尚未描述的大型轮虫一起出现在Oldsmar组中部的第二个有孔虫组合中。中奥德斯玛单元的有孔虫组合属于伊普西时代,上奥德斯玛单元的有孔虫组合属于鲁特梯时代。这两个组合表明,在Oldsmar组中上段早始新世至中始新世沉积时期,佛罗里达台地的内陆架水深不超过40 m。
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来源期刊
Carnets De Geologie
Carnets De Geologie Earth and Planetary Sciences-Geology
CiteScore
2.90
自引率
14.30%
发文量
21
审稿时长
>12 weeks
期刊介绍: Information not localized
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