Eocene gastropods of the New Forest, UK

Geology Today Pub Date : 2025-01-24 DOI:10.1111/gto.12503
James Barnet
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Abstract

Gastropods expanded into niches vacated by both terrestrial and marine organisms following the end-Cretaceous mass extinction, to become one of the dominant mollusc groups of the Cenozoic. The Selsey Formation of Eocene age was deposited within a shallow marine embayment across the Hampshire Basin (southern England) and contains a particularly diverse gastropod assemblage, forming the surface geology across the northern part of the New Forest National Park. Here, I use closely related gastropod species alive in the seas today to offer insights into the lifestyles and habitats of extinct Eocene species. By integrating this with other geological evidence, including gastropod preservation and other associated fossils, I paint a picture of the climate and environment on the New Forest seafloor during the Eocene epoch.

Abstract Image

英国新森林始新世腹足动物
在白垩纪末期大灭绝之后,腹足类动物扩展到陆生和海洋生物空出的生态位,成为新生代软体动物的主要群体之一。始新世时代的塞尔西组沉积在横跨汉普郡盆地(英格兰南部)的浅海海湾内,包含特别多样化的腹足类动物组合,形成了横跨新森林国家公园北部的地表地质。在这里,我用现在生活在海洋中的腹足类动物来深入了解灭绝的始新世物种的生活方式和栖息地。通过结合其他地质证据,包括腹足动物的保存和其他相关化石,我描绘了一幅始新世时期新森林海底气候和环境的图景。
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CiteScore
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