Collaborative Research: Was There a Shift Toward Small, Non-Fossilizing Plankton after the End of the Cretaceous Mass Extinction?

浮游植物生活在海洋表面，利用阳光和二氧化碳产生有机物质。这种初级生产构成了大多数海洋食物网的基础，是全球碳循环的关键部分。在现代海洋中，浮游生物正在受到变暖和海洋酸化的影响。过去地质学中海洋温度和化学的自然变化可以帮助我们了解诸如变暖和酸化等压力因素的长期影响。大约6600万年前的古近纪（K-Pg）大灭绝事件就是这样一个全球变化时期。钙质（化石形成）微型浮游生物是白垩纪海洋中占主导地位的初级生产者之一。然而，这一组的93%的物种在K-Pg边界灭绝，它们再也没有占主导地位。以往关于浮游生物对K-Pg事件反应的研究一般仅限于对留下物理化石记录的物种的研究。因此，这些研究只提供了古代浮游生物生态系统的部分观点。拟议中的工作将通过使用称为生物标志物的化学化石来克服这一限制。这些新数据将与传统的物理化石一起用于重建K-Pg事件后海洋浮游生物群落的变化。人们通常认为，非浮游植物填补了钙质微型浮游生物减少留下的差距。这项研究将有助于验证这一假设。记录非浮游生物和浮游生物的变化将提高我们对浮游生物生态长期变化的理解，以及这些变化如何改变海洋碳循环。该项目将培训早期职业研究人员和本科生，并将通过与德克萨斯州奥斯汀和科罗拉多州博尔德的组织和计划合作开展的推广和教育活动向更广泛的受众传播结果。该项目将开发来自突尼斯，西班牙和美国墨西哥湾沿岸5个地点的脂质生物标志物，钙质浮游生物和浮游有孔虫的数据集。突尼斯的三个地点（El Kef、Elles和El Melah）代表大陆架上的一个深度断面（古深度为200 - 500 m），Caravaca代表更深的水（~600 - 1000 m），而Brazos代表一个浅水架，这将使我们能够测试北非和美国海湾沿海平原之间的区域变化。这些数据将允许测试以下假设：1。在K-Pg大灭绝之后，在低多样性的钙质微型浮游生物"灾难"组合期间，一个低多样性的非浮游植物组合出现了水华.钙质微型浮游生物多样性的恢复与非浮游植物的减少有关。异养浮游有孔虫组合的变化与整个自养浮游生物组合的周转有关。大灭绝后的初级生产者群落主要由藻类和蓝藻等较小的浮游植物组成，这将增加浅水沃茨的碳循环，减少向深海的碳输出。这项研究将提高我们对白垩纪末大灭绝后恢复的理解，并全面了解浮游生物生态在海洋生态系统变化中的作用。此外，重建整个浮游生物生态系统，而不仅仅是浮游生物的部分，将代表着我们研究古代海洋的工具箱的重大改进。该奖项反映了NSF的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。

Phytoplankton, which live in the surface ocean, produce organic matter from sunlight and carbon dioxide. This primary production forms the base of most marine food webs and is a critical part of the global carbon cycle. In the modern ocean plankton are being impacted by warming and ocean acidification. Natural changes in ocean temperature and chemistry in the geologic past can help us understand the long-term effects of stressors such as warming and acidification. The Cretaceous-Paleogene (K-Pg) mass extinction event ~66 million years ago was one such time of global change. Calcareous (fossil-forming) nanoplankton were one of the dominant primary producers in the Cretaceous ocean. However, 93% of species of this group went extinct at the K-Pg boundary, and they were never again as dominant. Previous studies of the plankton response to the K-Pg event have generally been limited to studies of species which leave a physical fossil record. Thus, these studies provided only a partial view of ancient plankton ecosystems. The proposed work will overcome this limitation by using chemical fossils called biomarkers. These new data will be used together with traditional physical fossils to reconstruct changes in the marine plankton community following the K-Pg event. It has often been assumed that non-fossilizing phytoplankton filled the gap left by the decline in calcareous nannoplankton. This study will help test that hypothesis. Documenting the changes in both non-fossilizing and fossilizing plankton will improve our understanding of long-term changes in plankton ecology, and of how those changes could alter the ocean carbon cycle. This project will train early career researchers and undergraduate students, and will disseminate results to broader audiences through outreach and educational activities in partnership with organizations and programs in Austin, TX and Boulder, CO.The project will develop datasets of lipid biomarkers, calcareous nannoplankton, and planktic foraminifera from 5 sites in Tunisia, Spain, and the US Gulf Coast. Three sites in Tunisia (El Kef, Elles, and El Melah) represent a depth transect on a continental shelf (paleodepths of 200-500 m), Caravaca represents deeper water (~600-1000 m), while Brazos represent a shallow shelf which will allow us to test regional variability between north Africa and the US Gulf Coastal Plain. These data will allow tests of the following hypotheses:1. A low-diversity assemblage of non-fossilizing phytoplankton bloomed in the aftermath of the K-Pg extinction, during the time of low diversity calcareous nannoplankton “disaster” assemblages.2. Subsequent recovery of calcareous nannoplankton diversity is associated with a decline in non-fossilizing phytoplankton.3. Shifts in the heterotrophic planktic foraminifera assemblages are tied to turnover in the whole autotrophic plankton assemblage.4. The post-extinction community of primary producers was dominated by smaller phytoplankton like algae and cyanobacteria, and would have increased carbon recycling in shallow waters and reduced carbon export to the deep sea.The study will improve our understanding of the recovery after the end Cretaceous mass extinction and in our overall understanding of the role of plankton ecology in marine ecosystem change. Additionally, reconstructing the whole plankton ecosystem, and not just the part that fossilizes, would represent a significant improvement of our toolkit to investigate ancient oceans.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.