Biotic Response to Paleoenvironmental Change in the Ediacaran and Early Cenozoic
The effects of changes to environments on Earth in the past have been well documented, and we have fossil evidence of how organisms responded to these changes. In the past, possible responses to environmental change have ranged from extinction and origination to migration to physical morphological c...
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| Other Authors: | , |
| Format: | Thesis |
| Language: | English |
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eScholarship, University of California
2019
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| Online Access: | https://escholarship.org/uc/item/29402215 https://escholarship.org/content/qt29402215/qt29402215.pdf |
| Summary: | The effects of changes to environments on Earth in the past have been well documented, and we have fossil evidence of how organisms responded to these changes. In the past, possible responses to environmental change have ranged from extinction and origination to migration to physical morphological changes. As we are currently facing the prospect of dramatic alterations to Earth’s environments, understanding how life responded in the past may be one of our best opportunities to gauge how future scenarios might play out.Here I present new data detailing how two different groups of organisms were living in fluctuating environments at two times in Earth’s history. During the Ediacaran there was a unique subset of organisms with three-fold symmetry that went extinct before the beginning of the Cambrian. Although they were relatively abundant and diverse, representing ~12-15% of the taxonomic diversity of the second (White Sea) Ediacaran assemblage, no animals at any point afterwards have had tri-radially symmetric body plans. I show that most of these tri-radial taxa share many morphological and ecological similarities beyond their distinctive body plan and were likely related members of a tri-radial clade. Furthermore, there is evidence that multiple tri-radial taxa were generalists, able to survive in a wide variety of environments, indicating that a relatively sharp environmental change would have been necessary to eliminate this group. An almost opposite scenario is true for deep-sea ostracodes during Eocene Thermal Maximum 2 (ETM2) in the equatorial and North Atlantic. Using high-resolution sampling from ocean drill cores (ODP Site 1258 and IODP Site U1409) I show that, although this was a relatively smaller event than the preceding Paleocene-Eocene Thermal Maximum, ostracodes respond in noticeable ways. Ostracode diversity and abundance (as measured by accumulation rate) remain low throughout the duration of ETM2. Additionally, the dominant species in these cores exhibit a size decrease that is also correlated ... |
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