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Deconvolving the early record of eukaryotic evolution

Project description

Understand evolutionary changes by analysing ancient rocks

The Neoproterozoic Era (1 to 0.54 billion years ago) was a time of ecological and evolutionary transformations, leading to the emergence of animals after nearly 4 billion years of bacterial dominance. This period was marked by environmental disturbances, which are reflected in sedimentary rocks. However, the exact nature and impact of these disturbances remain poorly understood. The ERC-funded DNE project will develop methodologies that combine organic geochemistry, isotope geochemistry, and palaeontology to analyse ancient rocks. The project seeks to enhance our understanding of the carbon cycle in ancient habitats. Additionally, it will help identify the organisms from this era, providing valuable insights into the ecosystems that existed prior to the rise of animal life.

Objective

The Neoproterozoic Era (1 to 0.54 billion years ago) witnessed some of the most dramatic ecological and evolutionary changes in Earth history, which culminated in the appearance and diversification of animals. After almost 4 billion years of bacterial dominance, it took life on our planet just ~250 million years to go from the proliferation of unicellular eukaryotes to diversification of animals. This sequence of rapid ecological and evolutionary changes is thought to be related to unprecedented environmental perturbations, which occurred during this time interval and are recorded in sedimentary rocks. We know these perturbations did happen, but not their magnitude, duration, or driving mechanisms. One of the major limitations of interpreting the data is that each sample represents tens, or even hundreds of years of sedimentation, and contains a mixture of unevenly preserved remains of organisms that lived throughout this time. This project focuses on new methodological approaches at the interface of organic geochemistry, isotope geochemistry, and palaeontology to deconvolve the mixed signals of ancient rocks. Stable carbon isotope analysis on biomarkers of specific groups of organisms would provide insights about the carbon cycle at their habitat; analysing biomarker composition of the first complex microfossils would allow to identify which organisms they were; position-specific isotopic composition of ancient biomarkers might reveal their biosynthetic pathway and thus identify the first ecologically successful eukaryotes on our planet. The study is designed to extract information about the composition and ecology of ancient ecosystems, as well as the history of carbon cycle throughout the critical time of the rise and diversification of complex life. It aims to resolve what it takes a habitable planet to evolve complex life, and, in turn, how life on our planet responded to possibly the largest perturbations in the global carbon cycle in the Earth history.

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Host institution

UNIVERSITAET BREMEN
Net EU contribution

Net EU financial contribution. The sum of money that the participant receives, deducted by the EU contribution to its linked third party. It considers the distribution of the EU financial contribution between direct beneficiaries of the project and other types of participants, like third-party participants.

€ 1 859 131,00
Address
Bibliothekstrasse 1
28359 Bremen
Germany

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Region
Bremen Bremen Bremen, Kreisfreie Stadt
Activity type
Higher or Secondary Education Establishments
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Total cost

The total costs incurred by this organisation to participate in the project, including direct and indirect costs. This amount is a subset of the overall project budget.

€ 1 859 131,00

Beneficiaries (2)

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