EPROAMA · Environmental changes and global recovery of primary producers after the Cretaceous/Paleogene boundary (KPgB): A molecular fossil approach
Horizon 2020 — Marie Skłodowska-Curie Actions
- Duration
- 2022-01-01 → 2023-12-31
- EU contribution
- €224,934
- Participants
- 1
- Scheme
- MSCA-IF
Lines connect the coordinator with its partners.
Results in brief
Environmental changes and global recovery of primary producers after the Cretaceous/Paleogene boundary (KPgB): A molecular fossil approach
I used this fellowship to study the environmental changes and global recovery of primary producers after the Cretaceous/Paleogene boundary (K-Pg): A molecular fossil approach (EPROAMA). This fellowship was carried out at the University of Bristol (UoB-UK) under the supervision of Prof. Richard D. Pancost. The K-Pg (≈66.02 Ma ago). It represents the last of the five major mass extinctions in Earth´s history. Determining the nature of the associated rapid environmental change and biotic recovery is critical for understanding the cause and effects of this event, a key event in the history of life on our planet and potentially relevant for future biotic events. My results show, the non-fossilising phytoplankton community was impacted at K-Pg event, as was reflected in the source and character of organic matter reached the seafloor. But in addition, the recovery time of this community (algae, bacteria, and archaea.) was very different depended to the distant to the impact site (distal and proximal sections). 1 Objectives My EPROAMA proposal had the following specific research objectives, which were cut across 5 work packages (WP1-WP5): 1. Determine changes in algal organic matter (OM) inputs and their timing relative to the ejecta release and anoxia across the KPg section (Caracava) (WP3 and WP4). 2. Determine how long it took for pre-event distributions and conditions to return (WP3 and WP4). 3. Determine the carbon isotopic composition of n-alkanes (inferred to derive from leaf waxes), yielding one of the first and highest resolution terrestrial (atmospheric) records of carbon cycle disruption (WP4). 2. Explanation of the work carried per WP -WP1: Management. Deliverables (D1.1 and D.1.2) were performed. -WP2: Field work for sampling the Caravaca section from K-Pg. Deliverable D.2.1 was performed and a core from Caravaca section was recovery, but in addition, we also made another fieldtrip to take samples from other two outcrops located in USA. The Risk Management RM1 projected wasn't happened and the Milestone M1 was obtained perfectly. -WP3: Analysis of organic compounds from K-Pg in the Caravaca section. Deliverable D.3.1 was performed and all extraction and analyses from Caravaca samples were finished. In addition, we also analyzed the samples from the others USA K-Pg sections. The Risks Management RM2 and RM3 projected weren't happened and the Milestone M3 was performed. I wrote 3 papers, 1 was published and 2 are under revision. -WP4: Analysis of carbon isotopic composition of n-alkanes from Caravaca section. Deliverable D.4.1 was performed and all stable carbon isotopic composition on n-alkanes from Caravaca section and USA section were finished. The Risks Management RM2 and RM3 projected weren't happened and the Milestone M4 was in progress, I am writing 2 papers more. -WP5: Disseminations and communications. Deliverables D.5.1, D.5.2, D.5.5 D.5.6, D.5.7 and D5.8 were performed. D.5.3 I am working on it, I bought the dominion, and I am working in the design and content of the webpage, and D.5.4 wasn´t performed for technical problems. All lab work was carried out in the Organic Geochemistry Unit (OGU), based within the Schools of Earth Science and Chemistry at the UoB-UK,
Data: CORDIS, © European Union
Project objective
The mass extinction marking the Cretaceous/Palaeogene boundary (KPgB), 66.02 million years ago. It was one of the most devastating events in the history of life, as well as the most recent and best studied of the ‘big five’ mass extinctions that occurred during the Phanerozoic. After decades of research, one of the most critical lines of inquiry is understanding the short- to long-term effects of this impact on the global environmental system, including the re-establishment of pre-impact environmental conditions and marine biological productivity. After characterizing how the recovery of palaeoenvironmental conditions were by the analysis of inorganic geochemical proxies, critical questions were raised about the nature of and recovery after the event. how did primary productivity and the biological pump change and how did that impact the source and character of organic matter reaching the seafloor? And crucially, how did these interlinked processes recover after the impact event? The Caravaca section is amongst the most continuous, well-preserved, and well-studied KPgB distal sections in the world. This allows these questions to be explored using molecular fossils (or biomarkers) – for the first time in this section and consequently at unprecedented stratigraphic resolution. The approach will broadly encompass several methods, all of which will be carried out in the OGU (Organic Geochemistry Unit) at Bristol University. These will include but are not limited to, the determination of total organic carbon (TOC) contents; the extract and analysis of the biomarkers from ground samples; the determination of key biomarker abundances and distributions by GC and GC-MS in order to ascertain changes in organic matter (OM) source, algal assemblages, terrestrial biomarkers, redox state (pristane/phytane ratio; homohopane index) and microbial inputs (hopanes); and finally, to explore changes in ‘apparent thermal maturity’ which could reflect changes in reoworked OM input.
Original text from CORDIS.
Participants
- UNIVERSITY OF BRISTOL · BRISTOLCoordinatorUnited Kingdom
Links
Data: CORDIS, © European Union
