School of Earth & Environmental Sciences
Earth Sciences at St Andrews dates to the 17th Century, a rich tradition that shapes our vision for the future: to define the cutting edge of Earth, environmental, and planetary science, and deliver unparalleled student education.
Our research is both curiosity driven, addressing profound questions about the co-evolution of Earth and life, and applied, delivering societal and economic impact. It spans recent environmental change to planetary formation, underpinned by state-of-the-art analytical and field capabilities.
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Geology and geochronology of the Tana Basin, Ethiopia : LIP volcanism, super eruptions and Eocene-Oligocene environmental change (2016-06-01) - Journal articleNew geological and geochronological data define four episodes of volcanism for the Lake Tana region in the northern Ethiopian portion of the Afro–Arabian Large Igneous Province (LIP): pre-31 Ma flood basalt that yielded a ...
Hydrologic indicators of hot spots and hot moments of mercury methylation potential along river corridors (2016-10-15) - Journal articleThe biogeochemical cycling of metals and other contaminants in river-floodplain corridors is controlled by microbial activity responding to dynamic redox conditions. Riverine flooding thus has the potential to affect ...
Response of deep subsurface microbial community to different carbon sources and electron acceptors during ∼2 months incubation in microcosms (2017-02-20) - Journal articleAcetate plays a key role as electron donor and acceptor and serves as carbon source in oligotrophic deep subsurface. It can be produced from inorganic carbon by acetogenic microbes or through breakdown of more complex ...
The DeepMIP contribution to PMIP4 : experimental design for model simulations of the EECO, PETM, and pre-PETM (version 1.0) (2017-02-23) - Journal articlePast warm periods provide an opportunity to evaluate climate models under extreme forcing scenarios, in particular high (> 800ppmv) atmospheric CO2 concentrations. Although a post hoc intercomparison of Eocene (∼ 50 Ma) ...
A record of Neogene seawater δ11B reconstructed from paired δ11B analyses on benthic and planktic foraminifera (2017-02-24) - Journal articleThe boron isotope composition (δ11B) of foraminiferal calcite reflects the pH and the boron isotope composition of the seawater the foraminifer grew in. For pH reconstructions, the δ11B of seawater must therefore be known, ...