Research Projects

Photos from left to right: (1) Students taking sediment push cores through a bog in Denmark, (2) picking forams from deep sea sediment cores on a research cruise, (3) studying cross-bedding in the Entrada Sandstone, Arches national park. (4) Multi-collector ICP mass spectrometer used for measurements of Ca and Mg isotopes.

The Earth history team is and interdisciplinary research group that spans fields of geochemistry, geobiology, field geology, and computational modeling. We are particularly interested in the co-evolution of climate and life across Earth history, from >3 billions years ago until today.

The Boring Billion

Photos from left to right: (1) Waterton Lakes National Park (2) Team photo (field season summer 2025) (3) Molar Tooth structure in Siyeh Formation carbonates (4) Overview over Waterton Lake

At the beginning of the Mesoproterozoic Era, 1600 million years ago, Canada was connected to Australia, forming part of the supercontinent Columbia. Around 1400 millon years ago, Columbia started to break apart, creating deep intracontinental rifts where isolated ocean basins formed. Today, the sediments that were deposited in these ancient basins make up the rocks of the Belt-Purcell Supergroup in British Columbia (Canada) and Montana (USA), and the McArthur Basin in Australia. It is not a coincident that these now far-apart areas are host to some of the world’s most productive ore-bearing sedimentary deposits. The ore fluids that created these base metal seafloor deposits were a product of the paleo-environmental conditions during the initial rifting of Columbia. Hot climatic conditions produced an evaporitic environment and lead to the formation of highly saline brines. Thermal convection drove the circulation of these brines through the sediment-pile, leaching and concentrating metals, and forming both veins and stratabound disseminated sulphide deposits with high concentrations of trace metals, such as Cu, Co, and Zn. The unique marine environments that developed during the initial rifting of Columbia hosted some of the earliest eukaryotic life on Earth. For example, eukaryotic micro-fossils have been found in the Greyson Formation (~1460 Ma), in the Belt-Purcell Supergroup, Montana.

In the Earth History group we research the relationship between the evolution of eukaryotic life on Earth and the availability of bio-essential trace metals in these unique rift-basins. We apply novel geochemical tools to estimate the degree of post-depositional alteration and circulation of ore-bearing fluids. These geochemical tools include (1) Rb-Sr dating of clay minerals within shale dominated sediments, (2) measurements of Mg, Ca, and Sr isotopes in carbonate dominated sediments, (3) measurements of bio-essential trace elements such Cu, Zn, Mo, V, and Co, (4) numerical modelling of fluid-flow and quantification of alteration, (5) collection of macro- and microfossils, biomarkers, and evaluating organic matter maturity.

This research project is co-funded by the Australian Research Council and NSERC Alliance International Collaboration.

Carbonate diagenesis

For geochemists and Earth historians alike diagenesis is often regarded as a problem to be avoided. Diagenetic processes add complexity to the geochemical signals and in the worst case can obliterate the primary environmental information. Instead of attempting to avoid diagenesis, our research seeks to extract the primary chemical information from ancient carbonate sediments by better understanding the diagenetic processes. Diagenetic reactions involve fluids in the subsurface and the amount of fluid flow determines the extent to which diagenesis alters or preserves the original geochemical signals (fluid- and sediment-buffered diagenesis). We have developed a numerical model that simulates these reactions between carbonate and pore-fluids along a flow path (Ahm et al., 2018). The model has been ground-truthed against measurements of calcium and magnesium isotopes from modern to Neogene carbonate sediments in the Bahamas. By quantifying the style and extent of early marine diagenesis (fluid- versus sediment-buffered), this model can explain much of the stratigraphic and lateral variability observed in the chemistry of Neogene shallow-water carbonate sediments and extract the chemical composition of contemporaneous seawater. When applied to ancient carbonate sediments, the model can be used to 'see through' diagenesis and more accurately reconstruct records of past seawater chemistry.

Ongoing research involve integrating additional geochemical proxies into the model framework and seek to generate complementary datasets (e.g., for Li and S isotopes see Murphy et al., 2021 and Bryant et al., 2022, respectively):

Photos from left to right: (1) The Buah Formation in Oman containing the Shuram carbon isotope excursion. (2) The Hadash cap carbonate in Oman, overlying snowball Earth deposits. (3) The Noonday cap carbonate in Death Valley, overlying snowball Earth deposits. (4) View over outcrop in the Panamints Range, Death Valley.

Neoproterozoic carbon isotope excursions

The variability in carbon isotope values from Neoproterozoic platform carbonates exceeds that of the Cenozoic deep sea record by almost an order of magnitude. The Neoproterozoic record is characterized by high baseline values +5-10‰ that are interrupted by dramatic negative excursions with values down to -15‰. The origins of the Neoproterozoic carbon isotope excursions are still widely debated, because δ13C values below -5‰ can not be explained by a traditional steady state carbon cycle model. A continued research effort in the Earth history group is investigating the link between the local depositional environment and diagenetic history of these Neoproterozoic carbonates. In addition to constraining the effects from diagenesis, we attempt to disentangle the influence of primary variabilities in local surface-waters chemistry on stratigraphic records from platform carbonates. Local effects are important to consider because observation from modern shallow-water depositional systems have shown that local carbon cycling and diagenesis largely controls the carbon isotope values of platform carbonates. Research in the group, and with collaborators, spans several Neoproterzoic carbon isotope excursions such as the Precambrian-Cambrian boundary, the Ediacaran Shuram excursion, the snowball Earth cap carbonates, the Trezona excursion, the Taishir excursion, and the Islay excursion.

Group and collaboration papers on Neoproterozoic carbon isotope excursions:

Photos from left to right: (1) Aragonite fans from ~2.8 billion year old carbonates from the Steep Rock Formation. (2) Stromatolites from the Steep Rock Formation. (3) The old Steep Rock mine, exposing Archean carbonate and banded iron formation. (4) Field work in northern Ontario involves dealing with rainy weather and lush vegetation.

The origins of life and the Great Oxidation Event

Throughout the history of our planet, Earth's surface has gone through critical transitions. Perhaps most dramatic is the evolution of oxygenic photosynthesis and the rise of atmospheric oxygen more than 2.3 billion years ago (the Great Oxidation Event). This event is expected to have caused major changes in the global carbon cycle, which may be recorded by the composition of stable carbon isotopes in carbonate rocks. However, ancient carbonate sediments deposited before the Great Oxidation Event have baseline carbon isotope values of approximately 0‰ - broadly similar to baseline values recorded in Phanerozoic! This observation challenges our understanding of how sediments record and preserve signals of the global carbon cycle. It is likely that the carbon cycle on early Earth was significantly different from the modern and included fluxes that may not exist on Earth today. Moreover, only a fraction of ancient carbonate sediments is preserved in the geologic record due to the continuous recycling of ocean crust through the forces of plate tectonics. The chemistry of sediment may also be altered during the transformation of primary sediment into rocks (diagenesis). As a result, it is possible that the chemistry of the ancient carbonate sediments is not telling us a true story of the ancient carbon cycle. Ongoing research in the Earth history group includes using calcium and magnesium isotope measurements from Archean carbonates to better understand the carbon cycle on early Earth.

This project is funded by the Simons Foundation Collaboration on the Origins of Life and NSERC Discovery.

Group and collaboration papers on the Great Oxidation Event:

Also, check out this new presentation by Daniel Garduno Ruiz on modelling atmospheric oxygen and the GOE: Youtube Link

Kinetic effects on seawater carbonate chemistry

Shallow marine carbonate sediments are deposited in shallow restricted environments where the chemistry of the surface waters are significantly offset from the chemistry of the open ocean. As a result, it is difficult to directly link the geochemistry of ancient platform sediments with changes in global geochemical cycles. In the Earth history group, we explore how air-sea gas exchange of carbon dioxide may affect surface water chemistry and the carbon-isotopic composition of platform carbonate sediments.

Highly variable carbon isotope DIC values in shallow-water environments are possible due to slow rates of air-sea gas exchange, meaning that surface water carbon isotope values can diverge from equilibrium with the overlying atmosphere. The exchange of carbon dioxide across the air-sea interface is associated with kinetic isotope effects, with the preferential dissolution and degassing of 12C. Surface waters that have low DIC concentrations with net invasion of carbon dioxide may therefore have lower carbon isotope values compared to surface waters with high DIC concentration and net degassing of carbon dioxide. In the modern ocean these kinetic effects are relatively small. In contrast, kinetic isotope effects associated with gas exchange can be pronounced in shallow-water hypersaline and restricted environments (e.g., Lazar and Erez, 1992; Clark et al. 1992; Beeler et al. 2020). In these settings, carbonate with carbon isotope values between -25 and +15‰ have been documented. We use numerical models, ground-truthed in modern observations, to explore kinetic isotope effects associated with air-sea gas exchange of carbon dioxide and explore the potential role of kinetic isotopes effect in the carbon isotope record of ancient platform sediments.

Photos from left to right: (1) Figure outlining frame-work of carbonate chemistry model. (2) Outcrop at Vinini Creek, showing the extend of oxidative weathering on ancient strata. (3) The differences between Fe minerals in outcrop and core samples reveals the effects from oxidative weathering.

Sensitivity of Fe speciation to oxidative weathering

The concentration of reactive Fe in sedimentary rocks is extremely sensitive to modern weathering processes. Understanding the record of redox sensitive elements in ancient sediments is fundamental for extracting records of the concentration of atmospheric oxygen through Earth history. By using trace element analysis of samples from a shallow drill-core and coincident outcrop from Vinini Creek (Central Nevada), we found that in core samples there is abundant iron bound to pyrite and siderite minerals. In contrast, in outcrop samples much of that iron had been remobilized and transformed into iron oxides. This work emphasizes the limitations for using measurements of the concentration of pyrite and iron oxide in rocks collected from outcrop to infer past changes in oxygen levels (the iron speciation proxy) and highlights the need for more robust methods to evaluate the degree of alteration and diagenesis in ancient sediments.