Research

Research overview:

Climate science relies upon an expanding toolkit of geochemical techniques for quantifying climate variations over earth history prior to our observational records. But ecology is still incipient in the development of proxies for quantifying past changes. This is the gap I aim to fill through my research. 

Using a geochemical technique -- the nitrogen isotopic composition (δ15N) of organics in fish otoliths (ear stones) -- that I developed with doctoral advisors Bess Ward and Danny Sigman at Princeton U, trophic level studies of fossil fishes are possible. I am applying this method to studies of historical (e.g., heavily fished Atlantic cod populations) and ancient (e.g., fossil otoliths from Miocene sediments) fish populations. The ultimate aim of my research is to gain a better understanding of the controls, feedbacks, and 'natural' variations in aquatic food webs. Through postdoctoral training at the Smithsonian Institution with Aaron O'Dea and UC Berkeley's Integrative Biology Department with Seth Finnegan, I am integrating paleontological methods and a deep time perspective into my research agenda.

I am particularly interested in patterns relating to high trophic level fishes in marine ecosystems, as fisheries resources form the economic, cultural, and nutritional foundation of coastal communities around the world. Quantitative records of ecological variations in the past will be critical to improve predictions about the future of marine ecosystems. Due to the lack of tools available for quantifying trophic level in animals, there are still major gaps in our understanding of the importance of trophic level across extinction events, for rates of speciation within and among clades, and for long term macroevolutionary patterns broadly.  

RESEARCH THEMES

methods

Can natural abundance stable isotopes of otolith organics be used as a tracer of fish dietary changes? Calibration, methods development, reproducibility

historical ecology

What was 'natural' in the past? Otolith-derived trophic level information is required because  animal tissues degrade quickly (and are therefore inaccessible for isotope analyses of ancient fishes)

paleontology

Does trophic level 'matter' for evolutionary outcomes? Detecting the drivers and consequences of fish trophic level on million-year timescales

isotopic groundtruthing

Using fossil-bound N isotopes for trophic reconstruction requires consideration of temporal and spatial averaging of 'isotopic baseline' 

environmental stressors

Has deoxygenation of the Baltic Sea affected cod trophic dynamics over their life history? 

biomineralization

What biomineralizatiion pathways are used by fishes to make their otoliths?