
John A. Higgins
· Professor of GeosciencesPrinceton University · Geosciences
Active 1919–2026
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About
Professor John A. Higgins is a faculty member in the Department of Geosciences at Princeton University, where he leads the Higgins Research Laboratory. His primary research interest is the evolution of the carbon cycle and the global climate system over Earth history. He focuses on processes that control the chemical composition of seawater and how these processes have changed on geologic timescales. Additionally, he studies how the chemistry of carbonate sediments is affected by post-depositional processes such as early diagenetic recrystallization, dolomitization, and hydrothermal alteration. Professor Higgins employs a variety of tools in his research, including numerical models of chemical and isotopic biogeochemical cycles, analysis of traditional stable isotopes of oxygen and carbon, and the application of new isotope systems such as magnesium, calcium, and potassium. His work contributes to understanding the complex interactions within Earth's climate and geochemical systems, shedding light on the history of Earth's climate and biogeochemical processes.
Research topics
- Geology
- Chemistry
- Paleontology
- Geochemistry
- Oceanography
- Environmental chemistry
- Environmental science
- Ecology
- Materials science
- Earth science
Selected publications
A lithium-isotope perspective on the evolution of carbon and silicon cycles
Nature · 2021 · 152 citations
Groundwater discharge impacts marine isotope budgets of Li, Mg, Ca, Sr, and Ba
Nature Communications · 2021 · 100 citations
Groundwater-derived solute fluxes to the ocean have long been assumed static and subordinate to riverine fluxes, if not neglected entirely, in marine isotope budgets. Here we present concentration and isotope data for Li, Mg, Ca, Sr, and Ba in coastal groundwaters to constrain the importance of groundwater discharge in mediating the magnitude and isotopic composition of terrestrially derived solute fluxes to the ocean. Data were extrapolated globally using three independent volumetric estimates…
Earth and Planetary Science Letters · 2020 · 98 citations
Senior authorCorrespondingEarth-Science Reviews · 2021 · 75 citations
The origin of carbonate mud and implications for global climate
Proceedings of the National Academy of Sciences · 2022 · 54 citations
Carbonate mud represents one of the most important geochemical archives for reconstructing ancient climatic, environmental, and evolutionary change from the rock record. Mud also represents a major sink in the global carbon cycle. Yet, there remains no consensus about how and where carbonate mud is formed. Here, we present stable isotope and trace-element data from carbonate constituents in the Bahamas, including ooids, corals, foraminifera, and algae. We use geochemical fingerprinting to demons…
Recent grants
NSF · $576k · 2015–2020
CAREER: What sets the CO2 thermostat? Insights from the global geochemical cycles of Ca, Mg, and K
NSF · $819k · 2017–2022
NSF · $1.1M · 2018–2024
Frequent coauthors
- 44 shared
Daniel P. Schrag
- 27 shared
Clara L. Blättler
- 22 shared
Anne‐Sofie C. Ahm
- 19 shared
Adam C. Maloof
Princeton University
- 18 shared
D. Santiago Ramos
- 17 shared
Michael L. Bender
BASF (Germany)
- 17 shared
Daniel A. Stolper
University of California, Berkeley
- 17 shared
Francis A. Macdonald
Labs
Awards & honors
- UCAR Next Generation Science Fellow (2024)
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