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Isotopic evidence for elevated photorespiration during the last glacial period

Low carbon dioxide levels during the last glacial period enhanced photorespiration in trees across North America, indicating a decline in land plant productivity, according to measurements of clumped isotopes in subfossil wood samples.

Max K. Lloyd
Rebekah S. Sprengel
Daniel A. Stolper
Research05 Nov 2025
Nature Geoscience

Volume: 18, P: 1232-1238
Cerium/lead and lead isotope ratios in arc magmas and the enrichment of lead in the continents

Daniel M. Miller
Steven L. Goldstein
Charles H. Langmuir
Research07 Apr 1994
Nature

Volume: 368, P: 514-520
An abiotic model for stromatolite morphogenesis

John P. Grotzinger
Daniel H. Rothman
Research03 Oct 1996
Nature

Volume: 383, P: 423-425
A record of deep-ocean dissolved O₂ from the oxidation state of iron in submarine basalts

Deep-ocean O2 concentrations over the past 3.5 billion years are estimated using the oxidation state of iron in submarine basalts and indicate that deep-ocean oxygenation occurred in the Phanerozoic.

Daniel A. Stolper
C. Brenhin Keller
Research03 Jan 2018
Nature

Volume: 553, P: 323-327
Neogene cooling driven by land surface reactivity rather than increased weathering fluxes

A carbon cycle model constrained by weathering-sensitive isotopic tracers reveals that long-term cooling in the Neogene period reflects a change in how surface denudation is partitioned into weathering and erosion.

Jeremy K. Caves Rugenstein
Daniel E. Ibarra
Friedhelm von Blanckenburg
Research03 Jul 2019
Nature

Volume: 571, P: 99-102