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Daniel Ibarra
Brown UniversityMeeting roles in:
Balancing the weathering budget in deglaciating catchments: a case study from Kachemak Bay, AK
Time-dependent controls of clay mineral formation impact the net alkalinity generation from rock weathering
Lab dissolution experiments and reactive transport models reveal the interplay between alkalinity generation and secondary mineral formation in the Upper Deschutes Basin, Oregon
Hydrologic and geomorphic controls on bedrock organic carbon export
Glacial Lake Mojave core sedimentology, chronology, and initial lake state interpretations.
Paleohydrologic Analysis of Glacial Lake Mojave using Shoreline Tufa and Ostracod Valve Geochemistry
Using Stable Isotope and Clumped Isotope Analysis to Reconstruct Surface Uplift of the Altai Mountains.
Plant wax record of hydroclimate over the last two glacial cycles at Bear Lake and Great Salt Lake, Utah
Is Mono at Mono? Revisiting the Mono Lake Excursion with High-Resolution Paleomagnetic Records
Impact of clay mineralogy on lithium isotope fractionation during rock weathering
Moisture Source vs Rainfall Amount in a Last Interglacial Stalagmite from the Philippines
Origin and Accumulation of Lithium in Groundwater
The Origin and Enrichment of Sedimentary Basin Lithium Brines: A Case Study from the Upper Devonian Leduc Formation, Alberta Basin, Canada
Neogene Southwestern U.S. Temperatures Paced by Global Temperature Change
Lithium Isotopes as Tracers of Silicate Weathering Intensity and Clay Formation in the East River Watershed, Colorado
~1,500 Years of Gardiner’s Clay Varves Extend the Record of Laurentide Ice in Southern New England to Before the Last Glacial Maximum
Isotopic and mineralogical fingerprinting of late Pleistocene iron oxide “Rattle Stones” in southern New England and implications for a potential Last Glacial Maximum sea-level highstand
Comparing Triple Oxygen (δ18O-δ17O) and δ18O-δ2H Isotope Systematics Using a Lake Balance Approach: Insights from Bear Lake, Utah-Idaho
Triple Oxygen Isotope Constraints on Fluid Alteration of Serpentinite, Twin Sisters Massif, Washington
Mineral and Textural Observations of Serpentinized Fault Surfaces at Twin Sisters, WA
Does secondary mineral formation compete or cooperate with organic matter storage?
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