Peter Swart
mgg.rsmas.miami.edu
0000-0002-6743-6162
98 papers found
Refreshing results…
A calibration equation between Δ 48 values of carbonate and temperature
InterCarb: A Community Effort to Improve Interlaboratory Standardization of the Carbonate Clumped Isotope Thermometer Using Carbonate Standards
An abrupt Middle-Miocene increase in fluid flow into the Leeward Margin Great Bahama Bank, constraints from δ44Ca and Δ47 values
Calibration of carbonate-water triple oxygen isotope fractionation: seeing through diagenesis in ancient carbonates
Anomalous δ13C in Particulate Organic Carbon at the Chemoautotrophy Maximum in the Cariaco Basin
Boiled or roasted? Bivalve cooking methods of early Puerto Ricans elucidated using clumped isotopes
Dripwater and Calcite Geochemistry Variations in a Monitored Bahamas Cave
Cyclic anoxia and organic rich carbonate sediments within a drowned carbonate platform linked to Antarctic ice volume changes: Late Oligocene-early Miocene Maldives
A diagenetic origin for isotopic variability of sediments deposited on the margin of Great Bahama Bank, insights from clumped isotopes
Oxygen Isotopic Exchange Between CO 2 and Phosphoric Acid: Implications for the Measurement of Clumped Isotopes in Carbonates
Deposition and early diagenesis of microbial mud in the Florida Everglades
Do drifts deposited adjacent to carbonate platforms record the signal of global carbon isotopic values?
Evaluating the fidelity of the cerium paleoredox tracer during variable carbonate diagenesis on the Great Bahamas Bank
The limited link between accommodation space, sediment thickness, and inner platform facies distribution (Holocene-Pleistocene, Bahamas)
A Kinetic Difference Between 12 C- and 13 C-Bound Oxygen Exchange Rates Results in Decoupled δ18 O and Δ47 Values of Equilibrating DIC Solutions
Revised interpretations of stable C and O patterns in carbonate rocks resulting from meteoric diagenesis
The effect of changing seawater Ca and Mg concentrations upon the distribution coefficients of Mg and Sr in the skeletons of the scleractinian coral Pocillopora damicornis
Light Stable Isotopic Compositions of Enriched Mantle Sources: Resolving the Dehydration Paradox
Hydrodynamic control of whitings on Great Bahama Bank
Microbially mediated organomineralization in the formation of ooids
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