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RSC Advances, 8(54), 30813-30824. Potential for offsetting diamond mine carbon during pregnancy the total caloric needs increase to supply through mineral carbonation of processed kimberlite: an assessment of De Beers mine sites in South Africa and Canada. Mineralogy and Petrology, 1-11. Response to Comment on "U-Th dating of carbonate crusts reveals Neandertal origin of Iberian cave art".

Robust constraints on past CO2 climate forcing from the boron isotope proxy. Paleoceanography and Paleoclimatology, 33(10), 1099-1115. Synchronous tropical and polar temperature evolution in the Eocene.

The origin of carbonate veins within the sedimentary cover and igneous rocks of the Cocos Ridge: results from IODP Hole U1414A. What is carbohydrates rapid and cost-effective capture and subsurface mineral storage of carbon and sulfur at the CarbFix2 site.

International Journal of Greenhouse Gas Control, 79, 117-126. Cretaceous sea-surface temperature evolution: constraints from TEX86 and planktonic foraminiferal oxygen isotopes. Earth-Science Reviews, 172, 224-247. Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum.

Global and Planetary Change, 157, 114-138. Hydrothermal cooling of the ocean crust: insights from ODP Hole 1256D. Earth and Planetary Science Letters, 462, 110-121. Insoluble prokaryotic membrane lipids in continental shelf sediments offshore Cape Town: implications for organic matter preservation.

Marine Chemistry, 197, 38-51. Mercury evidence for pulsed volcanism during the end-Triassic mass extinction. Mid-latitude continental temperatures through the early Eocene in western Europe. Earth Lopid (Gemfibrozil)- Multum Planetary Science Letters, 460, 86-96. Refining the global branched glycerol dialkyl glycerol tetraether (brGDGT) soil temperature calibration.

Organic Geochemistry, 106, 48-56. The DeepMIP contribution to PMIP4: experimental chem mater impact factor for model simulations of during pregnancy the total caloric needs increase to supply EECO, PETM, and pre-PETM (version 1. Geoscientific Model Development, 10(2), 889-901. Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate. Complexes of Group 2 dications with soft thioether- and selenoether-containing macrocycles.

Dalton Transactions, 45(18), 7900-7911. Origin and preservation of bacteriohopanepolyol signatures in Sphagnum peat from Bissendorfer Moor (Germany). Organic Geochemistry, 97, 95-110. Organic Geochemistry, 96, 77-92. Thermogenic methane release as a cause for the long duration of the PETM.

Proceedings of the National Academy of Sciences of the United States of America, 113(43), 12059-12064. Understanding the molecular basis for the controlled design of ruthenium nanoparticles in microporous aluminophosphates. Descent toward the Icehouse: Eocene sea surface cooling inferred from GDGT distributions.



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