Early hydrothermal carbon uptake by the upper oceanic crust: Insight from in situ U-Pb dating

Alteration of ocean crust provides a strong temperature dependent feedback on the geological carbon cycle and is a primary driver of the Sr-isotopic composition of seawater

(2015) Laurence A. Coogan et al.   EARTH AND PLANETARY SCIENCE LETTERS

U–Pb dating of cements in Mesozoic ammonites

(2014) Q. Li et al.   CHEMICAL GEOLOGY

Tectonic interleaving along the Main Central Thrust, Sikkim Himalaya

(2014) Catherine M. Mottram et al.   JOURNAL OF THE GEOLOGICAL SOCIETY

Calcium carbonate veins in ocean crust record a threefold increase of seawater Mg/Ca in the past 30 million years

(2013) Svenja Rausch et al.   EARTH AND PLANETARY SCIENCE LETTERS

Evidence that low-temperature oceanic hydrothermal systems play an important role in the silicate-carbonate weathering cycle and long-term climate regulation

(2013) Laurence A. Coogan et al.   GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS

Secular variation in carbon uptake into the ocean crust

(2011) K.M. Gillis et al.   EARTH AND PLANETARY SCIENCE LETTERS

Reconstructing Past Seawater Mg/Ca and Sr/Ca from Mid-Ocean Ridge Flank Calcium Carbonate Veins

(2010) R. M. Coggon et al.   SCIENCE