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Jadranka Bare?ic, Sanja Faivre, Andreja Sironic, Damir Borkovic, Ivanka Lovrencic Mikelic, Russel N. Drysdale and Ines Krajcar Bronic
Tufa is a fresh-water surface calcium carbonate deposit precipitated at or near ambient temperature, and commonly contains the remains of macro- and microphytes. Many Holocene tufas are found along the Zrmanja River, Dalmatian karst, Croatia. In this wor...
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Augusto Nicolás Varela, María Sol Raigemborn, Patricio Emmanuel Santamarina, Sabrina Lizzoli, Thierry Adatte and Ulrich Heimhofer
The Cenomanian Mata Amarilla Formation (MAF) in southern Patagonia (~55° S paleolatitude, Austral-Magallanes Basin, Argentina) is composed mainly of stacked fluvial deposits with intercalated paleosols, which document Cenomanian environments at high-pale...
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Nikolai Pedentchouk, Barry Bennett and Steve Larter
This study investigates the magnitude and direction of stable C and H isotope shifts of n-C15?30 alkanes from biodegraded oils sourced from Type II (Oil suite S) and Type II/III (Oil suite H) kerogens. Compound-specific isotope data show a 2.0? 13C-enric...
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Yuichi Morishita and Ayaka Wada
The Kamioka mine, located in Gifu Prefecture in Japan, is famous for the large water Cherenkov detector system, the Super-Kamiokande. The Kamioka skarn-type Pb?Zn deposits are formed in crystalline limestone and are replaced by skarn minerals within the ...
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Henrik Drake, Magnus Ivarsson and Christine Heim
The oceanic and continental lithosphere constitutes Earth?s largest microbial habitat, yet it is scarcely investigated and not well understood. The physical and chemical properties here are distinctly different from the overlaying soils and the hydrosphe...
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