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Rifting under steam - how rift magmatism triggers methane venting from sedimentary basins
Berndt, C., Hensen, C., Mortera-Gutierrez, C., Sarkar, S., Geilert, S., Schmidt, M., … Lizarralde, D. (2016). Rifting under steam - how rift magmatism triggers methane venting from sedimentary basins. Geology, 44(9), 767-770. https://doi.org/10.1130/G38049.1
Water mass denitrification during the latest Permian extinction in the Sverdrup Basin, Arctic Canada
Knies, J., Grasby, S. E., Beauchamp, B., & Schubert, C. J. (2013). Water mass denitrification during the latest Permian extinction in the Sverdrup Basin, Arctic Canada. Geology, 41(2), 167-170. https://doi.org/10.1130/G33816.1
Recovery of the forest ecosystem in the tropical lowlands of northern Guatemala after disintegration of Classic Maya polities
Mueller, A. D., Islebe, G. A., Anselmetti, F. S., Ariztegui, D., Brenner, M., Hodell, D. A., … Kennett, D. J. (2010). Recovery of the forest ecosystem in the tropical lowlands of northern Guatemala after disintegration of Classic Maya polities. Geology, 38(6), 523-526. https://doi.org/10.1130/G30797.1
Noble gas signatures of high recharge pulses and migrating jet stream in the late Pleistocene over Black Mesa, Arizona, United States
Zhu, C., & Kipfer, R. (2010). Noble gas signatures of high recharge pulses and migrating jet stream in the late Pleistocene over Black Mesa, Arizona, United States. Geology, 38(1), 83-86. https://doi.org/10.1130/G30369.1
Groundwater and climate dynamics derived from noble gas, <SUP>14</SUP>C, and stable isotope data
Klump, S., Grundl, T., Purtschert, R., & Kipfer, R. (2008). Groundwater and climate dynamics derived from noble gas, 14C, and stable isotope data. Geology, 36(5), 395-398. https://doi.org/10.1130/G24604A.1
Aerobic microbial dolomite at the nanometer scale: implications for the geologic record
Sánchez-Román, M., Vasconcelos, C., Schmid, T., Dittrich, M., McKenzie, J. A., Zenobi, R., & Rivadeneyra, M. A. (2008). Aerobic microbial dolomite at the nanometer scale: implications for the geologic record. Geology, 36(11), 879-882. https://doi.org/10.1130/G25013A.1
Quantification of soil erosion rates related to ancient Maya deforestation
Anselmetti, F. S., Hodell, D. A., Ariztegui, D., Brenner, M., & Rosenmeier, M. F. (2007). Quantification of soil erosion rates related to ancient Maya deforestation. Geology, 35(10), 915-918. https://doi.org/10.1130/G23834A.1
High-resolution analyses of an early Holocene climate event may imply decreased solar forcing as an important climate trigger
Björck, S., Muscheler, R., Kromer, B., Andresen, C. S., Heinemeier, J., Johnsen, S. J., … Veski, S. (2001). High-resolution analyses of an early Holocene climate event may imply decreased solar forcing as an important climate trigger. Geology, 29(12), 1107-1110. https://doi.org/10.1130/0091-7613(2001)029<1107:HRAOAE>2.0.CO;2
Mapping the architecture of glaciofluvial sediments with three-dimensional georadar
Beres, M., Green, A., Huggenberger, P., & Horstmeyer, H. (1995). Mapping the architecture of glaciofluvial sediments with three-dimensional georadar. Geology, 23(12), 1087-1090. https://doi.org/10.1130/0091-7613(1995)023<1087:MTAOGS>2.3.CO;2
Minimum <SUP>10</SUP>Be exposure ages of early Pliocene for the Table Mountain Plateau and the Sirius Group at Mount Fleming, Dry Valleys, Antarctica
Ivy-Ochs, S., Schlüchter, C., Kubik, P. W., Dittrich-Hannen, B., & Beer, J. (1995). Minimum 10Be exposure ages of early Pliocene for the Table Mountain Plateau and the Sirius Group at Mount Fleming, Dry Valleys, Antarctica. Geology, 23(11), 1007-1010. https://doi.org/10.1130/0091-7613(1995)023<1007:MBEAOE>2.3.CO;2