Results 151 to 160 of about 113,669 (215)

Viral infections stimulate the metabolism and shape prokaryotic assemblages in submarine mud volcanoes. [PDF]

ISME J, 2012
Corinaldesi C, Dell'Anno A, Danovaro R.
europepmc   +1 more source

Toledo Mud Hens score card and civic magazine, volume 2, 1945

This issue of the Toledo Mud Hens Score Card and Civic Magazine details the history of the city of Toledo, Ohio from 1845 to 1885. Published in 1945, it includes rules for scoring baseball and a blank score card from the Milwaukee Brewers at the Toledo ...

core  

The Size of Greater India: Estimates by Comparing the Apparent Polar Wander Paths of the Tethyan Himalaya and the Indian Craton

Geochemistry, Geophysics, Geosystems, Volume 27, Issue 10, October 2026.
Abstract The northern extent of Greater India is a critical, yet highly debated, parameter for reconstructing the India‐Asia collision. Previous paleomagnetic estimates, including the fill‐the‐gap and fixed great circle approaches, yield widely varying results, spanning from ∼200 to ∼3,000 km. These large discrepancies stem principally from two primary
Xianwei Jiao, Suo Wang, Yong Zhao, Tongming Fang   +3 more
wiley   +1 more source

Comparing microbial populations from diverse hydrothermal features in Yellowstone National Park: hot springs and mud volcanoes. [PDF]

Front Microbiol
Rowe L, Dowd SE, Davidson K, Kovarik C, VanAken M, Jarabek A, Taylor C.   +6 more
europepmc   +1 more source

Early Archean serpentine mud volcanoes at Isua, Greenland, as a niche for early life. [PDF]

Proc Natl Acad Sci U S A, 2011
Pons ML, Quitté G, Fujii T, Rosing MT, Reynard B, Moynier F, Douchet C, Albarède F.   +7 more
europepmc   +1 more source

The Wilson Cycle of the North Altyn Ocean: A Record of Subduction Initiation, Slab Rollback, and Final Closure

Geochemistry, Geophysics, Geosystems, Volume 27, Issue 10, October 2026.
Abstract The North Altyn ophiolitic belt was formed by the subduction–closure of the Altyn segment of the Proto–Tethys Ocean and recorded the accretion of Tarim to northern Gondwana, but the timing of initial subduction and detailed tectonic transition processes remain poorly constrained. This study reports the oldest Phanerozoic magmatic record of 537 
Long Chen, Jinlong Yao, Guochun Zhao, Yigui Han, Qian Liu, Donghai Zhang, Xijun Zhao, Hang Yang, Wei Li   +8 more
wiley   +1 more source

Toledo Mud Hens score card and civic magazine, volume 1, 1947

This issue of the Toledo Mud Hens Score Card and Civic Magazine gives a short history of the University of Toledo, in Toledo, Ohio. Published in 1947, it includes short biographies of select Toledo Mud Hens players and umpires, information about the new ...

core  

Ground Penetrating Radar Observations of Subsurface Structures From the Makgadikgadi Pans (Botswana): A Terrestrial Analogue of Martian Playa Lakes

Journal of Geophysical Research: Planets, Volume 131, Issue 10, October 2026.
Abstract Playa lakes are considered promising landing sites on Mars because of their strong astrobiological potential. Therefore, sediments and buried structures in terrestrial playa lakes have become the focus of numerous analogue studies. The inclusion of ground penetrating radar (GPR) in the payloads of Martian missions has opened new avenues for ...
M. Shawel, L. Capozzoli, T. H. Kahsay, B. Kgosidintsi, G. Romano, A. T. Selepeng, F. Franchi   +6 more
wiley   +1 more source

Toledo Mud Hens score card and civic magazine, volume 4, 1945

This issue of the Toledo Mud Hens Score Card and Civic Magazine details the history of the city of Toledo, Ohio from 1917 to 1945. Published in 1945, it includes rules for scoring baseball and a blank score card from the Kansas City Blues at the Toledo ...

core  

3D Architecture of Kodiak Butte as Evidence of Fluvial or Shoal‐Water Environments in Jezero Crater, Mars

Journal of Geophysical Research: Planets, Volume 131, Issue 10, October 2026.
Abstract The Mars 2020 mission has explored depositional environments recorded in a fan‐shaped deposit on the western side of Jezero crater. Kodiak butte is an isolated outcrop of sedimentary rock ∼1 km south of the western fan scarp and may be an erosional remnant of said fan.
O. A. Kanine, M. P. Lamb, B. L. Ehlmann, J. P. Grotzinger, C. D. Tate   +4 more
wiley   +1 more source