Zobrazeno 1 - 10
of 174
pro vyhledávání: '"J. A. De Moor"'
Autor:
Raegan Paul, Timothy J Rogers, Kate M Fullerton, Matteo Selci, Martina Cascone, Murray H Stokes, Andrew D Steen, J Maarten de Moor, Agostina Chiodi, Andri Stefánsson, Sæmundur A Halldórsson, Carlos J Ramirez, Gerdhard L Jessen, Peter H Barry, Angelina Cordone, Donato Giovannelli, Karen G Lloyd
Publikováno v:
PLoS ONE, Vol 18, Iss 8, p e0281277 (2023)
Microbial communities in terrestrial geothermal systems often contain chemolithoautotrophs with well-characterized distributions and metabolic capabilities. However, the extent to which organic matter produced by these chemolithoautotrophs supports h
Externí odkaz:
https://doaj.org/article/b8cf7c9b5ccf40fe9a0f58eaac60e14b
Autor:
Geoffroy Avard, Mauricio Mora, Henriette Bakkar, Guillermo Alvarado, Mario Angarita, Monserrat Cascante, J. Maarten de Moor, María Martínez, Cyril Muller, Javier Pacheco, Paulo Ruiz, Gerardo Soto
Publikováno v:
Volcanica, Vol 4, Iss S1, Pp 141-161 (2021)
Costa Rica hosts ten volcanic complexes and is highly tectonically active due to its location at the interaction between the Cocos, Nazca, and Caribbean plates and the Panama microplate. Three of the five historically active volcanoes had frequent er
Externí odkaz:
https://doaj.org/article/653dea0b6fb14d2a93b316e14f511102
Autor:
Donato Giovannelli, Peter H. Barry, J. Maarten de Moor, Gerdhard L. Jessen, Matthew O. Schrenk, Karen G. Lloyd
Publikováno v:
Frontiers in Microbiology, Vol 13 (2022)
Despite being one of the largest microbial ecosystems on Earth, many basic open questions remain about how life exists and thrives in the deep subsurface biosphere. Much of this ambiguity is due to the fact that it is exceedingly difficult and often
Externí odkaz:
https://doaj.org/article/c7f886774bd944b994ec50673ace4dcc
Autor:
P. H. Barry, J. M. De Moor, A. Chiodi, F. Aguilera, M. R. Hudak, D. V. Bekaert, S. J. Turner, J. Curtice, A. M. Seltzer, G. L. Jessen, E. Osses, J. M. Blamey, M. J. Amenábar, M. Selci, M. Cascone, A. Bastianoni, M. Nakagawa, R. Filipovich, E. Bustos, M. O. Schrenk, J. Buongiorno, C. J. Ramírez, T. J. Rogers, K. G. Lloyd, D. Giovannelli
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Subduction zones represent the interface between Earth’s interior (crust and mantle) and exterior (atmosphere and oceans), where carbon and other volatile elements are actively cycled between Earth reservoirs by plate tectonics. Helium is a sensiti
Externí odkaz:
https://doaj.org/article/4f322e99cae24a638940d1b21922b890
Autor:
J. Rüdiger, A. Gutmann, N. Bobrowski, M. Liotta, J. M. de Moor, R. Sander, F. Dinger, J.-L. Tirpitz, M. Ibarra, A. Saballos, M. Martínez, E. Mendoza, A. Ferrufino, J. Stix, J. Valdés, J. M. Castro, T. Hoffmann
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 3371-3393 (2021)
Volcanic emissions are a source of halogens in the atmosphere. Rapid reactions convert the initially emitted hydrogen halides (HCl, HBr, and HI) into reactive species such as BrO, Br2, BrCl, ClO, OClO, and IO. The activation reaction mechanisms in th
Externí odkaz:
https://doaj.org/article/8eb722bb937345e1a1e87749fed1070f
Autor:
Timothy J. Rogers, Joy Buongiorno, Gerdhard L. Jessen, Matthew O. Schrenk, James A. Fordyce, J. Maarten de Moor, Carlos J. Ramírez, Peter H. Barry, Mustafa Yücel, Matteo Selci, Angela Cordone, Donato Giovannelli, Karen G. Lloyd
Publikováno v:
The ISME Journal
Autor:
Andrés Ulloa, Fernando Gázquez, Aurelio Sanz-Arranz, Jesús Medina, Fernando Rull, José María Calaforra, Guillermo E. Alvarado, María Martínez, Geoffroy Avard, J. Maarten De Moor, Jo De Waele
Publikováno v:
International Journal of Speleology, Vol 47, Iss 2, Pp 229-246 (2018)
The caves of the Irazú volcano (Costa Rica), became accessible after the partial collapse of the NW sector of the Irazú volcano in 1994, offering the opportunity to investigate active minerogenetic processes in volcanic cave environments. We perfor
Externí odkaz:
https://doaj.org/article/392fa0f901cf4d2d9bf4a93b473a98d8
Autor:
John Stix, J. Maarten de Moor
Publikováno v:
Earth, Planets and Space, Vol 70, Iss 1, Pp 1-19 (2018)
Abstract This paper examines phreatic eruptions which are driven by inputs of magma and magmatic gas. We synthesize data from several significant phreatic systems, including two in Costa Rica (Turrialba and Poás) which are currently highly active an
Externí odkaz:
https://doaj.org/article/c0102afc31474b12b753dbd79020b31b
Autor:
J. Rüdiger, J.-L. Tirpitz, J. M. de Moor, N. Bobrowski, A. Gutmann, M. Liuzzo, M. Ibarra, T. Hoffmann
Publikováno v:
Atmospheric Measurement Techniques, Vol 11, Pp 2441-2457 (2018)
Volcanoes are a natural source of several reactive gases (e.g., sulfur and halogen containing species) and nonreactive gases (e.g., carbon dioxide) to the atmosphere. The relative abundance of carbon and sulfur in volcanic gas as well as the total
Externí odkaz:
https://doaj.org/article/19b1a0ccdf8e4353b8946e07095f58e4
Autor:
David V. Bekaert, Peter H. Barry, Michael W. Broadley, David J. Byrne, Bernard Marty, Carlos J. Ramírez, J. Maarten de Moor, Alejandro Rodriguez, Michael R. Hudak, Adam V. Subhas, Saemundur A. Halldórsson, Andri Stefánsson, Antonio Caracausi, Karen G. Lloyd, Donato Giovannelli, Alan M. Seltzer
Publikováno v:
Science Advances. 9
Mantle-derived noble gases in volcanic gases are powerful tracers of terrestrial volatile evolution, as they contain mixtures of both primordial (from Earth’s accretion) and secondary (e.g., radiogenic) isotope signals that characterize the composi