TY  - JOUR
A1  - Srama, Ralf
A1  - Krueger, H.
A1  - Yamaguchi, T.
A1  - Stephan, T.
A1  - Burchell, M.
A1  - Kearsley, A. T.
A1  - Sterken, V.
A1  - Postberg, F.
A1  - Kempf, S.
A1  - Grün, Eberhard
A1  - Altobelli, Nicolas
A1  - Ehrenfreund, P.
A1  - Dikarev, V.
A1  - Horanyi, M.
A1  - Sternovsky, Zoltan
A1  - Carpenter, J. D.
A1  - Westphal, A.
A1  - Gainsforth, Z.
A1  - Krabbe, A.
A1  - Agarwal, Jessica
A1  - Yano, H.
A1  - Blum, J.
A1  - Henkel, H.
A1  - Hillier, J.
A1  - Hoppe, P.
A1  - Trieloff, M.
A1  - Hsu, S.
A1  - Mocker, A.
A1  - Fiege, K.
A1  - Green, S. F.
A1  - Bischoff, A.
A1  - Esposito, F.
A1  - Laufer, R.
A1  - Hyde, T. W.
A1  - Herdrich, G.
A1  - Fasoulas, S.
A1  - Jaeckel, A.
A1  - Jones, G.
A1  - Jenniskens, P.
A1  - Khalisi, E.
A1  - Moragas-Klostermeyer, Georg
A1  - Spahn, Frank
A1  - Keller, H. U.
A1  - Frisch, P.
A1  - Levasseur-Regourd, A. C.
A1  - Pailer, N.
A1  - Altwegg, K.
A1  - Engrand, C.
A1  - Auer, S.
A1  - Silen, J.
A1  - Sasaki, S.
A1  - Kobayashi, M.
A1  - Schmidt, J.
A1  - Kissel, J.
A1  - Marty, B.
A1  - Michel, P.
A1  - Palumbo, P.
A1  - Vaisberg, O.
A1  - Baggaley, J.
A1  - Rotundi, A.
A1  - Roeser, H. P.
T1  - SARIM PLUS-sample return of comet 67P/CG and of interstellar matter
JF  - EXPERIMENTAL ASTRONOMY
N2  - The Stardust mission returned cometary, interplanetary and (probably) interstellar dust in 2006 to Earth that have been analysed in Earth laboratories worldwide. Results of this mission have changed our view and knowledge on the early solar nebula. The Rosetta mission is on its way to land on comet 67P/Churyumov-Gerasimenko and will investigate for the first time in great detail the comet nucleus and its environment starting in 2014. Additional astronomy and planetary space missions will further contribute to our understanding of dust generation, evolution and destruction in interstellar and interplanetary space and provide constraints on solar system formation and processes that led to the origin of life on Earth. One of these missions, SARIM-PLUS, will provide a unique perspective by measuring interplanetary and interstellar dust with high accuracy and sensitivity in our inner solar system between 1 and 2 AU. SARIM-PLUS employs latest in-situ techniques for a full characterisation of individual micrometeoroids (flux, mass, charge, trajectory, composition()) and collects and returns these samples to Earth for a detailed analysis. The opportunity to visit again the target comet of the Rosetta mission 67P/Churyumov-Gerasimeenternko, and to investigate its dusty environment six years after Rosetta with complementary methods is unique and strongly enhances and supports the scientific exploration of this target and the entire Rosetta mission. Launch opportunities are in 2020 with a backup window starting early 2026. The comet encounter occurs in September 2021 and the reentry takes place in early 2024. An encounter speed of 6 km/s ensures comparable results to the Stardust mission.
KW  - Interstellar dust
KW  - Cometary dust
KW  - Churyumov Gerasimenko
KW  - Interplanetary dust
KW  - IMF
KW  - Cosmic vision
KW  - Sample return
KW  - Dust collector
KW  - Mass spectrometry
Y1  - 2012
U6  - https://doi.org/10.1007/s10686-011-9285-7
SN  - 0922-6435
SN  - 1572-9508
VL  - 33
IS  - 2-3
SP  - 723
EP  - 751
PB  - SPRINGER
CY  - DORDRECHT
ER  - 
TY  - JOUR
A1  - Ijiri, Akira
A1  - Inagaki, Fumio
A1  - Kubo, Yusuke
A1  - Adhikari, Rishi Ram
A1  - Hattori, Shohei
A1  - Hoshino, Tatsuhiko
A1  - Imachi, Hiroyuki
A1  - Kawagucci, Shinsuke
A1  - Morono, Yuki
A1  - Ohtomo, Yoko
A1  - Ono, Shuhei
A1  - Sakai, Sanae
A1  - Takai, Ken
A1  - Toki, Tomohiro
A1  - Wang, David T.
A1  - Yoshinaga, Marcos Y.
A1  - Arnold, Gail L.
A1  - Ashi, Juichiro
A1  - Case, David H.
A1  - Feseker, Tomas
A1  - Hinrichs, Kai-Uwe
A1  - Ikegawa, Yojiro
A1  - Ikehara, Minoru
A1  - Kallmeyer, Jens
A1  - Kumagai, Hidenori
A1  - Lever, Mark Alexander
A1  - Morita, Sumito
A1  - Nakamura, Ko-ichi
A1  - Nakamura, Yuki
A1  - Nishizawa, Manabu
A1  - Orphan, Victoria J.
A1  - Roy, Hans
A1  - Schmidt, Frauke
A1  - Tani, Atsushi
A1  - Tanikawa, Wataru
A1  - Terada, Takeshi
A1  - Tomaru, Hitoshi
A1  - Tsuji, Takeshi
A1  - Tsunogai, Urumu
A1  - Yamaguchi, Yasuhiko T.
A1  - Yoshida, Naohiro
T1  - Deep-biosphere methane production stimulated by geofluids in the Nankai accretionary complex
JF  - Science Advances
Y1  - 2018
U6  - https://doi.org/10.1126/sciadv.aao4631
SN  - 2375-2548
VL  - 4
IS  - 6
PB  - American Assoc. for the Advancement of Science
CY  - Washington
ER  - 
TY  - GEN
A1  - Ijiri, Akira
A1  - Inagaki, Fumio
A1  - Kubo, Yusuke
A1  - Adhikari, Rishi Ram
A1  - Hattori, Shohei
A1  - Hoshino, Tatsuhiko
A1  - Imachi, Hiroyuki
A1  - Kawagucci, Shinsuke
A1  - Morono, Yuki
A1  - Ohtomo, Yoko
A1  - Ono, Shuhei
A1  - Sakai, Sanae
A1  - Takai, Ken
A1  - Toki, Tomohiro
A1  - Wang, David T.
A1  - Yoshinaga, Marcos Y.
A1  - Arnold, Gail L.
A1  - Ashi, Juichiro
A1  - Case, David H.
A1  - Feseker, Tomas
A1  - Hinrichs, Kai-Uwe
A1  - Ikegawa, Yojiro
A1  - Ikehara, Minoru
A1  - Kallmeyer, Jens
A1  - Kumagai, Hidenori
A1  - Lever, Mark Alexander
A1  - Morita, Sumito
A1  - Nakamura, Ko-ichi
A1  - Nakamura, Yuki
A1  - Nishizawa, Manabu
A1  - Orphan, Victoria J.
A1  - Røy, Hans
A1  - Schmidt, Frauke
A1  - Tani, Atsushi
A1  - Tanikawa, Wataru
A1  - Terada, Takeshi
A1  - Tomaru, Hitoshi
A1  - Tsuji, Takeshi
A1  - Tsunogai, Urumu
A1  - Yamaguchi, Yasuhiko T.
A1  - Yoshida, Naohiro
T1  - Deep-biosphere methane production stimulated by geofluids in the Nankai accretionary complex
T2  - Postprints der Universität Potsdam Mathematisch-Naturwissenschaftliche Reihe
N2  - Microbial life inhabiting subseafloor sediments plays an important role in Earth’s carbon cycle. However, the impact of geodynamic processes on the distributions and carbon-cycling activities of subseafloor life remains poorly constrained. We explore a submarine mud volcano of the Nankai accretionary complex by drilling down to 200 m below the summit. Stable isotopic compositions of water and carbon compounds, including clumped methane isotopologues, suggest that ~90% of methane is microbially produced at 16° to 30°C and 300 to 900 m below seafloor, corresponding to the basin bottom, where fluids in the accretionary prism are supplied via megasplay faults. Radiotracer experiments showed that relatively small microbial populations in deep mud volcano sediments (10 2 to 10 3 cells cm −3 ) include highly active hydrogenotrophic methanogens and acetogens. Our findings indicate that subduction-associated fluid migration has stimulated microbial activity in the mud reservoir and that mud volcanoes may contribute more substantially to the methane budget than previously estimated.
T3  - Zweitveröffentlichungen der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe - 802 
KW  - multiply-substituted isotopologues
KW  - marine subsurface sediments
KW  - carbon isotopic composition
KW  - submarine mud volcano
KW  - intact polar lipids
KW  - fore-arc basin
KW  - subseafloor sediments
KW  - microbial lipids
KW  - Cascadia margin
KW  - organic-acids
Y1  - 2019
U6  - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-427002
SN  - 1866-8372
IS  - 802
ER  -