Zobrazeno 1 - 10
of 206
pro vyhledávání: '"Nehrke, G."'
Autor:
Devriendt, L.S., Mezger, E.M., Olsen, E.K., Watkins, J.M., Kaczmarek, K., Nehrke, G., de Nooijer, L.J., Reichart, G.-J.
Publikováno v:
In Geochimica et Cosmochimica Acta 1 December 2021 314:294-312
Autor:
Klages, J. P., Hillenbrand, C.-D., Bohaty, S. M., Salzmann, U., Bickert, T., Lohmann, G., Knahl, H. S., Gierz, P., Niu, L., Titschack, J., Kuhn, G., Frederichs, T., Müller, J., Bauersachs, T., Larter, R. D., Hochmuth, K., Ehrmann, W., Nehrke, G., Rodríguez-Tovar, F. J., Schmiedl, G.
Publikováno v:
Science; 7/19/2024, Vol. 385 Issue 6706, p322-327, 6p, 1 Color Photograph, 3 Diagrams
Autor:
Pederson, C.L., Mavromatis, V., Dietzel, M., Rollion-Bard, C., Breitenbach, S.F.M., Yu, D., Nehrke, G., Immenhauser, A.
Publikováno v:
In Sedimentary Geology August 2020 406
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Autor:
Seepma, S.Y.M.H., Ruiz-Hernandez, S.E., Nehrke, G., Soetaert, K., Philipse, A.P., Kuipers, B.W.M., Wolthers, M.
The effect of stoichiometry on the new formation and subsequent growth of CaCO3 was investigated over a large range of solutionstoichiometries (10–4 < raq < 104, where raq = {Ca2+}:{CO 32–}) at various, initially constant degrees of supersaturati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=narcis______::93c3217ebaa5521b2207fd99a8446c61
https://www.vliz.be/imisdocs/publications/34/359334.pdf
https://www.vliz.be/imisdocs/publications/34/359334.pdf
Autor:
Klages, J.P., Salzmann, U., Bickert, T., Hillenbrand, C.-D., Gohl, K., Kuhn, G., Bohaty, S.M., Titschack, J., Müller, J., Frederichs, T., Bauersachs, T., Ehrmann, W., van de Flierdt, T., Pereira, P.S., Larter, R.D., Lohmann, G., Niezgodzki, I., Uenzelmann-Neben, G., Zundel, M., Spiegel, C., Mark, C., Chew, D., Francis, J.E., Nehrke, G., Schwarz, F., Smith, J.A., Freudenthal, T., Esper, O., Pälike, H., Ronge, T.A., Dziadek, R., Afanasyeva, V., Arndt, J.E., Ebermann, B., Gebhardt, C., Hochmuth, K., Küssner, K., Najman, Y., Riefstahl, F., Scheinert, M., PS104, the Science Team of Expedition
The mid-Cretaceous period was one of the warmest intervals of the past 140 million years1–5, driven by atmospheric carbon dioxide levels of around 1,000 parts per million by volume6. In the near absence of proximal geological records from south of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cf65d76d967d194258415df31ffcae8d
http://hdl.handle.net/10044/1/76835
http://hdl.handle.net/10044/1/76835
Autor:
Ge, Y., Pederson, C.L., Lokier, S.W., Traas, J.P., Nehrke, G., Neuser, R.D., Goetschl, K.E., Immenhauser, Adrian
Modern cemented intervals (beachrock, firmgrounds to hardgrounds and concretionary layers) form in the lagoon and intertidal sabkha of Abu Dhabi. Seafloor lithification actively occurs in open, current‐swept channels in low‐lying areas between oo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______610::4f56530c4ec9a2899c6b4e110b6a37bb
https://publica.fraunhofer.de/handle/publica/265333
https://publica.fraunhofer.de/handle/publica/265333
Methane (CH4) production in the ocean surface mixed layer is a widespread but still largely unexplained phenomenon. In this context marine algae have recently been described as a possible source of CH4 in surface waters. In the present study we inves
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::652693ded607f53c64722f79b485b962
Publikováno v:
In Geochimica et Cosmochimica Acta 2007 71(9):2240-2249
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.