Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Juliane Fenner"'
Publikováno v:
Diatom Research. 30:55-64
Vanhoeffenus antarcticus was described by Heinrich Heiden from a net sample taken from 385 m depth by the Gauss expedition (First German Antarctic Expedition) while frozen in pack ice near the Antarctic continent in the austral summer of 1902–3. Va
Autor:
C. Venegas, Carlos Marquardt, M. Marchant, Heather Middleton, Alain Lavenu, Christopher Gomez, Juliane Fenner, J.P. Le Roux, D. Frassinetti, Kathryn M. Gregory-Wodzicki, B. Buchbinder
Publikováno v:
JOURNAL OF SOUTH AMERICAN EARTH SCIENCES
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
The stratigraphy, sedimentology, and paleontology of the Coquimbo Formation in a coastal section approximately 100 km north of La Serena was studied to establish relative low-order sea-level changes during the Neogene. During the Early–Middle Mioce
Autor:
Agata Di Stefano, Juliane Fenner
Publikováno v:
Marine Geology. 205:59-86
A quantitative analysis was carried out of planktonic diatoms (biogenic opal) and calcareous nannofossils (biogenic calcite) in late Quaternary sediments (MIS 1–6) from four cores along a N–S transect east of New Zealand from 39°50′S to 50°04
Autor:
Juliane Fenner
Publikováno v:
Rendiconti online della Società Geologica Italiana. 31:73-74
Publikováno v:
Marine Geology. 108:383-404
Four cores from the lower northwestern flank (3010–3726 m water depth) of the Chatham Rise, east of New Zealand, penetrated a post-glacial to last glacial sequence of mainly hemipelagic muds. An accurate time frame for this study is provided by wel
Autor:
Sven N. Nielsen, Danisa M. Olivares, Heather Middleton, Juliane Fenner, Scott E. Ishman, Norman D. Smith, J.P. Le Roux
Publikováno v:
Sedimentary Geology
SEDIMENTARY GEOLOGY
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
SEDIMENTARY GEOLOGY
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
The north-facing Bay of Tongoy in central Chile is flanked by topographic highs in the west and east. During the Miocene and Pliocene, the bay extended inland at least 30 km farther south than a present. It was filled with muds, sands, coquinas and g
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::98e1f756dbf3f5972e4559193d4b459a
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:233792
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:233792
Publikováno v:
SEDIMENTARY GEOLOGY
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Exceptionally good outcrops of Miocene to Pliocene deposits in the vicinity of submarine Paleozoic basement scarps at Carrizalillo, north of La Serena, reveal a wealth of sedimentary features not commonly observed. The most proximal facies consist of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e7a7fc32877cb1ebbf621e4aeaf31176
Autor:
Fred Rögl, Juliane Fenner, Claus Heilmann-Clausen, Birger Schmitz, Reinhard F. Sachsenhofer, Hans Egger
Sediments in the expanded Anthering Section at the northwestern Tethyan margin were deposited in an abyssal environment, at the continental rise to the south of the European plate. The section contains deposits from calcareous nannoplankton Zones NP9
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fefe0ab454bf283549644f3907f6230e
https://doi.org/10.1130/0-8137-2369-8.133
https://doi.org/10.1130/0-8137-2369-8.133
Autor:
Torsten Bickert, M.-Z. Won, H. Beiersdorf, Juliane Fenner, N. Petersen, Pavel Čepek, W. Weiss, Joachim Schönfeld
Publikováno v:
Marine Geology, 125 (1-2). pp. 29-59.
An undisturbed 16 m late Pliocene-Pleistocene sediment core spanning 2.6 Myr of deposition was recovered from the Manihiki Plateau by the German research vessel Sonne in 1990. This core 34KL complements the heavily disturbed late Pliocene-Pleistocene
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c436f9d92a72ef7af6733e558fb4b5d2
http://oceanrep.geomar.de/31249/
http://oceanrep.geomar.de/31249/