Results 111 to 120 of about 29,169 (250)
Shallow-water benthic foraminifera as proxy for natural versus human-induced environmental change
Ecosystem composition and functioning is not only subjected to human-induced alterations, ecosystems also subjected to natural (e.g. climate-induced) variability.
de Nooijer, Lennart Jan +8 more
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(Uploaded by Plazi from the Biodiversity Heritage Library) No abstract provided.
openaire +1 more source
The Foraminifera of the Gault of Folkestone.—I [PDF]
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openaire +3 more sources
New bio‐sequence framework for the Eocene–Oligocene transition in Zagros. Geochemical data validate basin depth control on SB1 vs. SB2 boundaries. SEM‐EDS analyses confirm subaerial exposure versus continuous deposition. Sensitivity analysis quantifies sub‐10% uncertainty in stratigraphic interpretations. Resolves the Pyrenean orogeny's variable impact
Sahar Rokni +4 more
wiley +1 more source
Deep-water agglutinated foraminifera (DWAF) were studied from Cores PS2177-5, PS2200-5, PS2212-3 and PS2185-6; from the R/V POLARSTERN ARK-VIII/3 Cruise in the central Arctic Ocean.
Kaminski, M.A., Evans, J.R.
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Niue represents one of many important steppingstones facilitating the dispersal of marine organisms across the tropical Pacific Ocean. This study is part of a collaborative expedition involving National Geographic Pristine Seas, the government of Niue ...
Shai Oron +3 more
doaj +1 more source
This study deals with limitations of frequency domain reflectometry sensors, including data drift, when monitoring clayey soils with pedogenic carbonates. Despite these inaccuracies, the results demonstrate that corrected measurements of soil water content can still successfully calibrate hydrological models.
Katarina Matan +3 more
wiley +1 more source
Analysis of agglutinated benthic foraminifera from surface samples collected in the San Pedro and Santa Catalina Basins reveals a predictable relationship between the proportions of morphogroups with decreasing bottom water oxygen levels and with the ...
Holbourn, A.E.L. +3 more
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Abstract The turnover rate of microbial cells drops steeply by increasing depth in the seabed, in accordance with the decreasing rate of organic matter mineralization. Bacterial endospore formation and germination may take place concurrently, yet their coupling to the mineralization rates during burial is poorly understood.
Bo Barker Jørgensen +6 more
wiley +1 more source
Foraminifera vizsgálatok sajólászlófalvai miocén üledékben
Paleoökológiai rekonstrukció foraminifera vizsgáltaok alapján sajólászlófalvai középső miocén csillámos tengeri homokból ...
Fülöp, Norbert
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