Zobrazeno 1 - 7
of 7
pro vyhledávání: '"J. M. van Iperen"'
Autor:
J. M. van Iperen, Geert-Jan A Brummer, Erica Koning, W. Helder, W van Raaphorst, T.C.E. van Weering
Publikováno v:
Deep Sea Research Part I: Oceanographic Research Papers. 48:2473-2495
The diatom species composition of settling biogenic silica particles collected in sediment traps was compared with the underlying sediment to determine the preservation of the various diatom species and to investigate the potential of biogenic silica
Publikováno v:
Hydrobiologia. :113-128
Autor:
J.H.F. Jansen, J. M. Van Iperen
Publikováno v:
Paleoceanography. 6:573-591
Accumulation rates of microfossil associations are independent of each other and, in addition to percentages, give indispensable information about the significance of micropaleontological data. Marine diatoms reveal that coastal upwelling in the Zair
Publikováno v:
Twelfth International Diatom Symposium ISBN: 9789048143245
Diatoms from 53 surface sediments (water depth 350–7200 m) of the Indonesian Archipelago were studied to determine the recent distribution of important assemblages. Three significant assemblages were distinguished, each related to hydrographie para
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::439a1c91d96f2efbf7f55a96763c38cb
https://doi.org/10.1007/978-94-017-3622-0_14
https://doi.org/10.1007/978-94-017-3622-0_14
Autor:
T.C.E. van Weering, J. M. van Iperen
Publikováno v:
Geological Society, London, Special Publications. 15:95-113
Publikováno v:
Netherlands Journal of Sea Research. 21:203-217
A study of 25 surface sediment samples from the Zaire (Congo) deep-sea fan in the southeastern Atlantic Ocean shows that 6 diatom groups can be distinguished by their distribution patterns. Two groups occur exclusively in shelf and slope deposits, 3
Publikováno v:
Radiocarbon. 31:557-569
Maps of accumulation rates of freshwater diatoms and opal phytoliths in the surface sediments of the Zaire fan show that both types of microfossils were supplied to the ocean floor by the Zaire River, and that opal phytoliths also have a southern sou