Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Diana, Menzel"'
Autor:
Samuel Tessier, Alexandre Lambion, Anatoly Peretyatko, Wim Vyverman, Laurent Viroux, Peter Vanormelingen, Bruno Leporcq, Diana Menzel, Geoffrey A. Codd, Jeroen Van Wichelen, Kathleen Van der Gucht, Aleksandra Wojnicz, Jean-Pierre Descy, Marianne Reilly, Gisèle Verniers, Yannick Lara, Ludwig Triest, Samuel Pirlot, Aaike De Wever, Annick Wilmotte
Publikováno v:
Freshwater Metadata Journal. :1-8
Publikováno v:
Aquatic Microbial Ecology. 69:135-143
Publikováno v:
Toxicon. 54:887-890
Cyanobacteria produce a wide range of potent toxins, including hepatotoxic microcystins. HPLC methods for microcystin analysis and purification almost invariably include acetonitrile in the elution gradient mobile phase. The recent, acute, global ace
Publikováno v:
Organic Geochemistry. 36:1037-1053
The organic matter of three time-equivalent Pliocene sapropels was characterized as being predominantly Type II kerogen using RockEval pyrolysis. It is dominated by amorphous organic matter, originating mainly from marine organisms, as indicated by t
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 190:273-287
Biomarkers (alkenones, loliolide/isololiolide, dinosterol and C30 1,15-diol/keto-ol) representative of four major classes of marine primary producers (haptophytes, diatoms, dinoflagellates, eustigmatophytes, respectively) from three sites of an east
Autor:
Jeroen, Van Wichelen, Ineke, Van Gremberghe, Pieter, Vanormelingen, Ann-Eline, Debeer, Bruno, Leporcq, Diana, Menzel, Geoffrey A, Codd, Jean-Pierre, Descy, Wim, Vyverman
Publikováno v:
Environmental microbiology. 12(10)
Despite its importance for bloom toxicity, the factors determining the population structure of cyanobacterial blooms are poorly understood. Here, we report the results of a two-year field survey of the population dynamics of Microcystis blooms in a s
Publikováno v:
Marine Geology, 189(3-4), 215. Elsevier
Carotenoids were analysed in ca. 1-cm thick subsamples of three laterally time-equivalent sapropels from a west–east transect of the eastern Mediterranean Basin to study euxinic periods during Pliocene sapropel formation. The amount of intact isore
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ef9288dd7b1053cac79ebb9d63e5dcdb
https://dspace.library.uu.nl/handle/1874/4278
https://dspace.library.uu.nl/handle/1874/4278