Zobrazeno 1 - 10
of 10
pro vyhledávání: '"D. R. Gröcke"'
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-9 (2023)
Abstract Macroalgae is an under-utilised tool as a bioindicator of anthropogenic nitrogen loading to the coastal environment in the UK. This study compared two island systems—Jersey (Channel Islands) and St Mary’s (Isles of Scilly) to assess how
Externí odkaz:
https://doaj.org/article/92234c684eed4968b37200fa74546238
Autor:
E. L. McClymont, M. J. Bentley, D. A. Hodgson, C. L. Spencer-Jones, T. Wardley, M. D. West, I. W. Croudace, S. Berg, D. R. Gröcke, G. Kuhn, S. S. R. Jamieson, L. Sime, R. A. Phillips
Publikováno v:
Climate of the Past, Vol 18, Pp 381-403 (2022)
Antarctic sea ice is a critical component of the climate system affecting a range of physical and biogeochemical feedbacks and supporting unique ecosystems. During the last glacial stage, Antarctic sea ice was more extensive than today, but uncertain
Externí odkaz:
https://doaj.org/article/3f878391848842cc8e1e1dace712a02e
Autor:
C. Rocha, C. Veiga-Pires, J. Scholten, K. Knoeller, D. R. Gröcke, L. Carvalho, J. Anibal, J. Wilson
Publikováno v:
Hydrology and Earth System Sciences, Vol 20, Iss 8, Pp 3077-3098 (2016)
Natural radioactive tracer-based assessments of basin-scale submarine groundwater discharge (SGD) are well developed. However, SGD takes place in different modes and the flow and discharge mechanisms involved occur over a wide range of spatial and te
Externí odkaz:
https://doaj.org/article/388a3466202045d194cf5bcfebdff108
Autor:
N. A. G. M. van Helmond, A. Sluijs, N. M. Papadomanolaki, A. G. Plint, D. R. Gröcke, M. A. Pearce, J. S. Eldrett, J. Trabucho-Alexandre, I. Walaszczyk, B. van de Schootbrugge, H. Brinkhuis
Publikováno v:
Biogeosciences, Vol 13, Iss 9, Pp 2859-2872 (2016)
Oceanic Anoxic Event 2 (OAE2), a ∼ 600 kyr episode close to the Cenomanian–Turonian boundary (ca. 94 Ma), is characterized by relatively widespread marine anoxia and ranks amongst the warmest intervals of the Phanerozoic. The early stages of OAE2
Externí odkaz:
https://doaj.org/article/9edad019019c475bad3296d6f18b27d3
Publikováno v:
Royal Society Open Science, Vol 3, Iss 5 (2016)
Owing to Rhenium (Re) having no known biological role, it is not fully understood how Re is concentrated in oil kerogens. A commonly held assumption is that Re is incorporated into decomposing biomass under reducing conditions. However, living macroa
Externí odkaz:
https://doaj.org/article/3add30afaac44481a92d60ccb6c2357c
Publikováno v:
Solid Earth, Vol 2, Iss 2, Pp 245-257 (2011)
Oceanic anoxic events were time intervals in the Mesozoic characterized by widespread distribution of marine organic matter-rich sediments (black shales) and significant perturbations in the global carbon cycle. These perturbations are globally recor
Externí odkaz:
https://doaj.org/article/1d9e111aa58c460d9c96c448c50c681d
Publikováno v:
Solid Earth, Vol 2, Iss 2, Pp 107-123 (2011)
Vintage 2-D (two-dimensional) seismic reflection surveys from the sparsely explored Mentelle Basin (western Australian margin) have been reprocessed and integrated with a recent high-quality 2-D seismic survey and stratigraphic borehole data. Interpr
Externí odkaz:
https://doaj.org/article/6fa1b178c877438ba8e49d1ba97ddf38
Autor:
S E, Groves, C A, Roberts, S, Lucy, G, Pearson, D R, Gröcke, G, Nowell, C G, Macpherson, G, Young
Publikováno v:
American journal of physical anthropology. 151(3)
Early Medieval England is described historically as a time when people migrated from the Continent to English shores. This study tests the hypothesis that those buried in the Bowl Hole cemetery, Bamburgh, Northumberland were nonlocally born, because
Oceanic anoxic events were time intervals in the Mesozoic characterized by widespread distribution of marine organic-rich sediments (black shales) and significant perturbations in the global carbon cycle. The expression of these perturbations is glob
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7a9e73d76cc42917574a90444070818f
https://doi.org/10.5194/sed-3-385-2011
https://doi.org/10.5194/sed-3-385-2011