Zobrazeno 1 - 10
of 1 251
pro vyhledávání: '"T Tyrrell"'
Autor:
Jedid-Jah Jonker
Publikováno v:
Beleidsonderzoek Online.
Publikováno v:
Biogeosciences, Vol 17, Pp 2289-2314 (2020)
The nutrient composition (high in nitrate but low in silicate) of Subantarctic Mode Water (SAMW) forces diatom scarcity across much of the global surface ocean. This is because diatoms cannot grow without silicate. After formation and downwelling at
Externí odkaz:
https://doaj.org/article/d68f8a1d351d4394a9347f61b83fab5b
What drives the latitudinal gradient in open-ocean surface dissolved inorganic carbon concentration?
Publikováno v:
Biogeosciences, Vol 16, Pp 2661-2681 (2019)
Previous work has not led to a clear understanding of the causes of spatial pattern in global surface ocean dissolved inorganic carbon (DIC), which generally increases polewards. Here, we revisit this question by investigating the drivers of observed
Externí odkaz:
https://doaj.org/article/3c34a73b9b404803b88b14a419a34938
Autor:
C. J. Daniels, A. J. Poulton, W. M. Balch, E. Marañón, T. Adey, B. C. Bowler, P. Cermeño, A. Charalampopoulou, D. W. Crawford, D. Drapeau, Y. Feng, A. Fernández, E. Fernández, G. M. Fragoso, N. González, L. M. Graziano, R. Heslop, P. M. Holligan, J. Hopkins, M. Huete-Ortega, D. A. Hutchins, P. J. Lam, M. S. Lipsen, D. C. López-Sandoval, S. Loucaides, A. Marchetti, K. M. J. Mayers, A. P. Rees, C. Sobrino, E. Tynan, T. Tyrrell
Publikováno v:
Earth System Science Data, Vol 10, Pp 1859-1876 (2018)
The biological production of calcium carbonate (CaCO3), a process termed calcification, is a key term in the marine carbon cycle. A major planktonic group responsible for such pelagic CaCO3 production (CP) is the coccolithophores, single-celled ha
Externí odkaz:
https://doaj.org/article/019f51949ba14bbe9d40e0fc388fa6f8
Autor:
A. Charalampopoulou, A. J. Poulton, D. C. E. Bakker, M. I. Lucas, M. C. Stinchcombe, T. Tyrrell
Publikováno v:
Biogeosciences, Vol 13, Iss 21, Pp 5917-5935 (2016)
Although coccolithophores are not as numerically common or as diverse in the Southern Ocean as they are in subpolar waters of the North Atlantic, a few species, such as Emiliania huxleyi, are found during the summer months. Little is actually known a
Externí odkaz:
https://doaj.org/article/2cc39b0d2ff14342b9c03366fc64a0d2
Autor:
T. Tyrrell, E. P. Achterberg
Publikováno v:
Biogeosciences, Vol 11, Iss 24, Pp 7269-7274 (2014)
Externí odkaz:
https://doaj.org/article/65b49ad42ec44b95a449c678aa246f51
Autor:
S. Richier, E. P. Achterberg, C. Dumousseaud, A. J. Poulton, D. J. Suggett, T. Tyrrell, M. V. Zubkov, C. M. Moore
Publikováno v:
Biogeosciences, Vol 11, Iss 17, Pp 4733-4752 (2014)
The ongoing oceanic uptake of anthropogenic carbon dioxide (CO2) is significantly altering the carbonate chemistry of seawater, a phenomenon referred to as ocean acidification. Experimental manipulations have been increasingly used to gauge how conti
Externí odkaz:
https://doaj.org/article/53ba3449192544d99a5fed336ce80889
Publikováno v:
Biogeosciences, Vol 11, Iss 17, Pp 4771-4782 (2014)
Within the context of the UK Ocean Acidification project, Emiliania huxleyi (type A) coccolith morphology was examined from samples collected during cruise D366. In particular, a morphometric study of coccolith size and degree of calcification was ma
Externí odkaz:
https://doaj.org/article/e4c812c135994d0c908a9591a4fcfe70
Autor:
M. Ribas-Ribas, V. M. C. Rérolle, D. C. E. Bakker, V. Kitidis, G. A. Lee, I. Brown, E. P. Achterberg, N. J. Hardman-Mountford, T. Tyrrell
Publikováno v:
Biogeosciences, Vol 11, Iss 16, Pp 4339-4355 (2014)
Four carbonate system variables were measured in surface waters during a cruise aimed at investigating ocean acidification impacts traversing northwestern European shelf seas in the summer of 2011. High-resolution surface water data were collected fo
Externí odkaz:
https://doaj.org/article/ed6be4cf09624a7c91da5ad57b613f43
Autor:
G. A. MacGilchrist, T. Shi, T. Tyrrell, S. Richier, C. M. Moore, C. Dumousseaud, E. P. Achterberg
Publikováno v:
Biogeosciences, Vol 11, Iss 13, Pp 3695-3706 (2014)
It has been proposed that increasing levels of pCO2 in the surface ocean will lead to more partitioning of the organic carbon fixed by marine primary production into the dissolved rather than the particulate fraction. This process may result in enhan
Externí odkaz:
https://doaj.org/article/7c2223ed5ffa419383f373a6423b43ac