Zobrazeno 1 - 10
of 355
pro vyhledávání: '"C. Tamburini"'
Publikováno v:
Biogeosciences, Vol 20, Pp 4165-4182 (2023)
Through the constant rain of sinking marine particles in the ocean, carbon (C) trapped within is exported into the water column and sequestered when reaching depths below the mesopelagic zone. Atmospheric CO2 levels are thereby strongly related to th
Externí odkaz:
https://doaj.org/article/78cd0ebcdb554d4c886fe2915fdb6a45
Autor:
S. H. M. Jacquet, C. Tamburini, M. Garel, A. Dufour, F. Van Vambeke, F. A. C. Le Moigne, N. Bhairy, S. Guasco
Publikováno v:
Biogeosciences, Vol 18, Pp 5891-5902 (2021)
We report on the sub-basin variability in particulate organic carbon (POC) remineralization in the western and central Mediterranean Sea in late spring during the PEACETIME (ProcEss studies at the Air–sEa Interface after dust deposition in the MEdi
Externí odkaz:
https://doaj.org/article/a7b86cf5453d46b5a37290edfd5ca8ba
Autor:
F. Van Wambeke, E. Pulido, P. Catala, J. Dinasquet, K. Djaoudi, A. Engel, M. Garel, S. Guasco, B. Marie, S. Nunige, V. Taillandier, B. Zäncker, C. Tamburini
Publikováno v:
Biogeosciences, Vol 18, Pp 2301-2323 (2021)
Ectoenzymatic activity, prokaryotic heterotrophic abundances and production were determined in the Mediterranean Sea. Sampling was carried out in the sub-surface, the deep chlorophyll maximum layer (DCM), the core of the Levantine intermediate waters
Externí odkaz:
https://doaj.org/article/8bb6d4977a274155886d9aac9665ada5
Autor:
S. H. M. Jacquet, D. Lefèvre, C. Tamburini, M. Garel, F. A. C. Le Moigne, N. Bhairy, S. Guasco
Publikováno v:
Biogeosciences, Vol 18, Pp 2205-2212 (2021)
In the ocean, remineralization rate associated with sinking particles is a crucial variable. Since the 1990s, particulate biogenic barium (Baxs) has been used as an indicator of carbon remineralization by applying a transfer function relating Baxs to
Externí odkaz:
https://doaj.org/article/9c0e30fbaf554e6894e2a74b9b333c98
Publikováno v:
Biogeosciences, Vol 17, Pp 3757-3778 (2020)
Around 30 species of marine bacteria can emit light, a critical characteristic in the oceanic environment is mostly deprived of sunlight. In this article, we first review current knowledge on bioluminescent bacteria symbiosis in light organs. Then, f
Externí odkaz:
https://doaj.org/article/a425ae489e754f218f4846e362cc57f5
The complete classification of the finite simple groups that are $(2,3)$-generated is a problem which is still open only for orthogonal groups. Here, we construct $(2, 3)$-generators for the finite odd-dimensional orthogonal groups $\Omega_{2k+1}(q)$
Externí odkaz:
http://arxiv.org/abs/2306.02390
Autor:
K. Schroeder, C. Millot, L. Bengara, S. Ben Ismail, M. Bensi, M. Borghini, G. Budillon, V. Cardin, L. Coppola, C. Curtil, A. Drago, B. El Moumni, J. Font, J. L. Fuda, J. García-Lafuente, G. P. Gasparini, H. Kontoyiannis, D. Lefevre, P. Puig, P. Raimbault, G. Rougier, J. Salat, C. Sammari, J. C. Sánchez Garrido, A. Sanchez-Roman, S. Sparnocchia, C. Tamburini, I. Taupier-Letage, A. Theocharis, M. Vargas-Yáñez, A. Vetrano
Publikováno v:
Ocean Science, Vol 9, Iss 2, Pp 301-324 (2013)
The long-term monitoring of basic hydrological parameters (temperature and salinity), collected as time series with adequate temporal resolution (i.e. with a sampling interval allowing the resolution of all important timescales) in key places of the
Externí odkaz:
https://doaj.org/article/865a176f607c4852a41060fff2b22ae5
We construct $(2,3)$-generators for the finite $8$-dimensional orthogonal groups, proving the following results: the groups $\Omega_8^+(q)$ and $P\Omega_8^+(q)$ are $(2,3)$-generated if and only if $q\geq 4$; the groups $\Omega_8^-(q)$ and $P\Omega_8
Externí odkaz:
http://arxiv.org/abs/2201.00367
This paper is a new important step towards the complete classification of the finite simple groups which are $(2, 3)$-generated. In fact, we prove that the symplectic groups $Sp_{2n}(q)$ are $(2,3)$-generated for all $n\geq 4$. Because of the existin
Externí odkaz:
http://arxiv.org/abs/2005.10347
In this paper we prove that the unitary groups $SU_n(q^2)$ are $(2,3)$-generated for any prime power $q$ and any integer $n\geq 8$. By previous results this implies that, if $n\geq 3$, the groups $SU_n(q^2)$ and $PSU_n(q^2)$ are $(2,3)$-generated, ex
Externí odkaz:
http://arxiv.org/abs/1807.09270