Four Governors of the Arquebusiers' Civic Guard, Amsterdam

Govert Flinck; 6 ft. 7 59/64 in.x 9 ft. 1 29/64 in.; oil on canvas

Gas hydrate investigation at the Amsterdam mud volcano

We investigated gas hydrate in situ inventories as well as the composition and principal transport mechanisms of fluids expelled at the Amsterdam mud volcano (AMV; 2,025 m water depth) in the Eastern Mediterranean Sea. Pressure coring (the only technique preventing hydrates from decomposition during recovery) was used for the quantification of light hydrocarbons in near-surface deposits. The cores (up to 2.5 m in length) were retrieved with an autoclave piston corer, and served for analyses of gas quantities and compositions, and pore-water chemistry. For comparison, gravity cores from sites at the summit and beyond the AMV were analyzed. A prevalence of thermogenic light hydrocarbons was inferred from average C1/C2+ ratios <35 and d13C-CH4 values of -50.6 per mil. Gas venting from the seafloor indicated methane oversaturation, and volumetric gas-sediment ratios of up to 17.0 in pressure cores taken from the center demonstrated hydrate presence at the time of sampling. Relative enrichments in ethane, propane, and iso-butane in gas released from pressure cores, and from an intact hydrate piece compared to venting gas suggest incipient crystallization of hydrate structure II (sII). Nonetheless, the co-existence of sI hydrate can not be excluded from our dataset. Hydrates fill up to 16.7% of pore volume within the sediment interval between the base of the sulfate zone and the maximum sampling depth at the summit. The concave-down shapes of pore-water concentration profiles recorded in the center indicate the influence of upward-directed advection of low-salinity fluids/fluidized mud. Furthermore, the SO42- and Ba2+ pore-water profiles in the central part of the AMV demonstrate that sulfate reduction driven by the anaerobic oxidation of methane is complete at depths between 30 cm and 70 cm below seafloor. Our results indicate that methane oversaturation, high hydrostatic pressure, and elevated pore-water activity caused by low salinity promote fixing of considerable proportions of light hydrocarbons in shallow hydrates even at the summit of the AMV, and possibly also of other MVs in the region. Depending on their crystallographic structure, however, hydrates will already decompose and release hydrocarbon masses if sediment temperatures exceed ca. 19.3°C and 21.0°C, respectively. Based on observations from other mud volcanoes, the common occurrence of such temperatures induced by heat flux from below into the immediate subsurface appears likely for the AMV.

Compte rendu de Kockaert, Hendrik J. & Steurs, Frieda (Eds.). (2015). Handbook of terminology (HOT), vol. 1. Amsterdam: Benjamins, 558 p.

Paru dans Parallèles 28/2, p. 105-108

New 9-Terpenyl(7-Terpenyl)Purines: synthesis and cytotoxicity

The purine ring system is one of the most widely distributed N-heterocycles in Nature [1] and many structurally modified purine nucleosides and nucleotides have activities ranging from antineoplastic and antiviral to antihypertensive, antiasthmatic, antituberculosis, etc [2]. Among the purine derivatives, we have put our attention on natural N-alkylpurines such as the asmarines or agelasimines, a group of secondary metabolites isolated from marine sponges with very interesting biological properties [3]. They have a diterpenoid moiety attached to the N-7 nitrogen atom of an adenine and are usually isolated in very small quantities, which limited their structure-activity relationship studies. Our research group has been involved for years in the design, synthesis and biological evaluation of cytotoxic compounds related to natural products, including the chemoinduction of bioactivity on inactive terpenoids [4]. These diterpenoid include compounds such as communic or cupressic acids that bear decaline moieties very close to those present in the above-mentioned marine natural products. These facts prompted us to design and prepare new terpenylpurine derivatives starting from natural monoterpenoids and diterpenoids, commercially available or isolated from their natural sources and transformed into appropriate alkylated agents. Thus, we have prepared purines alkylated at N-7 and N-9 positions with isoprenoids, monoterpenoids and diterpenoids, using two different synthetic approaches: from 6-chloropurine or from 4,5-diamine-6-chloropyrimidine. The structure of the synthesized purines are shown in the following figure. The purine analogues synthesized have been evaluated for their cytotoxicity against four tumour human cell lines (breast, non-small lung, cervical and hepatocellular carcinoma) and non-tumour cells (porcine liver primary cells). The most cytotoxic derivatives were those with a diterpenoid rest on the purine. The results obtained allowed to draw conclusions on the structure-activity relationship of the compounds in order to evaluate the influence of the terpenyl size on their cytotoxic properties.

8-Ammonionaphthalene-2-sulfonate monohydrate : the zwitterionic hydrate of 1,7-Cleve's acid

The structure of 8-amino-2-naphthalenesulfonic acid monohydrate (1,7-Cleve's acid hydrate), C10H9NO3S.H2O, shows the presence of a sulfonate-aminium group zwitterion, both groups and the water molecule of solvation giving cyclic R3/3(8) intermolecular hydrogen-bonding interactions forming chains which extend down a axis of the unit cell. Additional peripheral associations, including weak aromatic ring pi-pi interactions [centroid-centroid distance 3.6299(15)A], result in a two-dimensional sheet structure.