The geologic emissions of greenhouse gases (CO2 and CH4) have an important natural contribution in the globalcarbon budget. Tectonics, through faults in geothermal and oil producing areas, play a significant role in the release ofC-gases in many non-volcanic regions of the Earth. Methane, the most abundant organic compound in Earth’satmosphere, has a potential global warming that is 28 times higher than that of CO2 on a 100-year time horizon. In thisstudy, δ13C-CH4, δ2H-CH4 and light hydrocarbon (alkane: CH4, C2H6, C3H8, C3H6, i-C4H10, n-C4H10; alkene C3H6, iC4H8; and aromatic C6H6) gas concentration data of 119 gas samples (103 unpublished data and 16 literature data) fromvolcanic-hydrothermal, geothermal and cold discharges are used to shed light on the genetic processes that have formedCH4 in the complex geodynamic setting of Greece. On the basis of the spatial distribution of the gas discharges andtheir type of emission, the whole dataset was subdivided into 4 main “domains”, as follows: 1) Volcanic Arc (VA); 2)External Hellenides (EH); 3) Internal Hellenides (IH); 4) Hellenic Hinterland (HH). Almost each group is characterized,as long as subdivided, in 3 groups based on the type of emission (on-land free or dissolved gases and submarine gases)and a 4th group includes literature data. Concentrations of CH4 range from < 2 to 925,200 µmol/mol and its isotopicratios cover a wide range (δ13C from -79.8 ‰ to +45 ‰; δ2H from -311 ‰ to +301 ‰) indicating the different primarysources and the secondary post-genetic processes (oxidation) that can significantly affect the origin of this gascompound. Hydrocarbons in the CH4-dominated gases discharged from the EH are showing a clear biotic origin. Inparticular, those collected in the Gavrovo-Tripolis zone are showing a dominating biotic origin, whereas it is alsonoticeable that some gas samples of the Ionian zone are produced by both microbial activity and thermal maturation ofsedimentary organic matter. The CO2-dominated gas discharges from the main geothermal systems of the IH and fromthe VA most likely predominantly contain abiogenic CH4 deriving from CO2 reduction. However, some of the gasdischarges of the geothermal and volcanic-hydrothermal systems located in the neritic sedimentary Pelagonian,Gavrovo-Tripolis and Attico-cycladic zones (IH) and in Rhodope massif (HH), seem to exhibit significant contributionsfrom thermogenic sources. The presence of abiotic methane was also recognized in the hyperalkaline aqueous solutionsthat are issuing from the ophiolites of Othrys and Argolida (Pindos zone (EH)). Most of the geothermal gases ofSubpelagonian and Vardar/Axios zones (IH), the cold manifestations of the Rhodope massif (HH) and some of thevolcanic-hydrothermal ones of the Attico-cycladic zone (VA) are presenting a microbial oxidation of CH4.
|Numero di pagine||1|
|Stato di pubblicazione||Published - 2017|