This file was created by the TYPO3 extension publications --- Timezone: CEST Creation date: 2026-06-03 Creation time: 05:09:50 --- Number of references 42 article Kondrashova202590 Article 2025 10.1134/S0024490224700792 Lithology and Mineral Resources 60 90 – 113 1 https://www.scopus.com/inward/record.uri?eid=2-s2.0-85219676923&doi=10.1134%2fS0024490224700792&partnerID=40&md5=edd1794faa1bfa9d4c4056d2422627b9 Cited by: 0 N.I. Kondrashova P.V. Medvedev A.V. Lyutikov article Koeberl2024 Article 2024 10.1016/j.precamres.2024.107511 Precambrian Research 411 https://www.scopus.com/inward/record.uri?eid=2-s2.0-85199011245&doi=10.1016%2fj.precamres.2024.107511&partnerID=40&md5=22998621e16fab640511fd8ef4648ec4 Cited by: 0; All Open Access, Hybrid Gold Open Access Christian Koeberl Toni Schulz Matthew S. Huber article stueken2022hydrothermal 2022 Astrobiology Mary Ann Liebert, Inc., publishers 140 Huguenot Street, 3rd Floor New~… Eva E Stüeken Kalle Kirsimäe Aivo Lepland Anthony R Prave article qu2020hydrothermal 2020 Precambrian Research 343 Elsevier 105705 Yuangao Qu Mark A Zuilen Aivo Lepland article qu2018sample 2018 Precambrian Research 315 Elsevier 222--231 Yuangao Qu Aivo Lepland Mark A Zuilen Martin Whitehouse Alenka E {\v{C}}rne Anthony E Fallick article mougel2017chromium 2017 Earth and Planetary Science Letters 460 Elsevier 105--111 Bérengère Mougel Frédéric Moynier Christa Göpel article sharkov2017magmatic 2017 Geoscience Frontiers 8 Elsevier 621--640 4 E Sharkov M Bogina A Chistyakov incollection medvedev2016application Paleoproterozoic (2.0–2.2 Ga) stromatolites from drill cores of the ICDP Project FAR DEEP were studied by Raman spectroscopy and inductively coupled plasma mass spectrometry with laser ablation (LA-ICP MS) methods. Morphological features of the studied Paleoproterozoic stromatolites together with identification of synsedimentary carbonaceous matter by Raman spectroscopy are strong argument for biogenic origin of these carbonate buildups. Precision geochemical analysis of the stromatolite laminae composition links to sedimentary settings and environmental conditions of the microbialite formation. © 2016, Springer International Publishing Switzerland. 2016 English 21938571 10.1007/978-3-319-24987-2_26 Biogenic—Abiogenic Interactions in Natural and Anthropogenic Systems Lecture Notes in Earth System Sciences Springer 329--341 Institute of Geology, Karelian Research Centre, Russian Academy of Sciences, Petrozavodsk, Russian Federation 9783319249858 carbonate sediment; environmental conditions; geochemistry; inductively coupled plasma method; microbialite; Proterozoic; Raman spectroscopy; stromatolite, Baltic Shield; East European Craton https://www.scopus.com/inward/record.uri?eid=2-s2.0-85031924397&doi=10.1007%2f978-3-319-24987-2_26&partnerID=40&md5=61a51529fa2738c9bec6b15e8d33fbc9 cited By 1 Pavel V Medvedev Svetlana Y Chazhengina Sergey A Svetov article joosu2016petrography 2016 Geochimica et Cosmochimica Acta 186 Elsevier 135--153 Lauri Joosu Aivo Lepland Timmu Kreitsmann Kärt Üpraus Nick MW Roberts Päärn Paiste Adam P Martin Kalle Kirsimäe article Fallick2016224 A variety of carbonates of different geneses, as indicated by petrography and geochemistry, are found throughout 400 m of the volcano-sedimentary rocks of the Zaonega Formation of Palaeoproterozoic age in the Onega basin of Fennoscandia. Following intensive sampling and analysis of varied calcites from drillcore recovered during the ICDP FAR-DEEP program, we report a highly unusual depth distribution of calcite oxygen isotope values (δ18Ocal). Unprecedentedly for such rocks, the δ18Ocal values over the full depth interval of 400 m are strongly linearly correlated with depth (r2 = 0.9015, n = 178). We propose that this is the result of major oxygen isotope resetting through water–rock interaction with a fluid of relatively constant oxygen isotopic composition (δ18Ow). In this model, the observed linear δ18Ocal-depth relationship is then a consequence of the increase in temperature with depth because of the background geothermal gradient. Minor deviations from the overall linear trend are likely due to bed-scale geological factors including locally high impermeability, and oxygen isotope modification of δ18Ow by comparatively intense water–rock interaction. Were the observed δ18Ocal values to have been reset during the greenschist facies Svecofennian metamorphism which affected the rocks at c. 1800 Ma, the implied geothermal gradient of ∼560 °C km−1 is geologically unreasonable and, accordingly, this hypothesis is ruled out. Rather, the δ18Ocal variation of 5‰ over 400 m implies a near-surface depth for the rocks during fluid interaction, and this is consistent with a surface-derived origin of the infiltrating fluid (δ18Ow ∼−13.6‰ for a surface temperature of 15 °C and geothermal gradient of ∼52 °C km−1). It is speculated that the fluid accessed the carbonates from the basin edge by bed-parallel rather than cross-formational flow. There is an intriguing distribution of Na in the sedimentary rocks of the Zaonega Formation. Sodium is relatively abundant in rocks below a certain depth (the lowermost dolostone at ∼258 m), but rare in shallower sequences. It is argued that this distribution did not originate with the basin-scale fluid–rock interaction documented above, but may rather be the result of evaporite dissolution, and subsequent redistribution of soluble elements during fluid flow associated with the syndepositional emplacement of basin-wide igneous rocks. © 2016 Elsevier B.V. Article 2016 English 03019268 10.1016/j.precamres.2016.06.001 Precambrian Research 281 Elsevier B.V. 224 – 235 Isotope Geosciences Unit, SUERC, Rankine Avenue, East Kilbride G75 0QF, Scotland, United Kingdom; Norwegian Geological Survey, Leif Eirikssons vei 39, Trondheim, N-4791, Norway; School of Geosciences, Meston Building, University of Aberdeen, Old Aberdeen AB24 3UE, Scotland, United Kingdom; Department of Earth and Environmental Sciences, St. Andrews University, St. Andrews, Fife KY16 9ALScotland, United Kingdom calcite; carbonate; diagenesis; geothermal gradient; oxygen isotope; Proterozoic; water-rock interaction, Arkhangelsk [Russian Federation]; Fennoscandia; Onega Basin; Russian Federation https://www.scopus.com/inward/record.uri?eid=2-s2.0-84991641456&doi=10.1016%2fj.precamres.2016.06.001&partnerID=40&md5=b9507d0407235e6ff3cec62dade7994a Cited by: 6 A.E. Fallick V.A. Melezhik A.T. Brasier A.R. Prave article melezhik2015carbonate Several deep drillholes were made in the Onega palaeobasin by the Fennoscandian Arctic Russia-Drilling Early Earth Project (FAR-DEEP) of the International Continental Scientific Drilling Program (ICDP). These provided fresh core material documenting the Lomagundi-Jatuli Isotopic Event (LJIE), its termination, and the start of the Shunga Event (SHE) of an enhanced accumulation of organic matter. The cored section represents the most complete known record of the end of the LJIE.The late phase of the LJIE, recorded in FAR-DEEP Core 11A, is represented by the upper part of the Tulomozero Formation (TF), a 300-m-thick unit composed of variegated dolostones, siltstones and shales. Accumulated under oxic conditions on a shallow-water carbonate platform, the TF hosts the earliest known thick formations of halite and massive anhydrite. Low-temperature greenschist facies metamorphism caused partial recrystallisation of the rocks; however, a primary carbonate phase, the dolomite, exhibits a negligible degree of post-depositional alteration of the carbon isotope system. The dataset of 46 bulk-carbonate analyses of carbon and oxygen isotopes yielded δ13Ccarb ranging between +6.8 and +11.8‰, and revealed a positive excursion from +8 to +11.8‰ followed by a decline to +8‰ towards the top of the 300-m-thick succession.The cored part of the overlying Zaonega Formation (ZF) recovered in holes 12AB and 13A is an 800-m-thick unit composed of mixed siliciclastic-carbonate facies with numerous mafic lava flows and tuff beds intruded by gabbro sills. The formation represents an unprecedented episode of enhanced accumulation of organic-rich rocks and preserves the earliest known supergiant, petrified oilfield, all typifying the SHE. The sedimentological, petrographic, geochemical and C- and O-isotopic study of over 800m of core throughout the ZF suggests that the initial carbonate deposition occurred in a lacustrine environment, then rapidly proceeding through a lagoonal setting to a rifted deepwater shelf, and finally to a carbonate platform. Both the deepwater shelf and the platformal settings are marked by organic-rich environments. The primary dolomite was potentially exposed to syn- and post-depositional hydrothermal/metasomatic alterations, organic matter diagenesis, metamorphic mineral reactions, CO2 degassing, and finally a low-temperature, post-metamorphic calcitisation resulting in overall large fluctuations of δ13Ccarb between -22 and +8‰. The dataset of over 413 bulk-carbonate analyses of carbon and oxygen isotopes, screened petrographically and geochemically against post-depositional alteration, revealed 28 least-altered samples within three stratigraphic intervals, suggesting multiple positive and negative δ13Ccarb excursions throughout over 1000m of stratigraphy. A shift from +5 to +9‰ followed by a drop to near zero values marks the lower part of the ZF. A δ13Ccarb decline from +8‰ to below zero in the middle and upper part of the ZF defines the end of the LJIE. A subsequent prominent negative excursion down to -6‰ does not show convincing isotopic evidence for influence of methanogenesis, and hence appears to be of primary depositional origin. An erratic positive excursion in the uppermost part of the drilled section indicates return of δ13Ccarb to a near normal marine value. © 2015 Elsevier B.V. 2015 English 00128252 10.1016/j.earscirev.2015.05.005 Earth-Science Reviews 147 Elsevier 65--98 Geological Survey of Norway, Postboks 6315 Slupen, Trondheim, NO-7491, Norway; Scottish Universities Environmental Research Centre, Rankine Avenue, East Kilbride, Scotland, G75 0QF, United Kingdom; University of Aberdeen, Department of Geology and Petroleum Geology, Meston Building, Scotland, AB24 3UE, United Kingdom bitumen; carbon isotope; carbonate platform; depositional environment; dolomite; lithostratigraphy; organic matter; Proterozoic; sediment core, Arkhangelsk [Russian Federation]; Fennoscandia; Onega Basin; Russian Federation https://www.scopus.com/inward/record.uri?eid=2-s2.0-84930225434&doi=10.1016%2fj.earscirev.2015.05.005&partnerID=40&md5=06df153c1676b4786b9faf481f77f453 cited By 26 Victor A Melezhik Anthony E Fallick Alexander T Brasier Aivo Lepland article martin2015multiple 2015 Earth and Planetary Science Letters 424 Elsevier 226--236 Adam P Martin AR Prave DJ Condon Aivo Lepland Anthony E Fallick AE Romashkin PV Medvedev DV Rychanchik article gartner2014dating 2014 Precambrian Research 246 Elsevier 281--295 Claudia Gärtner Heinrich Bahlburg Victor A Melezhik Jasper Berndt article hanski2014new 2014 Precambrian Research 245 Elsevier 51--65 Eero J Hanski Hannu Huhma Victor A Melezhik article salminen2014travertine 2014 Precambrian Research 255 Elsevier 181--201 PE Salminen AT Brasier JA Karhu VA Melezhik article Salminen2013177 Article 2013 10.1016/j.precamres.2013.01.005 Precambrian Research 228 177 – 193 https://www.scopus.com/inward/record.uri?eid=2-s2.0-84873932514&doi=10.1016%2fj.precamres.2013.01.005&partnerID=40&md5=91b80fab323a97fb07dab21bd720d912 Cited by: 5 Paula E. Salminen Juha A. Karhu Victor A. Melezhik article salminen2013tracking 2013 Precambrian Research 228 Elsevier 177--193 Paula E Salminen Juha A Karhu Victor A Melezhik article Salminen2013165 Article 2013 10.1016/j.chemgeo.2013.10.018 Chemical Geology 362 165 – 180 https://www.scopus.com/inward/record.uri?eid=2-s2.0-84889086602&doi=10.1016%2fj.chemgeo.2013.10.018&partnerID=40&md5=43c6d80e95f32ca76d77e78cef2794f9 Cited by: 5 Paula E. Salminen Juha A. Karhu Victor A. Melezhik article salminen2013kolosjoki 2013 Chemical Geology 362 Elsevier 165--180 Paula E Salminen Juha A Karhu Victor A Melezhik article Lepland2013493 2013 English 9783642296581 18634621 10.1007/978-3-642-29659-8_1 Frontiers in Earth Sciences 7 Frontiers 493-502 Geological Survey of Norway, Postboks 6315 Sluppen, Trondheim NO-7491, Norway https://www.scopus.com/inward/record.uri?eid=2-s2.0-84871054257&doi=10.1007%2f978-3-642-29659-8_1&partnerID=40&md5=0313de5e5e42fd5e2d25237e44208348 cited By 2 A. Lepland M. Mesli R. Conze K. Fabian A.E. Fallick L.R. Kump article brasier2013earth As part of the International Continental Scientific Drilling Program's Fennoscandian Arctic Russia-Drilling Early Earth Project (ICDP FAR-DEEP), Palaeoproterozoic diamictic and associated rocks were targeted and recovered in Hole 3A on the Kola Peninsula of NW Russia. In addition to the diamictites, carbonate sedimentary rocks and volcanic ash layers (all metamorphosed to greenschist grade) were encountered. Sedimentology and geochemistry suggest deposition of the diamictites in an open-marine aragonite-precipitating environment. Sampling of the core and of outcrops from the same geographical area yielded a number of zircons for analyses, the majority of which were inherited. However a tuff at 20.01m core depth yielded zircons dated at 2434±1.2Ma (±6.6Myr including decay constant uncertainties) that we interpret as a magmatic age. These data, combined with dates from underlying intrusions, indicate deposition of the Polisarka Sedimentary Formation diamictites and underlying carbonates during an interval of time from ca. 2430 to 2440Ma. The carbonate rocks, which likely originally included aragonitic limestones, were deposited mostly in a deep-water setting (i.e. at least below storm wave base) and occur below the diamictite. They record two inorganic carbon δ13C excursions, from values of ca. 0‰ to minima of ca. -5.4‰, as the contact with the overlying diamictite is approached. The older (stratigraphically lower) excursion occurs about 9m below the base of the diamictic units and the younger one at 1m below. Throughout that interval, Mg/Ca ratios correlate strongly with δ13C (n=38, r=0.85), and combined with petrographic observations, this indicates that the first (stratigraphically lower) excursion was modified by secondary alteration and the second is recorded in resedimented dolostone clasts. It is tempting to speculate that these dolostone clasts were deposited in penecontemporaneous shallow-marine waters, and that their low δ13C values might reflect input of oxidised atmospheric methane to the ocean surface (and therefore the cause of the glaciation); the dolostones were subsequently resedimented into the deeper marine settings. However this must be left as a hypothesis to be tested when further age-constrained contemporaneous pre-glacial carbonate sections are found. © 2013 Elsevier B.V. 2013 English 03019268 10.1016/j.precamres.2013.06.007 Precambrian Research 235 Elsevier 278--294 Faculty of Earth and Life Sciences, Vrije Universiteit Amsterdam, De Boelelaan 1085, 1081HV Amsterdam, Netherlands; NERC Isotope Geosciences Laboratory, British Geological Survey, Environmental Science Centre, Keyworth, Nottingham NG12 5GG, United Kingdom; Geological Survey of Norway, Postboks 6315 Slupen, NO-7491 Trondheim, Norway; Centre for Geobiology, University of Bergen, Postboks 7803, NO-5020 Bergen, Norway; Department of Earth and Environmental Sciences, University of St Andrews, Scotland, St Andrews KY16 9AL, United Kingdom; Scottish Universities Environmental Research Centre, Rankine Avenue, East Kilbride, Scotland G75 0QF, United Kingdom; GNS Science, Private Bag 1930, Dunedin, New Zealand aragonite; carbon isotope; carbonate rock; deposition; diamictite; dolostone; geochemistry; geochronology; glaciation; inorganic carbon; methane; outcrop; oxidation; Proterozoic; sedimentology; tuff; volcanic ash, Kola Peninsula; Murmansk [Russian Federation]; Russian Federation https://www.scopus.com/inward/record.uri?eid=2-s2.0-84881086634&doi=10.1016%2fj.precamres.2013.06.007&partnerID=40&md5=5a00be1681b57f1df92ef8f5ca6e7291 cited By 27 AT Brasier AP Martin VA Melezhik AR Prave DJ Condon AE Fallick article martin2013dating Existing radio-isotopic age constraints indicate that the global Palaeoproterozoic Lomagundi-Jatuli large, positive carbonate carbon isotopic excursion, with δ13C values >+5‰, occurred between 2.2 and 2.06Ga. In the North Transfennoscandian Greenstone Belt of the Kola Peninsula, NW Russia, northern Norway and Finland, the Lomagundi-Jatuli Event is recorded in the carbonate rocks of the Umba and Kuetsjärvi Sedimentary Formations in the Imandra-Varzuga and Pechenga greenstone belts. In both areas, thick mafic volcanic units (Umba and Kuetsjärvi Volcanic Formations) overlie the carbon isotopic excursion-bearing sedimentary units. Overlying and younger sedimentary units contain carbonate rocks with δ13C values typically ranging between c. -1 and +3‰, signalling the termination of the Lomagundi-Jatuli excursion.Two new U-Pb ID-TIMS (isotope-dilution thermal ionisation mass spectrometry) zircon dates constrain this termination in both successions. The lower unit of the Il'mozero Sedimentary Formation is a cross- and parallel-bedded volcaniclastic greywacke derived largely from erosion of the underlying Umba Volcanic Formation. It has yielded detrital zircons with 207Pb/206Pb dates as young as 2055.5±2.3Ma, which is a maximum age for deposition and is inferred to date part of the underlying Umba volcanics. In Pechenga, the Kolosjoki Sedimentary Formation was intersected by a drill hole obtained by the ICDP (International Continental Scientific Drilling Program)-supported FAR-DEEP (Fennoscandian Arctic Russia-Drilling Early Earth Project) drilling programme. Zircons from a mafic fine tuff in this drill core have yielded a 207Pb/206Pb age of 2056.6±0.8Ma. This age is interpreted as an eruption age contemporaneous with sedimentation. The new age determinations overlap each other within uncertainty, and is within error of previously published detrital zircon ages of 2058±2Ma from the Kolosjoki Sedimentary Formation and 2049±28Ma from the Kuetsjärvi Volcanic Formation. Combined, these indicate that the Lomagundi-Jatuli excursion terminated across Fennoscandia by 2056.6±0.8Ma and may correlate with similar termination ages in Fennoscandia and the Transvaal, South Africa. © 2012. 2013 English 03019268 10.1016/j.precamres.2012.09.010 Precambrian Research 224 Elsevier 160--168 NERC Isotope Geosciences Laboratory, British Geological Survey, Keyworth NG125GG, United Kingdom; Department of Earth Sciences, University of St Andrews, St Andrews, Scotland, United Kingdom; Geological Survey of Norway, Postboks 6315 Slupen, 7491 Trondheim, Norway; Centre for Geobiology, University of Bergen, Postboks 7803, N-5020 Bergen, Norway; Tallinn Technical University, Institute of Geology, 19086 Tallinn, Estonia; Scottish Universities Environmental Research Centre, East Kilbride, Glasgow G75 0QF, Scotland, United Kingdom carbon isotope; carbonate rock; deposition; geochronology; greenstone belt; Proterozoic; radionuclide; sedimentation; uranium-lead dating; zircon, Fennoscandia; Finland; Kola Peninsula; Murmansk [Russian Federation]; Norway; Russian Federation; South Africa; Transvaal https://www.scopus.com/inward/record.uri?eid=2-s2.0-84867584239&doi=10.1016%2fj.precamres.2012.09.010&partnerID=40&md5=ec837ea3ef09acf151d9853f2ab60cdc cited By 40 Adam P Martin DJ Condon Anthony R Prave Victor A Melezhik Aivo Lepland Anthony E Fallick article asael2013coupled 2013 Chemical Geology 362 Elsevier 193--210 Dan Asael François LH Tissot Christopher T Reinhard Olivier Rouxel Nicolas Dauphas Timothy W Lyons Emmanuel Ponzevera Céline Liorzou Sandrine Chéron inproceedings rozanov2013unique 2013 SP MAIK Nauka/Interperiodica Doklady Biological Sciences 449 96--98 1 A Yu Rozanov MM Astafieva article kump20137 2013 Reading the Archive of Earth’s Oxygenation: Volume 3: Global Events and the Fennoscandian Arctic Russia-Drilling Early Earth Project Springer 1457--1514 Lee R Kump Anton B Kuznetsov Igor M Gorokhov Victor A Melezhik Juraj Farkaš Ramananda Chakrabarti Stein B Jacobsen Christopher T Reinhard Timothy W Lyons Olivier Rouxel others incollection melezhik20136 2013 Reading the Archive of Earth’s Oxygenation Springer 505--590 Victor A Melezhik Anthony R Prave Aivo Lepland Eero J Hanski Alexander E Romashkin Dmitry V Rychanchik Zhen-Yu Luo Evgenii V Sharkov Maria M Bogina Alex T Brasier others incollection lepland20135 2013 Reading the Archive of Earth’s Oxygenation Springer 493--502 Aivo Lepland Melanie Mesli Ronald Conze Karl Fabian Anthony E Fallick LR Kump article melezhik2012reading 2012 Springer Science & Business Media Victor Melezhik Anthony R Prave Eero J Hanski Anthony E Fallick Aivo Lepland Lee R Kump Harald Strauss article melezhik2012reading 2012 Springer Science and Business Media Victor Melezhik Anthony R Prave Anthony E Fallick Lee R Kump Harald Strauss Aivo Lepland Eero J Hanski article van2012mineral 2012 Geochimica et Cosmochimica Acta 83 Elsevier 252--262 Mark A Zuilen Daniel Fliegel Aivo Lepland Yuangao Qu Anja Schreiber Alexander E Romashkin Pascal Philippot article qu2012methanotrophy 2012 Geobiology 10 Wiley Online Library 467--478 6 Yu Qu AE {\v{C}}rne A Lepland MA Van Zuilen article reuschel2012isotopic 2012 Precambrian Research 192 Elsevier 78--88 M Reuschel VA Melezhik MJ Whitehouse A Lepland AE Fallick H Strauss incollection melezhik2012far 2012 Reading the Archive of Earth’s Oxygenation: Volume 3: Global Events and the Fennoscandian Arctic Russia-Drilling Early Earth Project Springer 1537--1552 Victor A Melezhik AR Prave incollection melezhik20121 2012 Reading the Archive of Earth’s Oxygenation: Volume 1: The Palaeoproterozoic of Fennoscandia as Context for the Fennoscandian Arctic Russia-Drilling Early Earth Project Springer 25--30 Victor A Melezhik incollection melezhik20121 2012 Reading the Archive of Earth’s Oxygenation: Volume 1: The Palaeoproterozoic of Fennoscandia as Context for the Fennoscandian Arctic Russia-Drilling Early Earth Project Springer 249--287 VA Melezhik article Brasier2011193 Palaeoproterozoic Tulomozero Formation carbonates of the Onega basin were targeted by ICDP FAR-DEEP Hole 10B. The recovered rocks contain abundant evidence for Palaeoproterozoic gypsum and anhydrite, particularly in the form of pseudomorphs of inclusion-containing nodules, swallow-tail twinned crystals and evaporite dissolution breccias. Similarly, sand-patch fabric indicates the former presence of surface-covering salt crusts in the Palaeoproterozoic. Atmospheric oxygen and seawater sulphate levels at that time must have been sufficient to allow such sulphates to form. Carbonate δ13C values are considered sedimentary or early diagenetic, predating greenschist facies metamorphism associated with the Svecofennian Orogeny. These carbonate δ13C values range from +7.7 to +15.7‰, with the highest (and lowest) values found in dolostones. The dolostones as well as calcitised calcium sulphates record the Lomagundi-Jatuli signal. However evidence for activity of sulphate-reducing and/or methanogenic bacteria seems to be lacking. Dolomite precipitation (or dolomitisation), calcium sulphate calcitisation and production of the high 13C values (processes which typically involve such bacteria in the Phanerozoic) are thus inferred to have proceeded without the direct influence of sulphate reducers and methanogens. The most plausible explanation for the Lomagundi-Jatuli excursion seems to remain significant sequestration of organic carbon in a location yet to be identified. © 2011 Elsevier B.V. 2011 English 03019268 10.1016/j.precamres.2011.05.011 Precambrian Research 189 193-211 Scottish Universities Environmental Research Centre, Scottish Enterprise Technology Park, East Kilbride G75 0QF, Scotland, United Kingdom; Department of Earth Sciences, University of St Andrews, St Andrews KY16 9AL, Scotland, United Kingdom; Geological Survey of Norway, Postboks 6315 Slupen, 7491 Trondheim, Norway; Centre for Geobiology, University of Bergen, Postboks 7803, N-5020 Bergen, Norway; Tallinn Technical University, Institute of Geology, 19086 Tallinn, Estonia 1-2 anhydrite; carbon isotope; carbonate; coastal sediment; dolomite; dolostone; gypsum; methanogenesis; organic carbon; oxygen; precipitation (chemistry); pseudomorph; sabkha; seawater; sulfate, Arkhangelsk [Russian Federation]; Onega Basin; Russian Federation, Centroberyx lineatus https://www.scopus.com/inward/record.uri?eid=2-s2.0-79960420590&doi=10.1016%2fj.precamres.2011.05.011&partnerID=40&md5=cdd41829d2321daf96e1df9daf94f593 cited By 22 A.T. Brasier A.E. Fallick A.R. Prave V.A. Melezhik A. Lepland inproceedings astafieva2011multicellular 2011 SPIE Instruments, Methods, and Missions for Astrobiology XIV 8152 50--59 Marina M Astafieva Alexei Yu Rozanov Richard B Hoover article melezhik2010great 2010 Scientific Drilling 9 Copernicus GmbH 23--29 Victor A Melezhik Aivo Lepland Alexander E Romashkin Dmitry V Rychanchik Melanie Mesli RE Finne Ronald Conze others article medvedev2009palaeoproterozoic 2009 Paleontological Journal 43 Springer 972--979 8 PV Medvedev VA Melezhik MM Filippov article melezhik2009petroleum 2009 Terra Nova 21 Wiley Online Library 119--126 2 Victor A Melezhik Anthony E Fallick Michail M Filippov Aivo Lepland Dmitry V Rychanchik Yuliya E Deines Pavel V Medvedev Alexander E Romashkin Harald Strauss article pasek2008session 2008 Astrobiology 8 Mary Ann Liebert, Inc. 140 Huguenot Street, 3rd Floor New Rochelle, NY 10801~… 356--361 2 Matthew Pasek Dominic Papineau Jelte Harnmeijer article melezhik2006icdp 2006 Scientific Drilling 2 56--57 Victor A Melezhik Aivo Lepland