Publicación:
Gorgona Island (Colombia) as a terrestrial analog of Syrtis Major (Mars): Evidence from geochemical meta-analyses and compositional figures of merit

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dc.contributor.authorDavid Tovar, María Angelica
dc.contributor.authorLeal, M.A.
dc.contributor.authorDe Pablo, M. A.
dc.contributor.authorSan Martin-Lobos, J.
dc.contributor.authorTchegliakova, N.
dc.contributor.authorVélez, F.
dc.contributor.authorMolina, A.
dc.contributor.authorLeone, G.
dc.contributor.authorSanchez , Jimena
dc.contributor.authorA. Torres
dc.contributor.authorBonilla, M.A.
dc.contributor.authorAcevedo Barrios, Rosa Leonor
dc.contributor.authorCancino-Escalante, G.
dc.contributor.researcherRosa Acevedo-Barrios
dc.contributor.researchgroupGrupo de Investigación Estudios Químicos y Biológicos
dc.contributor.seedbedsSemillero de Investigación en Ciencias Ambientales
dc.coverage.temporalComunidad cientifica y academica en general
dc.date.accessioned2026-05-11T18:56:26Z
dc.date.issued2026-04-28
dc.descriptionContiene mapas, gráficos
dc.description.abstractThe identification of terrestrial analogs is a key strategy for advancing our understanding of the geological and geochemical evolution of Mars. This study evaluates the potential of Gorgona Island (Colombian Pacific) as a geochemical analog of Syrtis Major. Gorgona Island hosts a diversity of mafic and ultramafic lithologies, including basalts, gabbros, picrites, dunites, wehrlites, and also komatiites, which are the youngest reported on Earth. To assess the degree of compositional similarity, a meta-analysis of previously published data was conducted, comparing geochemical information from Gorgona Island with that derived from orbital instruments on Mars (TES, GRS, OMEGA, and CRISM) and from SNC meteorites. The analysis focused on classical discriminant ratios (Al₂O₃/TiO₂) and Compositional Figures of Merit (FOMc), applied both to individual datasets and to averaged values weighted by the areal proportion of lithologies on Gorgona Island. The results show that enriched and depleted basalts, along with Spinifex-Textured komatiites (containing <18% MgO), exhibit a high degree of geochemical similarity with Syrtis Major (FOMc >0.87), whereas dunites and wehrlites consistently display low values. The positive slope of the Al₂O₃/TiO₂ ratio observed in both Gorgona and Mars is characteristic of MORB-type oceanic crust, reinforcing the link between Terrestrial MORB/OIB and Martian Basalts described by previous studies. These findings highlight Gorgona Island as a robust terrestrial analog of Syrtis Major, providing a natural laboratory for investigating magmatic processes relevant to Mars. Furthermore, this work outlines future directions, including the acquisition of new high-resolution geochemical data from Gorgona Island and the integration of recent in situ data from Mars, with the aim of refining comparative models of planetary magmatism.
dc.description.researchareaMicrobiología y toxicología ambiental
dc.description.tableofcontents1. Introduction 2.Materials and methods 3. Results 4.Discussion 5.Conclusions 6. References
dc.description.technicalinfoNo Aplica
dc.format.extent18 páginas
dc.format.mimetypeapplication/pdf
dc.identifier.citationD. Tovar, M. Leal, M.A. de Pablo, J. San Martin-Lobos, N. Tchegliakova, F. Vélez, A. Molina, G. Leone, J. Sánchez, A. Torres, A. Bonilla, R. Acevedo-Barrios, G. Cancino-Escalante,Gorgona Island (Colombia) as a terrestrial analog of Syrtis Major (Mars): Evidence from geochemical meta-analyses and compositional figures of merit,Icarus, Volume 456, 2026,117133,ISSN 0019-1035, https://doi.org/10.1016/j.icarus.2026.117133.
dc.identifier.doi10.1016/j.icarus.2026.117133
dc.identifier.urihttps://hdl.handle.net/20.500.12585/14446
dc.language.isoeng
dc.publisherIcarus
dc.publisher.placeColombia
dc.relation.references1. D. Tovar, M. Leal, M.A. de Pablo, J. San Martin-Lobos, N. Tchegliakova, F. Vélez, A. Molina, G. Leone, J. Sánchez, A. Torres, A. Bonilla, R. Acevedo-Barrios, G. Cancino-Escalante,Gorgona Island (Colombia) as a terrestrial analog of Syrtis Major (Mars): Evidence from geochemical meta-analyses and compositional figures of merit,Icarus, Volume 456, 2026,117133,ISSN 0019-1035, https://doi.org/10.1016/j.icarus.2026.117133.
dc.relation.referencesArndt, N.T., Naldrett, A.J., Pyke, D.R., 1977. Komatiitic and iron-rich tholeiitic lavas of Munro township, Northeast Ontario. J. Petrol. 18 (2), 319–369. https://doi.org/ 10.1093/petrology/18.2.319.
dc.relation.referencesArndt, N.T., Kerr, A.C., Tarney, J., 1997. Dynamic melting in plume heads: the formation of Gorgona komatiites and basalts. Earth Planet. Sci. Lett. 146 (1–2), 289–301. https://doi.org/10.1016/S0012-821X(96)00219-1.
dc.relation.referencesArndt, N., Lesher, M.C., Barnes, S.J., 2008. Komatiite. Cambridge University Press, p. 487.
dc.relation.referencesBandfield, J.L., 2002. Global mineral distributions on mars. J. Geophys. Res. Planets 107 (E6). https://doi.org/10.1029/2001JE001510, 9–1.
dc.relation.referencesBaratoux, D., Toplis, M.J., Monnereau, M., Gasnault, O., 2011. Thermal history of mars inferred from orbital geochemistry of volcanic provinces. Nature 472, 338–341. https://doi.org/10.1038/nature09903
dc.relation.referencesBaratoux, D., Samuel, H., Michaut, C., Toplis, M.J., Monnereau, M., Wieczorek, M., Garcia, R., Kurita, K., 2014. Petrological constraints on the density of the Martian crust. J. Geophys. Res. Planets 119, 1707–1727. https://doi.org/10.1002/ 2014JE004642.
dc.relation.referencesBeegle, L.W., Peters, G.H., Mungas, G.S., Bearman, G.H., Smith, J.A., Anderson, R.C., 2007. Mojave martian simulant: a new martian soil simulant. In: Lunar and Planetary Science Conference, p. 2005.
dc.relation.referencesBibring, J.-P., 2005. Mars surface diversity as revealed by the OMEGA/Mars express observations. Science 307 (5715), 1576–1581. https://doi.org/10.1126/ science.1108806
dc.relation.referencesBlack, B.A., Manga, M., 2016. The eruptibility of magmas at Tharsis and Syrtis Major on Mars. J. Geophys. Res. Planets 121 (6), 944–964. https://doi.org/10.1002/ 2016JE004998.
dc.relation.referencesBrown, A.J., Viviano, C.E., Goudge, T.A., 2020. Olivine-carbonate mineralogy of the Jezero crater region. J. Geophys. Res. Planets 125 (3). https://doi.org/10.1029/ 2019JE006011 e2019JE006011.
dc.relation.referencesBrügmann, G.E., Arndt, N.T., Hofmann, A.W., Tobschall, H.J., 1987. Noble metal abundances in komatiite suites from Alexo, Ontario and Gorgona Island, Colombia. Geochim. Cosmochim. Acta 51, 2159–2169. https://doi.org/10.1016/0016-7037 (87)90265-1.
dc.relation.referencesCampbell, I.H., Griffiths, R.W., 1990. Implications of mantle plume structure for the evolution of flood basalts. Earth Planet. Sci. Lett. 99 (1–2), 79–93. https://doi.org/ 10.1016/0012-821X(90)90072-6.
dc.relation.referencesChevrier, V., Math´e, P.E., 2007. Mineralogy and evolution of the surface of mars: a review. Planet. Space Sci. 55 (3), 289–314. https://doi.org/10.1016/j. pss.2006.05.039.
dc.relation.referencesChristensen, P.R., Bandfield, J.L., Clark, R.N., Edgett, K.S., Hamilton, V.E., Hoefen, T., Smith, M.D., 2000. Detection of crystalline hematite mineralization on Mars by the Thermal Emission Spectrometer: evidence for near-surface water. J. Geophys. Res. Planets 105 (E4), 9623–9642. https://doi.org/10.1029/1999JE001093.
dc.relation.referencesChristensen, P.R., Bandfield, J.L., Bell III, J.F., Gorelick, N., Hamilton, V.E., Ivanov, A., et al., 2003. Morphology and composition of the surface of Mars: Mars Odyssey THEMIS results. Science 300 (5628), 2056–2061. https://doi.org/10.1126/ science.1080885.
dc.relation.referencesClark, B.C., Gellert, R., Ming, D.W., Morris, R.V., Mittlefehldt, D.W., Squyres, S.W., 2006. PYTi-NiCr Signatures in the Columbia Hills are present in certain Martian meteorites. In Lunar and Planetary Science Conference.
dc.relation.referencesClenet, H., Pinet, P., Ceuleneer, G., Daydou, Y., Heuripeau, F., Rosemberg, C., et al., 2013. A systematic mapping procedure based on the modified Gaussian model to characterize magmatic units from olivine/pyroxenes mixtures: application to the Syrtis Major volcanic shield on mars. J. Geophys. Res. Planets 118 (8), 1632–1655. https://doi.org/10.1002/jgre.20112
dc.relation.referencesCousin, A., Sautter, V., Payr´e, V., Forni, O., Mangold, N., Gasnault, O., et al., 2017. Classification of igneous rocks analyzed by ChemCam at Gale crater, Mars. Icarus 288, 265–283. https://doi.org/10.1016/j.icarus.2017.01.014.
dc.relation.referencesDay, J.M., Tait, K.T., Udry, A., Moynier, F., Liu, Y., Neal, C.R., 2018. Martian magmatism from plume metasomatized mantle. Nat. Commun. 9 (1), 4799. https://doi.org/ 10.1038/s41467-018-07191-0.
dc.relation.referencesDemchuk, R.W., 2021. Detailed Mapping of Lava Flows in Syrtis Major Planum, Mars. Masters Thesis. Ohio University. http://rave.ohiolink.edu/etdc/view?acc_num=ohi ou1617806602421614.
dc.relation.referencesDietrich, V.J., Gansser, A., Sommerauer, J., Cameron, W.E., 1981. Palaeogene komatiites from Gorgona island, East Pacific-A primary magma for ocean floor basalts? Geochem. J. 15 (3), 141–161. https://doi.org/10.2343/geochemj.15.141.
dc.relation.referencesDuktig, B.R., 2023. Analyzing Compositional, Mineralogical, and Petrological Variations in Syrtis Major Planum Lava Flows throughout Martian Time. Masters Thesis. Ohio University. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou168324332383 4276.
dc.relation.referencesDunn, T.L., McSween Jr., H.Y., Christensen, P.R., 2007. Thermal emission spectra of terrestrial alkaline volcanic rocks: applications to Martian remote sensing. J. Geophys. Res. Planets 112 (E5). https://doi.org/10.1029/2006JE002766.
dc.relation.referencesDypvik, H., Hellevang, H., Krzesi´nska, A., Sætre, C., Viennet, J.C., Bultel, B., et al., 2021. The planetary terrestrial analogues library (PTAL)–an exclusive lithological selection of possible martian earth analogues. Planet. Space Sci. 208, 105339. https://doi.org/ 10.1016/j.pss.2021.105339.
dc.relation.referencesEcheverria, L.M., 1980. Tertiary or Mesozoic komatiites from Gorgona island, Colombia: field relations and geochemistry. Contrib. Mineral. Petrol. 73 (3), 253–266. https:// doi.org/10.1007/BF00381444.
dc.relation.referencesEcheverría, L.M., Aitken, B.G., 1986. Pyroclastic rocks: another manifestation of ultramafic volcanism on Gorgona Island, Colombia. Contrib. Mineral. Petrol. 92 (4), 428–436. https://doi.org/10.1007/BF00374425.
dc.relation.referencesEgger, M., Ebrahim, S., Smith, G.D., 2002. Where now for meta-analysis? Int. J. Epidemiol. 31 (1), 1–5. https://doi.org/10.1093/ije/31.1.1.
dc.relation.referencesEhlmann, B.L., Mustard, J.F., Murchie, S.L., Poulet, F., Bishop, J.L., Brown, A.J., et al., 2008. Orbital identification of carbonate-bearing rocks on mars. Science 322 (5909), 1828–1832. https://doi.org/10.1126/science.1164759.
dc.relation.referencesEmran, A., Tarnas, J.D., Stack, K.M., 2025. Global distribution of serpentine on mars. Geophys. Res. Lett. 52 (2). https://doi.org/10.1029/2024GL110630 e2024GL110630.
dc.relation.referencesFawdon, P., 2016. The Volcanic Evolution of Syrtis Major Planum, Mars. Open University (United Kingdom).
dc.relation.referencesFawdon, P., Skok, J.R., Balme, M.R., Vye-Brown, C.L., Rothery, D.A., Jordan, C.J., 2015. The geological history of Nili Patera, Mars. J. Geophys. Res., Planets 120 (5), 951–977. https://doi.org/10.1002/2015JE004795.
dc.relation.referencesFiliberto, J., 2017. Geochemistry of Martian basalts with constraints on magma genesis. Chem. Geol. 466, 1–14. https://doi.org/10.1016/j.chemgeo.2017.06.009.
dc.relation.referencesFiliberto, J., 2019, July. Geochemistry of Martian Basalts: Support for Mars Sample Return of a Noachian/Hesperian Lava. In Ninth International Conference on Mars, vol. 2089, p. 6019.
dc.relation.referencesFiliberto, J., Dasgupta, R., 2015. Constraints on the depth and thermal vigor of melting in the martian mantle. J. Geophys. Res. Planets 120 (1), 109–122. https://doi.org/ 10.1002/2014JE004745.
dc.relation.referencesFiliberto, J., Gross, J., Trela, J., Ferr´e, E.C., 2014. Gabbroic shergottite northwest Africa 6963: an intrusive sample of mars. Am. Mineral. 99 (4), 601–606. https://doi.org/ 10.2138/am.2014.4638.
dc.relation.referencesGill, R., 2011. Igneous Rocks and Processes: A Practical Guide. Wiley-Blackwell. Chapter 5, p. 148, box 5.5.
dc.relation.referencesGreenough, J.D., Ya’acoby, A., 2013. A comparative geochemical study of Mars and Earth basalt petrogenesis. Can. J. Earth Sci. 50 (1), 78–93. https://doi.org/10.1139/ cjes-2012-0023.
dc.relation.referencesGross, J., Filiberto, J., Bell, A.S., 2013. Water in the martian interior: evidence for terrestrial MORB mantle-like volatile contents from hydroxyl-rich apatite in olivine–phyric shergottite NWA 6234. Earth Planet. Sci. Lett. 369, 120–128. https:// doi.org/10.1016/j.epsl.2013.03.016.
dc.relation.referencesGrove, T.L., Parman, S.W., 2004. Thermal evolution of the earth as recorded by komatiites. Earth Planet. Sci. Lett. 219 (3–4), 173–187. https://doi.org/10.1016/ S0012-821X(04)00002-0.
dc.relation.referencesGurenko, A.A., Kamenetsky, V.S., Kerr, A.C., 2016. Oxygen isotopes and volatile contents of the Gorgona komatiites, Colombia: a confirmation of the deep mantle origin of H2O. Earth Planet. Sci. Lett. 454, 154–165. https://doi.org/10.1016/j. epsl.2016.08.035.
dc.relation.referencesHamilton, V.E., Christensen, P.R., 2000. Determining the modal mineralogy of mafic and ultramafic igneous rocks using thermal emission spectroscopy. J. Geophys. Res. Planets 105, 9717–9733. https://doi.org/10.1029/1999JE001113.
dc.relation.referencesHamilton, V.E., Wyatt, M.B., McSween Jr., H.Y., Christensen, P.R., 2001. Analysis of terrestrial and martian volcanic compositions using thermal emission spectroscopy: 2. application to martian surface spectra from the Mars Global Surveyor Thermal Emission Spectrometer. J. Geophys. Res. Planets 106 (E7), 14733–14746. https:// doi.org/10.1029/2000JE001353.
dc.relation.referencesHamilton, V.E., Christensen, P.R., Mcsween, H.Y., Bandfield, J.L., 2003. Searching for the source regions of martian meteorites using MGS TES: integrating martian meteorites into the global distribution of igneous materials on mars. Meteorit. Planet. Sci. 38, 871–885. https://doi.org/10.1111/j.1945-5100.2003.tb00284.x.
dc.relation.referencesHerzberg, C., Condie, K., Korenaga, J., 2010. Thermal history of the earth and its petrological expression. Earth Planet. Sci. Lett. 292 (1–2), 79–88. https://doi.org/ 10.1016/j.epsl.2010.01.022.
dc.relation.referencesHiesinger, H., Head III, J.W., 2004. The Syrtis Major volcanic province, Mars: synthesis from mars global surveyor data. J. Geophys. Res. Planets 109 (E1). https://doi.org/ 10.1029/2003JE002143.
dc.relation.referencesHood, D.R., Judice, T., Karunatillake, S., Rogers, D., Dohm, J.M., Susko, D., Carnes, L.K., 2016. Assessing the geologic evolution of Greater Thaumasia, Mars. J. Geophys. Res. Planets 121, 1753–1769. https://doi.org/10.1002/2016JE005046.
dc.relation.referencesHughes, E.B., Wray, J., Karunatillake, S., Fanson, G., Harrington, E., Hood, D.R., 2024. Water-limited hydrothermalism and volcanic resurfacing of Eridania Basin, Mars. J. Geophys. Res. 129 (7), e2024JE008461. https://doi.org/10.1029/2024JE008461.
dc.relation.referencesISO, 2014. SO 10788:2014(en) Space systems — Lunar simulants. Online Brows Platf. URL. https://www.iso.org/obp/ui#iso:std:iso:10788:ed-1:v1:en. accessed 05.20.25.
dc.relation.referencesJensen, L.S., Pyke, D.R., 1982. Komatiites in the Ontario Portion of the Abitibi Belt. Inist- CNRS & Bureau de Recherches G´eologiques et Mini`eres.
dc.relation.referencesKamenetsky, V.S., Gurenko, A.A., Kerr, A.C., 2010. Composition and temperature of komatiite melts from Gorgona Island, Colombia, constrained from olivine-hosted melt inclusions. Geology 38 (11), 1003–1006. https://doi.org/10.1130/G31143.1.
dc.relation.referencesKerr, A.C., 2005. La Isla de Gorgona, Colombia: a petrological enigma? Lithos 84 (1–2), 77–101. https://doi.org/10.1016/j.lithos.2005.02.006.
dc.relation.referencesKerr, A.C., Arndt, N.T., 2001. A note on the IUGS reclassification of the high-Mg and picritic volcanic rocks. J. Petrol. 42 (11), 2169–2171. https://doi.org/10.1093/ petrology/42.11.2169.
dc.relation.referencesKerr, A.C., Marriner, G.F., Arndt, N.T., Tarney, J., Nivia, A., Saunders, A.D., Duncan, R. A., 1996a. The petrogenesis of Gorgona komatiites, picrites and basalts: new field, petrographic and geochemical constraints. Lithos 37 (2–3), 245–260. https://doi. org/10.1016/0024-4937(95)00039-9.
dc.relation.referencesKerr, A.C., Tarney, J., Marriner, G.F., Nivia, A., Klaver, G.T., Saunders, A.D., 1996b. The geochemistry and tectonic setting of late cretaceous Caribbean and Colombian volcanism. J. S. Am. Earth Sci. 9, 111–120. https://doi.org/10.1016/0895-9811(96) 00031-4.
dc.relation.referencesKoppers, A.A., Becker, T.W., Jackson, M.G., et al., 2021. Mantle plumes and their role in Earth processes. Nat. Rev. Earth Environ. 2 (6), 382–401. https://doi.org/10.1038/ s43017-021-00168-6.
dc.relation.referencesLe Maitre, R.W., Streckeisen, A., Zanettin, B., Le Bas, M.J., Bonin, B., Bateman, P. (Eds.), 2005. Igneous Rocks: A Classification and Glossary of Terms: Recommendations of the International Union of Geological Sciences Subcommission on the Systematics of Igneous Rocks. Cambridge University Press.
dc.relation.referencesLentz, R.F., Taylor, G.J., Treiman, A.H., 1999. Formation of a martian pyroxenite: A comparative study of the nakhlite meteorites and Theo’s Flow. Meteorit. Planet. Sci. 34 (6), 919–932. https://doi.org/10.1111/j.1945-5100.1999.tb01410.x.
dc.relation.referencesLillis, R.J., Dufek, J., Kiefer, W.S., Black, B.A., Manga, M., Richardson, J.A., Bleacher, J. E., 2015. The Syrtis Major Volcano, Mars: A multidisciplinary approach to interpreting its magmatic evolution and structural development. J. Geophys. Res. Planets 120 (9), 1476–1496. https://doi.org/10.1002/2014JE004774.
dc.relation.referencesLiu, Y., Tice, M.M., Schmidt, M.E., Treiman, A.H., Kizovski, T.V., Hurowitz, J.A., Allwood, A.C., Henneke, J., Pedersen, D.A.K., VanBommel, S.J., Jones, M.W.N., Knight, A.L., Orenstein, B.J., Clarck, B.C., Elam, W.T., Heirwegh, C.M., Barber, T., Beegle, L., Benzerara, K., Bernard, S., Beyssac, O., Bosak, T., Brown, A.J., Cardarelli, E.L., Catling, D.C., Christian, J.R., Cloutis, E.A., Cohen, B.A., Davidoff, S., Fair´en, A.G., Farley, K.A., Flannery, D.T., Galvin, A., Grotzinger, J.P., Gupta, S.,Hall, J., Herd, C.D.K., Hickman-Lewis, K., Hodyss, R.P., Horgan, B.H.N., Johnson, J. R., Jørgensen, J.L., Kah, L.C., Maki, J.N., Mandon, L., Mangold, N., McCubbin, F.M., McLennan, S.M., Moore, K., Nachon, M., Nemere, P., Nothdurft, L.D., Nú˜nez, J.I., O’Neil, L., Quantin-Nataf, C.M., Sautter, V., Schuster, D.L., Siebach, K.L., Simon, J.I., Sinclair, K.P., Stack, K.M., Steele, A., Tarnas, J.D., Tosca, N.J., Uckert, K., Udry, R., Wade, L.A., Weiss, B.P., Wiens, R.C., Williford, K.H., Zorzano, M.P., 2022. An olivine cumulate outcrop on the floor of Jezero Crater. Mar. Sci. 377 (6614), 1513–1519. https://doi.org/10.1126/science.abo2756.
dc.relation.referencesLodders, K., 1998. A survey of shergottite, nakhlite and chassigny meteorites whole-rock compositions. Meteorit. Planet. Sci. 33 (S4), A183–A190. https://doi.org/10.1111/ j.1945-5100.1998.tb01331.x.
dc.relation.referencesLunning, N.G., Gardner-Vandy, K.G., Sosa, E.S., McCoy, T.J., Bullock, E.S., Corrigan, C. M., 2017. Partial melting of oxidized planetesimals: an experimental study to test the formation of oligoclase-rich achondrites Graves Nunataks 06128 and 06129. Geochim. Cosmochim. Acta 214, 73–85. https://doi.org/10.1016/j. gca.2017.07.004.
dc.relation.referencesLustrino, M., Bonin, B., Doroshkevich, A., Kerr, Z.G.A., Heilborn, M., Irving, T., Ivanov, A., Mitchel, R., Nakawaga, M., Natland, J., Pearce, J., Scott-Smith, B., Srivastava, R., Tappe, S., Wilson, M., Zellmer, G., 2020. IUGS Task Group on Igneous Rocks TGIR.
dc.relation.referencesMcCollom, T.M., Seewald, J.S., 2013. Serpentinites, hydrogen, and life. Elements 9 (2), 129–134. https://doi.org/10.2113/gselements.9.2.129.
dc.relation.referencesMcGetchin, T.R., Smith, J.R., 1978. The mantle of mars: some possible geological implications of its high density. Icarus 34 (3), 512–536. https://doi.org/10.1016/ 0019-1035(78)90042-8.
dc.relation.referencesMcSween Jr., H.Y., 2015. Petrology on mars. Am. Mineral. 100 (11􀀀12), 2380–2395. https://doi.org/10.2138/am-2015-5257.
dc.relation.referencesMcSween Jr., H.Y., Taylor, G.J., Wyatt, M.B., 2009. Elemental composition of the Martian crust. Science 324 (5928), 736–739. https://doi.org/10.1126/ science.116587.
dc.relation.referencesMcSween, H.Y., McLennan, S.M., 2014. Mars. In: Holland, Heinrich D., Turekian, Karl K. (Eds.), Treatise on Geochemistry, Second edition, pp. 251–300. https://doi.org/ 10.1016/B978-0-08-095975-7.00125-X.
dc.relation.referencesMendes, L.N., Martinsson, O., Jamal, D.L., Zadeh, A.A., Wanhainen, C., 2025. Lithogeochemistry and origin of the komatiites from Mundonguara mine in the Manica Greenstone Belt, Mozambique. J. Afr. Earth Sci. 223, 105494. https://doi. org/10.1016/j.jafrearsci.2024.105494.
dc.relation.referencesMetzger, P.T., Britt, D.T., Covey, S., Schultz, C., Cannon, K.M., Grossman, K.D., Mantovani, J., Mueller, R.P., 2019. Measuring the fidelity of asteroid regolith and cobble simulants. Icarus 321, 632–646. https://doi.org/10.1016/j. icarus.2018.12.019.
dc.relation.referencesMeyer, C., 2012a. Los Angeles – 698 Grams Enriched Basaltic Shergottite. In: Martian Meteorite Compendium. NASA. https://curator.jsc.nasa.gov/antmet/mmc/. accessed 06.20.25.
dc.relation.referencesMeyer, C., 2012b. Shergotty “Enriched” Basalt, 5 kg. In: Martian Meteorite Compendium. NASA. https://curator.jsc.nasa.gov/antmet/mmc/. accessed 06.20.25.
dc.relation.referencesMeyer, C., 2012c. QUE94201 – 12.02 grams depleted basaltic shergottite. In: Martian Meteorite Compendium. NASA. https://curator.jsc.nasa.gov/antmet/mmc/. accessed 06.20.25.
dc.relation.referencesMikolajewicz, N., Komarova, S.V., 2019. Meta-analytic methodology for basic research: a practical guide. Front. Physiol. 10, 203. https://doi.org/10.3389/fphys.2019.00203.
dc.relation.referencesMustard, J.F., Erard, S., Bibring, J.P., Head, J.W., Hurtrez, S., Langevin, Y., Pieters, C.C: m, Sotin, C.J., 1993. The surface of syrtis major: composition of the volcanic substrate and mixing with altered dust and soil. J. Geophys. Res. Planets 98 (E2), 3387–3400. https://doi.org/10.1029/92JE02682.
dc.relation.referencesMustard, J.F., Murchie, S., Erard, S., Sunshine, J., 1997. In situ compositions of Martian Volcanics: implications for the mantle. J. Geophys. Res. Planets 102, 25605–25615. https://doi.org/10.1029/97JE02354.
dc.relation.referencesMustard, J.F., Poulet, F., Gendrin, A., Bibring, J.P., Langevin, Y., Gondet, B., Mangold, N., Bellucci, G., Altieri, F., 2005. Olivine and pyroxene diversity in the crust of mars. Science 307 (5715), 1594–1597. https://doi.org/10.1126/ science.1109098.
dc.relation.referencesNair, A.M., Mathew, G., 2017. Geochemical modelling of terrestrial igneous rock compositions using laboratory thermal emission spectroscopy with an overview on its applications to Indian Mars Mission. Planet. Space Sci. 140, 62–73. https://doi. org/10.1016/j.pss.2017.04.009.
dc.relation.referencesNesbitt, R.W., Sun, S.S., Purvis, A.C., 1979. Komatiites; geochemistry and genesis. Can. Mineral. 17 (2), 165–186
dc.relation.referencesOdy, A., Poulet, F., Quantin, C., Bibring, J.-P., Bishop, J.L., Dyar, M.D., 2015. Candidates source regions of Martian meteorites as identified by OMEGA/MEx. Icarus 258, 366–383. https://doi.org/10.1016/j.icarus.2015.05.019.
dc.relation.referencesPearce, J.A., 2008. Geochemical fingerprinting of oceanic basalts with applications to ophiolite classification and the search for Archean oceanic crust. Lithos 100 (1–4), 14–48. https://doi.org/10.1016/j.lithos.2007.06.016.
dc.relation.referencesPeters, G.H., Abbey, W., Bearman, G.H., Mungas, G.S., Smith, J.A., Anderson, R.C., Douglas, S., Beegle, L.W., 2008. Mojave mars simulant—characterization of a new geologic mars analog. Icarus 197, 470–479. https://doi.org/10.1016/j. icarus.2008.05.004
dc.relation.referencesPoulet, F., Mangold, N., Platevoet, B., Bardintzeff, J.-M., Sautter, V., Mustard, J.F., Bibring, J.-P., Pinet, P., Langevin, Y., Gondet, B., Al´eon-Toppani, A., 2009. Quantitative compositional analysis of Martian mafic regions using the MEx/ OMEGA reflectance data. Icarus 201, 84–101. https://doi.org/10.1016/j. icarus.2008.12.042.
dc.relation.referencesPutirka, K., 2016. Rates and styles of planetary cooling on Earth, Moon, Mars, and Vesta, using new models for oxygen fugacity, ferric-ferrous ratios, olivine-liquid Fe-Mgexchange, and mantle potential temperature. Am. Mineral. 101 (4), 819–840. https://doi.org/10.2138/am-2016-5402.
dc.relation.referencesR Core Team, 2024. R: A Language and Environment for Statistical Computing. R Foundation for Statistical Computing, Vienna, Austria. https://www.R-project.or g/&gt.
dc.relation.referencesRamkissoon, N.K., Pearson, V.K., Schwenzer, S.P., Schr¨oder, C., Kirnbauer, T., Wood, D., et al., 2019. New simulants for Martian regolith: controlling iron variability. Planet. Space Sci. 179, 104722. https://doi.org/10.1016/j.pss.2019.104722.
dc.relation.referencesRampey, M., Harvey, R., 2012. Mars Hesperian magmatism as revealed by Syrtis major and the Circum-Hellas volcanic province. Earth Moon Planet. 109, 61–75. https:// doi.org/10.1007/s11038-012-9404-0.
dc.relation.referencesRamsey, M.S., Christensen, P.R., 1998. Mineral abundance determination: Quantitative deconvolution of thermal emission spectra. J. Geophys. Res. Solid Earth 103, 577–596. https://doi.org/10.1029/97JB02784.
dc.relation.referencesRani, A., Basu Sarbadhikari, A., Hood, D.R., Gasnault, O., Nambiar, S., Karunatillake, S., 2022. Consolidated chemical provinces on mars: implications for geologic interpretations. Geophys. Res. Lett. 49 (14). https://doi.org/10.1029/ 2022GL099235 e2022GL099235.
dc.relation.referencesRay, D., Misra, S., 2015. Martian basalts-planetary analogue of terrestrial MORBs?. In: European Planetary Science Congress. Europlanet, Nantes, France, p. 47.
dc.relation.referencesR´evillon, S., Arndt, N.T., Chauvel, C., Hallot, E., 2000. Geochemical study of ultramafic volcanic and plutonic rocks from Gorgona island, Colombia: the plumbing system of an oceanic plateau. J. Petrol. 41 (7), 1127–1153. https://doi.org/10.1093/ petrology/41.7.1127.
dc.relation.referencesR´evillon, S., Chauvel, C., Arndt, N.T., Pik, R., Martineau, F., Fourcade, S., Marty, B., 2002. Heterogeneity of the Caribbean plateau mantle source: Sr, o and he isotopic compositions of olivine and clinopyroxene from Gorgona island. Earth Planet. Sci. Lett. 205 (1–2), 91–106. https://doi.org/10.1016/S0012-821X(02)01003-8.
dc.relation.referencesReyes, D.P., Christensen, P.R., 1994. Evidence for komatiite-type lavas on mars from Phobos ISM data and other observations. Geophys. Res. Lett. 21 (10), 887–890. https://doi.org/10.1029/94GL01002.
dc.relation.referencesRichards, M.A., Duncan, R.A., Courtillot, V.E., 1989. Flood basalts and hot-spot tracks: plume heads and tails. Science 246 (4926), 103–107. https://doi.org/10.1126/ science.246.4926.103.
dc.relation.referencesRickman, D., Hoelzer, H., Carpenter, P., Sibille, L., Howard, R., Owens, C., 2007. A quantitative method for evaluating regolith simulants. In: AIP Conference Proceedings, vol. 880. American Institute of Physics, pp. 957–963. https://doi.org/ 10.1063/1.2437539. No. 1.
dc.relation.referencesRickman, D., Hoelzer, H., Fourroux, K., 2009. Lunar Regolith Figures of Merit. In Lunar Regolith/Simulant Workshop (No. MSFC-2219).
dc.relation.referencesRiel, N., Duarte, J.C., Almeida, J., Kaus, B.J., Rosas, F., Rojas-Agramonte, Y., Popov, A., 2023. Subduction initiation triggered the Caribbean large igneous province. Nat. Commun. 14 (1), 786. https://doi.org/10.1038/s41467-023-36419-x.
dc.relation.referencesRubin, A.E., Warren, P.H., Greenwood, J.P., Verish, R.S., Leshin, L.A., Hervig, R.L., et al., 2000. Los Angeles: the most differentiated basaltic Martian meteorite. Geology 28 (11), 1011–1014. https://doi.org/10.1130/0091-7613(2000)28<1011: LATMDB>2.0.CO;2.
dc.relation.referencesSalvatore, M.R., Mustard, J.F., Wyatt, M.B., Murchie, S.L., 2010. Definitive evidence of Hesperian basalt in Acidalia and Chryse planitiae. J. Geophys. Res. 115, E07005. https://doi.org/10.1029/2009JE003519.
dc.relation.referencesSalvatore, M.R., Goudge, T.A., Bramble, M.S., Edwards, C.S., Bandfield, J.L., Amador, E. S., et al., 2018. Bulk mineralogy of the NE Syrtis and Jezero crater regions of mars derived through thermal infrared spectral analyses. Icarus 301, 76–96. https://doi. org/10.1016/j.icarus.2017.09.019.
dc.relation.referencesSan Martin, J., Leone, G., Riveros-Jensen, K., Alam, M.A., Cabrera, R., San Martin, D., Oses, R., Blamey, J., Demergasso, C., Abrevaya, X., Guiliani, N., Britt, D., Liu, Y., Silva, W., Slumba, K., Tovar, D., Leal, M.A., de Pablo, M.A., 2025. Prospecting the first Chilean Martian simulants from the Atacama Desert for ISRU and potential applications. Icarus 429, 116403. https://doi.org/10.1016/j.icarus.2024.116403.
dc.relation.referencesScott, A.N., Oze, C., Tang, Y., O’Loughlin, A., 2017. Development of a Martian regolith simulant for in-situ resource utilization testing. Acta Astronaut. 131, 45–49. https:// doi.org/10.1016/j.actaastro.2016.11.024
dc.relation.referencesSerrano, L., Ferrari, L., Martínez, M.L., Petrone, C.M., Jaramillo, C., 2011. An integrative geologic, geochronologic and geochemical study of Gorgona Island, Colombia: implications for the formation of the Caribbean Large Igneous Province. Earth Planet. Sci. Lett. 309 (3–4), 324–336. https://doi.org/10.1016/j.epsl.2011.07.011
dc.relation.referencesShimizu, K., Shimizu, N., Komiya, T., Suzuki, K., Maruyama, S., Tatsumi, Y., 2009. CO2- rich komatiitic melt inclusions in Cr-spinels within beach sand from Gorgona Island, Colombia. Earth Planet. Sci. Lett. 288 (1–2), 33–43. https://doi.org/10.1016/j. epsl.2009.09.005.
dc.relation.referencesSibille, L., Carpenter, P., Schlagheck, R., French, R.A., 2006. Lunar Regolith Simulant Materials: Recommendations for Standardization, production, and usage (No. NASA/ TP-2006-214605). NASA Technical Publication
dc.relation.referencesStolper, E., McSween Jr., H.Y., 1979. Petrology and origin of the shergottite meteorites. Geochim. Cosmochim. Acta 43 (9), 1475–1498. https://doi.org/10.1016/0016-7037 (79)90142-X.
dc.relation.referencesStorey, M., Mahoney, J.J., Kroenke, L.W., Saunders, A.D., 1991. Are oceanic plateaus sites of komatiite formation? Geology 19 (4), 376–379. https://doi.org/10.1130/ 0091-7613(1991)019<0376:AOPSOK>2.3.CO;2.
dc.relation.referencesSutton, A.J., Higgins, J.P., 2008. Recent developments in meta-analysis. Stat. Med. 27 (5), 625–650. https://doi.org/10.1002/sim.2934.
dc.relation.referencesTaylor, G.J., 2009. Ancient lunar crust: origin, composition, and implications. Elements 5 (1), 17–22. https://doi.org/10.2113/gselements.5.1.17.
dc.relation.referencesTaylor, G.J., Martel, L.M.V., Karunatillake, S., Gasnault, O., Boynton, W.V., 2010. Mapping mars geochemically. Geology 38, 183–186. https://doi.org/10.1130/ G30470.1.
dc.relation.referencesTosca, N.J., Tice, M.M., Hurowitz, J.A., Pedersen, D.A., Henneke, J., Mandon, L., et al., 2025. In situ evidence for serpentinization within the M´aaz Formation, Jezero Crater, Mars. Sci. Adv. 11 (27), eadr8793. https://doi.org/10.1126/sciadv.adr8793.
dc.relation.referencesTreiman, A.H., 2003. Chemical compositions of Martian basalts (shergottites): some inferences on b; formation, mantle metasomatism, and differentiation in mars. Meteorit. Planet. Sci. 38 (12), 1849–1864.
dc.relation.referencesTrikalinos, T.A., Salanti, G., Zintzaras, E., Ioannidis, J.P., 2008. Meta-analysis methods. Adv. Genet. 60, 311–334. https://doi.org/10.1016/S0065-2660(07)00413-0.
dc.relation.referencesVerma, S.K., Oliveira, E.P., Silva, P.M., Moreno, J.A., Amaral, W.S., 2017. Geochemistry of komatiites and basalts from the Rio das Velhas and Pitangui greenstone belts, S˜ao Francisco craton, Brazil: implications for the origin, evolution, and tectonic setting. Lithos 284, 560–577. https://doi.org/10.1016/j.lithos.2017.04.024
dc.relation.referencesVickery, A.M., Melosh, H.J., 1987. The large crater origin of SNC meteorites. Science 237, 738–743. https://doi.org/10.1126/science.237.4816.738.
dc.relation.referencesWaterton, P., Arndt, N., 2023. Komatiites: their geochemistry and origins. In: The Archaean Earth: Tempos and Events (2nd Edition of The Precambrian 12Earth). Elsevier. https://doi.org/10.31223/X5PX0X.
dc.relation.referencesWerner, S.C., Ody, A., Poulet, F., 2014. The source crater of Martian shergottite meteorites. Science 343, 1343–1346. https://doi.org/10.1126/science.1247282.
dc.relation.referencesWyatt, M.B., Hamilton, V.E., McSween, H.Y., Christensen, P.R., Taylor, L.A., 2001. Analysis of terrestrial and Martian volcanic compositions using thermal emission spectroscopy: 1. Determination of mineralogy, chemistry, and classification strategies. J. Geophys. Res. Planets 106, 14711–14732. https://doi.org/10.1029/ 2000JE001356.
dc.relation.referencesWyatt, M.B., McSween, H.Y., 2007, May. TES and GRS compositions of the Martian surface: evidence for igneous and secondary chemical fractionation processes. In: AGU Spring Meeting Abstracts, vol. 2007 pp. P31A-07.
dc.relation.referencesZalewska, N.E., Mroczkowska-Szersze´n, M., Fritz, J., Błęcka, M., 2018. Modeling of surface spectra with and without dust from Martian infrared data: new aspects. Aircr. Eng. Aerosp. Technol. 91 (2), 333–345. https://doi.org/10.1108/AEAT-01- 2018-0051.
dc.rights.accessrightsinfo:eu-repo/semantics/openAccess
dc.rights.coarhttp://purl.org/coar/access_right/c_abf2
dc.rights.licenseAtribución 4.0 Internacional (CC BY 4.0)
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subject.ddc550 - Ciencias de la tierra::552 - Petrología
dc.subject.lembGeochemistry
dc.subject.lembPlanetary geology
dc.subject.lembIgneous rocks
dc.subject.lembBasalts
dc.subject.lembPetrology
dc.subject.lembPlanetary geological evolution
dc.subject.lembVolcanic islands — Colombia
dc.subject.lembGorgona island (Colombia)
dc.subject.lembMagmatism
dc.subject.lembComparative geology
dc.subject.ocde1. Ciencias Naturales
dc.subject.odsODS 15: Vida de ecosistemas terrestres. Proteger, restablecer y promover el uso sostenible de los ecosistemas terrestres, gestionar sosteniblemente los bosques, luchar contra la desertificación, detener e invertir la degradación de las tierras y detener la pérdida de biodiversidad
dc.subject.proposalPlanetary geochemistry
dc.subject.proposalTerrestrial analogs
dc.subject.proposalMineralogy
dc.subject.proposalUltramafic rocks
dc.subject.proposalFigures of merit
dc.titleGorgona Island (Colombia) as a terrestrial analog of Syrtis Major (Mars): Evidence from geochemical meta-analyses and compositional figures of merit
dc.typeArtículo de revista
dc.type.coarhttp://purl.org/coar/resource_type/c_18cf
dc.type.coarversionhttp://purl.org/coar/version/c_970fb48d4fbd8a85
dc.type.contentText
dc.type.driverinfo:eu-repo/semantics/article
dc.type.redcolhttp://purl.org/redcol/resource_type/ART
dc.type.versioninfo:eu-repo/semantics/publishedVersion
dcterms.audienceComunidad Científica y académica.
dspace.entity.typePublication
relation.isAuthorOfPublication74ceb186-b60b-4210-9548-9a89e1a8f37b
relation.isAuthorOfPublication.latestForDiscovery74ceb186-b60b-4210-9548-9a89e1a8f37b

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