Citation: David W. Schwartzman. Life’s Critical Role in the Long-term Carbon Cycle: the Biotic Enhancement of Weathering[J]. AIMS Geosciences, 2017, 3(2): 216-238. doi: 10.3934/geosci.2017.2.216
[1] | Brantley SL, Megonigal JP, Scatena FN, et al. (2011) Twelve testable hypotheses on the geobiology of weathering. Geobiology 9: 140-165. |
[2] | Akob DM, and Küsel K (2011) Where microorganisms meet rocks in the Earth's Critical Zone. Biogeosciences 8: 3531-3543. doi: 10.5194/bg-8-3531-2011 |
[3] | Brecheisen ZS, Richter D deB (2014) Ordering interfluves: a simple proposal for understanding critical zone evolution. Procedia Earth Planetary Sci 10: 77–81. |
[4] | Field JP, Breshears DD, Law DJ, et al. (2015) Critical Zone Services: Expanding Context, Constraints, and Currency beyond Ecosystem Services. Vadose Zone J 14. |
[5] | Summers S, Thomson BC, Whiteley A, et al. (2016). Mesophilic mineral weathering bacteria inhabit the critical-zone of a perennially cold basaltic environment. Geomicrobiology J 33: 52-62. |
[6] | Schwartzman DW, Volk T (1989) Biotic enhancement of weathering and the habitability of Earth. Nat 340: 457-460. doi: 10.1038/340457a0 |
[7] | Schwartzman D (1999 2002) Life, Temperature, and the Earth: The Self-Organizing Biosphere. New York: Columbia University Press. |
[8] | Schwartzman DW (2008) Coevolution of the Biosphere and Climate, In: S.E. Jorgensen SE, Fath B (eds.), Encyclopedia of Ecology, 1st Edition, Oxford: Elsevier B.V., 648-658. |
[9] | Brantley SL, Lebedeva M, Hausrath EM (2012) A geobiological view of weathering and erosion. In Knoll AH, Canfield DE, Konhauser KO (eds.) Fundamentals of Geobiology, 1st Edition., Oxford: Blackwell Publishing Ltd., 205-227. |
[10] | Lovelock JE, Watson AJ (1982) The regulation of carbon dioxide and climate: Gaia or geochemistry. Planet. Space Sci. 30: 795-802. |
[11] | Richter D deB, Billings SA (2015) "One physical system": Tansley's ecosystem as Earth's critical zone. New Phytol 206: 900-912. |
[12] | Bray AW, Oelkers EH, Bonneville S, et al. (2013) How bugs get their food: Linking mineral surface chemistry to nutrient availability. Mineral Mag 77: 765. |
[13] | Quirk J, Beerling DJ, Banwart SA, et al. (2012) Evolution of trees and mycorrhizal fungi intensifies silicate mineral weathering. Biol Lett 8: 1006-1011. |
[14] | Quirk J, Andrews MY, Leake JR, et al. (2014) Ectomycorrhizal fungi and past high CO2 atmospheres enhance mineral weathering through increased below-ground carbon-energy fluxes. Biol Lett 10: 387-393. |
[15] | Quirk J, Leake JR, Banwart SA, et al. (2014) Weathering by tree-root-associating fungi diminishes under simulated Cenozoic atmospheric CO2 decline. Biogeosciences 11: 321-331. doi: 10.5194/bg-11-321-2014 |
[16] | Burghelea C, Zaharescu DG, Dontsova K, et al. (2015) Mineral nutrient mobilization by plants from rock: influence of rock type and arbuscular mycorrhiza. Biogeochemistry 124:187-203. doi: 10.1007/s10533-015-0092-5 |
[17] | Callesen I, Harrison R, Stupak I, et al. (2016) Carbon storage and nutrient mobilization from soil minerals by deep roots and rhizospheres. For Ecol Manage 359: 322-331. doi: 10.1016/j.foreco.2015.08.019 |
[18] | Quirk J, Leake JR, Johnson DA, et al. (2015) Constraining the role of early land plants in Palaeozoic weathering and global cooling. Proc R Soc B 282: 20151115. |
[19] | Taylor LL, Leake JR, Quirk J, et al. (2009) Biological weathering and the long-term carbon cycle: integrating mycorrhizal evolution and function into the current paradigm. Geobiology 7: 171-191. doi: 10.1111/j.1472-4669.2009.00194.x |
[20] | Lucas Y (2001) The role of plants in controlling rates and products of weathering: Importance of biological pumping. Annu Rev Earth Planet Sci 29: 135-163. |
[21] | Buss HL, Sak PB, Webb SM, et al. (2008) Weathering of the Rio Blanco quartz diorite, Luquillo Mountains, Puerto Rico: Coupling oxidation, dissolution, and fracturing. Geochim Cosmochim Acta 72: 4488-4507. |
[22] | Navarre-Sitchler AK, Cole DR, Rother G, et al. (2013) Porosity and surface area evolution during weathering of two igneous rocks. Geochim Cosmochim Acta 109: 400-413. doi: 10.1016/j.gca.2013.02.012 |
[23] | Dorn RI (2014) Ants as a powerful biotic agent of olivine and plagioclase dissolution. Geol 42: 771-774. |
[24] | Chadwick OA, Derry LA, Vitousek PM, et al. (1999) Changing sources of nutrients during four million years of ecosystem development. Nat 397: 491-497. doi: 10.1038/17276 |
[25] | Chadwick KD, Asner GP (2016) Tropical soil nutrient distributions determined by biotic and hillslope processes. Biogeochemistry 127: 273-289. |
[26] | Porder S, Clark DA, Vitousek PM (2006) Persistence of rock-derived nutrients in the wet tropical forests of La Selva, Costa Rica. Ecology 87: 594-602. doi: 10.1890/05-0394 |
[27] | Callesen I, Harrison R, Stupak I, et al. (2016) Carbon storage and nutrient mobilization from soil minerals by deep roots and rhizospheres. For Ecol Manage 359: 322-331. doi: 10.1016/j.foreco.2015.08.019 |
[28] | Calmels D, Gaillardet J, Brenot A, et al. (2007) Sustained sulfide oxidation by physical erosion processes in the Mackenzie River basin: Climatic perspectives. Geol 35: 1003-1006. doi: 10.1130/G24132A.1 |
[29] | Torres MA, West AJ, Li G (2014) Sulphide oxidation and carbonate dissolution as a source of CO2 over geological timescales. Nat 507: 346-349. doi: 10.1038/nature13030 |
[30] | Torres MA, West AJ, Clark KE (2015) Geomorphic regime modulates hydrologic control of chemical weathering in the Andes–Amazon. Geochim Cosmochim Acta 166: 105–128. |
[31] | Caves JK, Jost AB, Laub KV, et al. (2016) Cenozoic carbon cycle imbalances and a variable weathering feedback. Earth Planet Sci Lett 450: 152-163. doi: 10.1016/j.epsl.2016.06.035 |
[32] | West AJ, Torres M, Moosdorf N, et al. (2016) Glacial weathering, sulfide oxidation, and the geologic evolution of CO2. Goldschmidt Conf Abstr 3402. |
[33] | Larson DW (1987) The absorption and release of water by lichens. In: Peveling E (ed.), Progress and Problems in Lichenology in the Eighties, Bibliothca lichenological 25, Berlin:J. Cramer, 351-360. |
[34] | Li Z, Liu L, Chen J, Teng HH (2016) Cellular dissolution at `hypha-and spore-mineral interfaces revealing unrecognized mechanisms and scales of fungal weathering. Geol 44: 319-322. doi: 10.1130/G37561.1 |
[35] | Jones D, Wilson MJ (1985) Chemical activity of lichens on mineral surfaces; a review. Int Biodeterior 21: 99-104. |
[36] | Chen J, Blume H-P, Beyer L (2000) Weathering of rocks induced by lichen colonization–a review. Catena 39: 121-146. doi: 10.1016/S0341-8162(99)00085-5 |
[37] | Amundson R, Heimsath A, Owen, et al. (2015) Hillslope soils and vegetation. Geomorphol 234: 122-13. doi: 10.1016/j.geomorph.2014.12.031 |
[38] | Hahm WJ, Riebe CS, Lukens CE, et al. (2014) Bedrock composition regulates mountain ecosystems and landscape evolution. Proc Natl Acad Sci USA. 111: 3338-3343. doi: 10.1073/pnas.1315667111 |
[39] | Schwartzman DW (2015) The case for a hot Archean climate and its implications to the history of the biosphere. Arxiv org April 1. |
[40] | Sheldon ND (2006) Precambrian paleosols and atmospheric CO2 levels. Precambrian Res 147: 148-155. doi: 10.1016/j.precamres.2006.02.004 |
[41] | Hren MT, Tice MM, Chamberlain CP (2009) Oxygen and hydrogen isotope evidence for a temperate climate 3.42 billion years ago. Nat 462: 205-208. |
[42] | Blake RE, Chang SJ, Lepland A (2010) Phosphate oxygen isotopic evidence for a temperate and biologically active Archaean ocean. Nat 464: 1029-1032. doi: 10.1038/nature08952 |
[43] | Rosing MT, Bird DK, Sleep NH, et al. (2010) No climate paradox under the faint early Sun. Nat 464: 744-747. |
[44] | Driese SG, Jirsa MA, Ren M, et al. (2011) Neoarchean paleoweathering of tonalite and metabasalt: Implications for reconstructions of 2.69 Ga early terrestrial ecosystems and paleoatmospheric chemistry. Precambrian Res 189: 1-17. |
[45] | Sheldon, ND, Tabor, NJ (2009) Quantitative paleoenvironmental and paleoclimatic reconstruction using paleosols. Earth-Sci Rev 95: 1-52. doi: 10.1016/j.earscirev.2009.03.004 |
[46] | de Wit MJ, Furnes H (2016) 3.5-Ga hydrothermal fields and diamictites in the Barberton Greenstone Belt-Paleoarchean crust in cold environments. Sci Adv 2: e1500368. |
[47] | Airapetian VS , Glocer A, Grono G, et al. (2016) Prebiotic chemistry and atmospheric warming of early Earth by an active young Sun. Nat Geosci 9: 452-455. |
[48] | Som, SM, Buick R, Hagadorn JW, et al. (2016) Earth's air pressure 2.7 billion years ago constrained to less than half of modern levels. Nat Geosci 9: 448-451. |
[49] | Som SM, Catling DC, Harnmeijer JP, et al. (2012) Air density 2.7 billion years ago limited to less than twice modern levels by fossil raindrop imprints. Nat 484: 359-362. |
[50] | Kavanagh L, Goldblatt C (2015) Using raindrops to constrain past atmospheric density. Earth Planet Sci Lett 413: 51-58. doi: 10.1016/j.epsl.2014.12.032 |
[51] | Sahagian D, Proussevitch A (2007) Paleoelevation measurement on the basis of vesicular basalts. Rev Mineral Geochem 66: 195-213. doi: 10.2138/rmg.2007.66.8 |
[52] | Fournier, GP, Alm, E J (2015) Ancestral Reconstruction of a Pre-LUCA Aminoacyl-tRNA Synthetase Ancestor Supports the Late Addition of Trp to the Genetic Code. J Mol Evol 80: 171-185. doi: 10.1007/s00239-015-9672-1 |
[53] | Romero-Romero ML, Risso VA, Martinez-Rodriguez S, et al. (2016) Selection for Protein Kinetic Stability Connects Denaturation Temperatures to Organismal Temperatures and Provides Clues to Archaean Life. PLoS ONE, 11: e0156657. doi: 10.1371/journal.pone.0156657 |
[54] | Tartèse, R, Chaussidon M, Gurenko A, et al. (2017) Warm Archean oceans reconstructed from oxygen isotope composition of early-life remnants. Geochem Perspect Lett 3: 55-65. |
[55] | Schwartzman DW, Volk T (1991) Biotic enhancement of weathering and surface temperatures on Earth since the origin of life. Glob Planet Change Sect 4: 357-371. |
[56] | Kasting JF, Ackerman TP (1986) Climatic consequences of a very high CO2 level in Earth's early atmosphere. Sci 234: 1383-1385. doi: 10.1126/science.11539665 |
[57] | Charnay B, Forget F, Wordsworth R, et al. (2013) Exploring the faint young Sun problem and the possible climates of the Archean Earth with a 3-D GCM. J Geophys Res: Atmos 118: 1-18. |
[58] | Le Hir G, Teitler Y, Fluteau F, et al. (2014) The faint young Sun problem revisited with a 3-D climate–carbon model–Part 1. Clim Past 10: 697-713. doi: 10.5194/cp-10-697-2014 |
[59] | Flament N, Coltice N, Rey PF (2013) The evolution of the 87Sr/86Sr of marine carbonates does not constrain continental growth. Precambrian Res 229: 177-188. |
[60] | Jellinek AM, Jackson MG (2015) Connections between the bulk composition, geodynamics and habitability of Earth. Nat Geosci 8: 587-593. doi: 10.1038/ngeo2488 |
[61] | Dessert C, Dupre B, Gaillardet J, et al. (2003) Basalt weathering laws and the impact of basalt weathering on the global carbon cycle. Chem Geol 202: 257-273. doi: 10.1016/j.chemgeo.2002.10.001 |
[62] | Dupre B, Dessert C, Oliva P, et al. (2003) Rivers, chemical weathering and Earth's climate. C R Geosciences 335: 1141-1160. doi: 10.1016/j.crte.2003.09.015 |
[63] | Ibarra DE, Caves JK, Moon S, et al. (2016) Differential weathering of basaltic and granitic catchments from concentration discharge relationships. Geochim Cosmochim Acta 190: 265-293. doi: 10.1016/j.gca.2016.07.006 |
[64] | Navarre-Sitchler A, Brantley S (2007) Basalt weathering across scales. Earth Planetary Sci Lett 261: 321-334. |
[65] | Eggleston CM, Hochella MF Jr, Parks GA (1989) Sample preparation and aging effects on dissolution rate and surface composition of diopside. Geochim Cosmochim Acta 53: 979-804. |
[66] | White AF, Brantley SL ( 2003) The effect of time on the weathering of silicate minerals: why do weathering rates differ in the laboratory and field? Chem Geol 202: 479-506. |
[67] | Grandstaff DE (1986) The dissolution rate of forsteritic olivine from Hawaiian beach sand. In: Coleman S, Dethier D (eds.) Rates of Chemical Weathering of Rocks and Minerals., New York: Academic Press, New York, 41-59. |
[68] | Rimstidt JD, Brantley SL, Olsen AA (2012) Systematic review of forsterite dissolution rate data. Geochim Cosmochim Acta 99: 159-178. doi: 10.1016/j.gca.2012.09.019 |
[69] | Wolff-Boenisch D, Gislason SR, Oelkers EH, et al. (2004) The dissolution rates of natural glasses as a function of their composition at pH 4 and 10.6, and temperatures from 25 to 74°C. Geochim Cosmochim Acta 68: 4843-4858. |
[70] | Shikazono N, Takino A, Ohtani, H (2005) An estimate of dissolution rate constant of volcanic glass in volcanic ash soil from the Mt. Fuji area, central Japan. Geochem J 39: 185-196. |
[71] | Gao G-L, Ding G-E, Wu B, et al. (2014) Fractal Scaling of Particle Size Distribution and Relationships with Topsoil Properties Affected by Biological Soil Crusts. PLoS ONE 9: e88559. doi: 10.1371/journal.pone.0088559 |
[72] | Schwartzman DW, Volk T (2015) Habitability for Complex Life and the Development and Self-Limitations of the Biotic Enhancement of Weathering, Puzzle of Earths Uninterrupted Habitability, Abstract Book, 12, London: Geological Society. |
[73] | Rad S, Rivé K, Vittecoqa B, et al. (2013) Chemical weathering and erosion rates in the Lesser Antilles: An overview in Guadeloupe, Martinique and Dominica. J South Am Earth Sci 45: 331-344. doi: 10.1016/j.jsames.2013.03.004 |
[74] | Hartmann J, Moosdorf N, Lauerwald R, et al. (2014) Global chemical weathering and associated P-release-The role of lithology, temperature and soil properties. Chem Geol 363: 145-163. |
[75] | Rivé K, Gaillardet J, Agrinier P, et al. (2013) Carbon isotopes in the rivers from the Lesser Antilles: origin of the carbonic acid consumed by weathering reactions in the Lesser Antilles. Earth Surf Processes Landforms 38: 1020-1035. doi: 10.1002/esp.3385 |
[76] | Maher K, Chamberlain CP (2014) Hydrologic regulation of chemical weathering and the geologic carbon cycle. Sci 343: 1502-1504. |
[77] | Murphy BP, Johnson JPL, Gasparini NM, et al. (2016) Chemical weathering as a mechanism for the climatic control of bedrock river incision. Nat 532: 223-237. doi: 10.1038/nature17449 |
[78] | Anders AM (2016) How rain affects rock and rivers. Nat 532: 186-187. doi: 10.1038/532186a |
[79] | Van Cappellen P (2013) Where groundwater meets surface water. Mineral Mag 77: 2388. |
[80] | Clair JSt, Moon S, Holbrook WS, et al. (2015) Geophysical imaging reveals topographic stress control of bedrock weathering. Sci 350: 534-538. doi: 10.1126/science.aab2210 |
[81] | Anderson RS (2015) Pinched topography initiates the critical zone. Sci 350: 506-507. |
[82] | Bazilevskaya E, Lebedeva M, Pavich M, et al. (2013) Where fast weathering creates thin regolith and slow weathering creates thick regolith. Earth Surf Process Landform 38: 847-858. |
[83] | West AJ (2012) Thickness of the chemical weathering zone and implications for erosional and climatic drivers of weathering and for carbon-cycle feedbacks. Geol 40: 811-814. doi: 10.1130/G33041.1 |
[84] | Herman F, Seward D, Valla PG, et al. (2013) Worldwide acceleration of mountain erosion under a cooling climate. Nat 504: 423-426. doi: 10.1038/nature12877 |
[85] | Galy V, Peucker-Ehrenbrink B, Eglinton T (2015) Global carbon export from the terrestrial biosphere controlled by erosion. Nat 521: 204-207. doi: 10.1038/nature14400 |
[86] | Li G, Hartmann J, Derry LA, et al. (2016) Temperature dependence of basalt weathering. Earth Planet Sci Lett 443: 59-69. doi: 10.1016/j.epsl.2016.03.015 |
[87] | Torres MA, West AJ, Clark KE, et al. (2016) The acid and alkalinity budgets of weathering in the Andes–Amazon system: Insights into the erosional control of global biogeochemical cycles. Earth Planet Sci Lett 450: 381–391. |
[88] | Pelak NF, Parolari AJ , Porporato A (2016) Bistable plant–soil dynamics and biogenic controls on the soil production function. Earth Surf Process Landforms 41: 1011-1017. |
[89] | Buendía C, Arens S, Hickler T, et al. (2014) On the potential vegetation feedbacks that enhance phosphorus availability - insights from a process-based model linking geological and ecological timescales. Biogeosciences 11: 3661-3683. doi: 10.5194/bg-11-3661-2014 |
[90] | Porada P, Weber B, Elbert W, et al. A (2014) Estimating impacts of lichens and bryophytes on global biogeochemical cycles. Global Biogeochem. Cycles 28: 71-85. doi: 10.1002/2013GB004705 |
[91] | Kelemen PB, Matter J (2008) In situ carbonation of peridotite for CO2 storage. Proc Natl Acad Sci USA105: 17295-17300. |
[92] | Schuiling RD, de Boer PL (2011) Rolling stones, fast weathering of olivine in shallow seas for cost-effective CO₂ capture and mitigation of global warming and ocean acidification. Earth Syst Dynam Discuss 2: 551-568. doi: 10.5194/esdd-2-551-2011 |
[93] | Ten Berge HFM., van der Meer HG, Steenhuizen JW, et al. (2012) Olivine weathering in soil, and its effects on growth and nutrient uptake in ryegrass (Lolium perenne L.). A Pot Experiment. PLOS One 7: e42098. doi: 10.1371/journal.pone.0042098 |
[94] | Hartmann J, West AJ, Renforth P, et al. (2013) Enhanced chemical weathering as a geoengineering strategy to reduce atmospheric carbon dioxide, supply nutrients, and mitigate ocean acidification. Rev Geophys 51: 113-149. doi: 10.1002/rog.20004 |
[95] | Matter JM, Stute M, Snaebjörnsdottir SO, et al. (2016) Rapid carbon mineralization for permanent disposal of anthropogenic carbon dioxide emissions. Sci 352: 1312-1314. |
[96] | Taylor LL, Quirk J, Thorley RMS, et al. (2016) Enhanced weathering strategies for stabilizing climate and averting ocean acidification. Nat Clim Change 6: 402–406. |
[97] | Schuiling RD (2017) Olivine weathering against climate change. Natural Science 9: 21-26. |
[98] | Juarez S, Dontsova K, Le Galliard J-F , et al. (2016) Effect of elevated CO2 and temperature on abiotic and biologically-driven basalt weathering and C sequestration. Geophys Res Abstr 18. |
[99] | Navarre-Sitchler AK, Cole DR, Rother G, et al. (2013) Porosity and surface area evolution during weathering of two igneous rocks. Geochim Cosmochim Acta 109: 400-413. |
[100] | Navarre-Sitchler A, Brantley S, Rother G (2015) How Porosity Increases During Incipient Weathering of Crystalline Silicate Rocks. Rev Mineral Geochem 80: 331-354. |
[101] | Aghamiri R, Schwartzman DW (2002) Weathering rates of bedrock by lichens: a mini watershed study. Chem Geol 188: 249-259. |
[102] | Zambell CB, Adams JM, Goring ML, et al. (2012) Effect of lichen colonization on chemical weathering of hornblende granite as estimated by aqueous elemental flux. Chem Geol 291: 166-174. |
[103] | Jackson TA, Keller WD (1970) A comparative study of the role of lichens and inorganic processes in the chemical weathering of recent Hawaiian lava flows. Am J Sci 269: 446-466. doi: 10.2475/ajs.269.5.446 |
[104] | Brady PV, Dorn RI, Brazel AJ, et al. (1999) Direct measurement of the combined effects of lichen, rainfall, and temperature on silicate weathering. Geochim Cosmochim Acta 63: 3293-3300. |
[105] | Stretch RC, Viles HA (2002) The nature and rate of weathering by lichens on lava flows on Lanzarote. Geomorphol 47: 87-94. doi: 10.1016/S0169-555X(02)00143-5 |
[106] | Lenton TM, Crouch M, Johnson M, et al. (2012) First plants cooled the Ordovician. Nat Geosci 5: 86-89. doi: 10.1038/ngeo1390 |
[107] | Moulton KL, Berner RA (1998) Quantification of the effect of plants on weathering: studies in Iceland. Geol 26: 895-898. |
[108] | Bormann BT, Wang D, Bormann FH, et al. (1998) Rapid, plant-induced weathering in an aggrading experimental ecosystem. Biogeochemistry 43: 129-155. doi: 10.1023/A:1006065620344 |
[109] | Berner RA, Kothaval Z (2001) Geocarb III: A revised model of atmospheric CO2 over Phanerozoic time. Am J Sci 301: 182-204. doi: 10.2475/ajs.301.2.182 |
[110] | Berner RA (2006) GEOCARBSULF: A combined model for Phanerozoic atmospheric O2 and CO2. Geochim Cosmochim Acta 70: 5653-5664. doi: 10.1016/j.gca.2005.11.032 |
[111] | Berner RA, Kothaval Z (2001) Geocarb III: A revised model of atmospheric CO2 over Phanerozoic time. Am J Sci 301: 182-204. |
[112] | Royer DL, Berner RA, Montanez IP, et al. (2004) CO2 as a primary driver of Phanerozoic climate. GSA Today 14: 4-10. |
[113] | Taylor LL, Banwart SA, Valdes PJ, et al. (2012) Evaluating the effects of terrestrial ecosystems, climate and carbon dioxide on weathering over geological time: a global-scale process-based approach. Phil. Trans. R. Soc. B, 367: 565-582. doi: 10.1098/rstb.2011.0251 |
[114] | Arens S, Kleidon A (2011) Eco-hydrological versus supply-limited weathering regimes and the potential for biotic enhancement of weathering at the global scale. Appl Geochem 26: S274-S278. doi: 10.1016/j.apgeochem.2011.03.079 |
[115] | Von Bloh W, Bounama C, Eisenack K, et al. (2008) Estimating the biogenic enhancement factor of weathering using an inverse viability method. Ecol Modell 216: 245-251. |
[116] | Schwartzman DW, Brantley S (2013) The Geobiology of Weathering: the 13th Hypothesis. Mineral Mag 77: 2170. |
[117] | Beraldi-Campesi H (2013) Early life on land and the first terrestrial ecosystems. Available from: http://www.ecologicalprocesses.com/content/2/1/1. |
[118] | Rastogi RP, Sinha RP, Moh SH, et al. (2014) Ultraviolet radiation and cyanobacteria. J Photochem Photobiol B 141: 154-169. doi: 10.1016/j.jphotobiol.2014.09.020 |
[119] | Lalonde SV, Konhauser KO (2015) Benthic perspective on Earth's oldest evidence for oxygenic photosynthesis. Proc Natl Acad Sci USA 112: 995-1000. doi: 10.1073/pnas.1415718112 |
[120] | Gauger T, Konhauser K, Kappler A (2015) Protection of phototrophic iron(II)-oxidizing bacteria from UV irradiation by biogenic iron(III) minerals: Implications for early Archean banded iron formation. Geol 43 (12): 1067-1070. |
[121] | Lenton TM, Daines SJ (2016) Matworld-the biogeochemical effects of early life on land. New Phytol doi: 10.1111/nph.14338. |
[122] | Garcia AK, Schopf JW, Yokobori S-i, et al. (2017) Reconstructed ancestral enzymes suggest long-term cooling of Earth's photic zone since the Archean. Proc Natl Acad Sci USA 114: 4619-4624. |
[123] | Sleep NH, Zahnle K, Carbon dioxide cycling and implications for climate on ancient Earth. J Geophys Res 106: 1373-1399. |
[124] | Kanzaki Y, Murakami T (2015) Estimates of atmospheric CO2 in the Neoarchean–Paleoproterozoic from paleosols. Geochim Cosmochim Acta 159: 190-219. |