Biogeodynamics: bridging the gap between surface and deep Earth processes

Life is sustained by a critical and not insubstantial set of elements, nearly all of which are contained within large rock reservoirs and cycled between Earth's surface and the mantle via subduction zone plate tectonics. Over geologic time scales, plate tectonics plays a critical role in recycling subducted bioactive elements lost to the mantle back to the ocean–biosphere system, via outgassing and volcanism. Biology additionally relies on tectonic processes to supply rock-bound ‘nutrients’ to marine and terrestrial ecosystems via uplift and erosion. Thus, the development of modern-style plate tectonics and the generation of stable continents were key events in the evolution of the biosphere on Earth, and similar tectonic processes could be crucial for the development of habitability on exoplanets. Despite this vital ‘biogeodynamic’ connection, directly testing hypotheses about feedbacks between the deep Earth and the biosphere remains challenging. Here, I discuss potential avenues to bridge the biosphere–geosphere gap, focusing specifically on the global cycling and bioavailability of major nutrients (nitrogen and phosphorus) over geologic time scales. This article is part of a discussion meeting issue ‘Earth dynamics and the development of plate tectonics’.

[1]  Donald E. Canfield,et al.  Ocean productivity before about 1.9 Gyr ago limited by phosphorus adsorption onto iron oxides , 2002, Nature.

[2]  D. Stolper,et al.  A record of deep-ocean dissolved O2 from the oxidation state of iron in submarine basalts , 2018, Nature.

[3]  C. Goldblatt,et al.  The Nitrogen Budget of Earth , 2015, 1505.03813.

[4]  K. Zahnle,et al.  Atmospheric science: Ancient air caught by shooting stars , 2016, Nature.

[5]  Heinrich D. Holland,et al.  Volcanic gases, black smokers, and the great oxidation event , 2002 .

[6]  E. Roden,et al.  Microbial acceleration of aerobic pyrite oxidation at circumneutral pH , 2017, Geobiology.

[7]  F. Albarède,et al.  A Zn isotope perspective on the rise of continents , 2013, Geobiology.

[8]  J. Chiarenzelli,et al.  Two Neoarchean supercontinents? Evidence from the Paleoproterozoic , 1998 .

[9]  T. Lenton,et al.  Biotic enhancement of weathering, atmospheric oxygen and carbon dioxide in the Neoproterozoic , 2003 .

[10]  J. Harnmeijer,et al.  Air density 2.7 billion years ago limited to less than twice modern levels by fossil raindrop imprints , 2012, Nature.

[11]  W. Fischer,et al.  Evolution of the global phosphorus cycle , 2016, Nature.

[12]  D. Sverjensky,et al.  Nitrogen speciation in upper mantle fluids and the origin of Earth's nitrogen-rich atmosphere , 2014 .

[13]  Y. Sano,et al.  Speciation and isotope ratios of nitrogen in fluid inclusions from seafloor hydrothermal deposits at ∼ 3.5 Ga , 2007 .

[14]  A. Bekker,et al.  The evolution of the marine phosphate reservoir , 2010, Nature.

[15]  M. Hamilton,et al.  The Paleoproterozoic Marathon Large Igneous Province: New evidence for a 2.1 Ga long-lived mantle plume event along the southern margin of the North American Superior Province , 2008 .

[16]  A. Hofmann,et al.  Evolution of atmospheric xenon and other noble gases inferred from Archean to Paleoproterozoic rocks , 2018, Geochimica et Cosmochimica Acta.

[17]  J. W. Peters,et al.  New insights into the evolutionary history of biological nitrogen fixation , 2013, Front. Microbiol..

[18]  F. Mackenzie,et al.  Experimental Study of Igneous and Sedimentary Apatite Dissolution: Control of pH, Distance from Equilibrium, and Temperature on Dissolution Rates , 2003 .

[19]  Toby Tyrrell,et al.  The relative influences of nitrogen and phosphorus on oceanic primary production , 1999, Nature.

[20]  D. Canfield,et al.  Iron oxides, divalent cations, silica, and the early earth phosphorus crisis , 2015 .

[21]  M. Kunzmann,et al.  Continental flood basalt weathering as a trigger for Neoproterozoic Snowball Earth , 2016 .

[22]  Peter A. Cawood,et al.  The continental record and the generation of continental crust , 2013 .

[23]  S. Poulton.  Sulfide oxidation and iron dissolution kinetics during the reaction of dissolved sulfide with ferrihydrite , 2003 .

[24]  Paul G. Falkowski,et al.  Evolution of the nitrogen cycle and its influence on the biological sequestration of CO2 in the ocean , 1997, Nature.

[25]  F. A. Richards,et al.  The influence of organisms on the composition of sea-water , 1963 .

[26]  G. Henderson,et al.  Lithium-isotope fractionation during continental weathering processes , 2003 .

[27]  Eva E. Stüeken,et al.  Isotopic evidence for biological nitrogen fixation by molybdenum-nitrogenase from 3.2 Gyr , 2015, Nature.

[28]  P. Schroeder,et al.  Illite-smectites diagenesis on and the influence of burial the geochemical cycling of nitrogen , 1998, Clay Minerals.

[29]  R. Berner,et al.  AUTHIGENIC APATITE FORMATION AND BURIAL IN SEDIMENTS FROM NON-UPWELLING, CONTINENTAL MARGIN ENVIRONMENTS , 1993 .

[30]  Peter A. Cawood,et al.  Continental growth seen through the sedimentary record , 2017 .

[31]  J. Harnmeijer,et al.  Earth's air pressure 2.7 billion years ago constrained to less than half of modern levels , 2016 .

[32]  A. Bekker,et al.  Aerobic bacterial pyrite oxidation and acid rock drainage during the Great Oxidation Event , 2011, Nature.

[33]  John H. Martin.  glacial-interglacial Co2 change : the iron hypothesis , 1990 .

[34]  D. Canfield,et al.  Anaerobic ammonium oxidation (anammox) in the marine environment. , 2005, Research in microbiology.

[35]  A. Bekker,et al.  Late Archean to Early Paleoproterozoic global tectonics, environmental change and the rise of atmospheric oxygen , 2005 .

[36]  A. J. Kaufman,et al.  Compositional evolution of the upper continental crust through time, as constrained by ancient glacial diamictites , 2016 .

[37]  Filipa L. Sousa,et al.  The physiology and habitat of the last universal common ancestor , 2016, Nature Microbiology.

[38]  H. Keppler,et al.  Nitrogen solubility in the deep mantle and the origin of Earth's primordial nitrogen budget , 2018 .

[39]  Christopher P. McKay,et al.  A possible nitrogen crisis for Archaean life due to reduced nitrogen fixation by lightning , 2001, Nature.

[40]  Bernhard Schnetger,et al.  A new particulate Mn–Fe–P-shuttle at the redoxcline of anoxic basins , 2010 .

[41]  R. Armstrong,et al.  Radiogenic isotopes: the case for crustal recycling on a near-steady-state no-continental-growth Earth , 1981, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.

[42]  C. Slomp,et al.  Phosphate adsorption in oxidized marine sediments , 1993 .

[43]  G. Cox,et al.  Linking the rise of atmospheric oxygen to growth in the continental phosphorus inventory , 2018 .

[44]  A. Bekker.  Chemostratigraphy of Paleoproterozoic carbonate successions of the Wyoming Craton: tectonic forcing of biogeochemical change? , 2003 .

[45]  P. Falkowski,et al.  Biogeochemical Controls and Feedbacks on Ocean Primary Production , 1998, Science.

[46]  D. Williams,et al.  The Biological Chemistry of the Elements , 1991 .

[47]  F. Horton.  Did phosphorus derived from the weathering of large igneous provinces fertilize the Neoproterozoic ocean? , 2015 .

[48]  Robert A. Berner,et al.  A model for atmospheric CO 2 over Phanerozoic time , 1991 .

[49]  H. Keppler,et al.  Nitrogen speciation in mantle and crustal fluids , 2014 .

[50]  D. Hilton,et al.  Subduction and Recycling of Nitrogen Along the Central American Margin , 2002, Science.

[51]  D. Schrag,et al.  A theory of atmospheric oxygen , 2017, Geobiology.

[52]  D. Canfield,et al.  Ferruginous Conditions: A Dominant Feature of the Ocean through Earth's History , 2011 .

[53]  C. Slomp,et al.  Vivianite is a key sink for phosphorus in sediments of the Landsort Deep, an intermittently anoxic deep basin in the Baltic Sea , 2016 .

[54]  T. Lenton,et al.  Nitrogen-enhanced greenhouse warming on early Earth , 2009 .

[55]  T. Lenton,et al.  Changing tectonic controls on the long‐term carbon cycle from Mesozoic to present , 2014 .

[56]  M. Wiedenbeck,et al.  Nitrogen evolution within the Earth's atmosphere–mantle system assessed by recycling in subduction zones , 2018 .

[57]  E. Stüeken,et al.  Biomass recycling and Earth’s early phosphorus cycle , 2017, Science Advances.

[58]  B. Marty,et al.  Nitrogen Isotopic Composition and Density of the Archean Atmosphere , 2013, Science.

[59]  B. Marty,et al.  Nitrogen Isotopes and Mantle Geodynamics: The Emergence of Life and the Atmosphere–Crust–Mantle Connection , 2013 .

[60]  L. Derry.  Causes and consequences of mid‐Proterozoic anoxia , 2015 .

[61]  P. Cartigny,et al.  Nitrogen isotopes in ophiolitic metagabbros: A re-evaluation of modern nitrogen fluxes in subduction zones and implication for the early Earth atmosphere , 2011 .

[62]  E E Stüeken,et al.  Modeling pN2 through Geological Time: Implications for Planetary Climates and Atmospheric Biosignatures. , 2016, Astrobiology.

[63]  D. Hilton,et al.  Release of subducted sedimentary nitrogen throughout Earth’s mantle , 2016 .

[64]  A. Zerkle,et al.  The geobiological nitrogen cycle: From microbes to the mantle , 2017, Geobiology.

[65]  M. Scambelluri,et al.  Nitrogen recycling in subducted mantle rocks and implications for the global nitrogen cycle , 2014, International Journal of Earth Sciences.

[66]  U. Wand,et al.  Isotopic variations of the fixed nitrogen in metamorphic rocks , 1986 .

[67]  S. Blain,et al.  The Iron Hypothesis , 2016 .

[68]  S. Poulton.  Biogeochemistry: Early phosphorus redigested , 2017 .

[69]  B. Beckmann,et al.  Redox sensitivity of P cycling during marine black shale formation: Dynamics of sulfidic and anoxic, non-sulfidic bottom waters , 2008 .

[70]  A. Bekker,et al.  Oxygen overshoot and recovery during the early Paleoproterozoic , 2012 .

[71]  R. Bustin,et al.  Influence of water column anoxia on the burial and preservation of carbon and phosphorus in marine shales , 1993 .

[72]  C. Goldblatt,et al.  Using raindrops to constrain past atmospheric density , 2015 .

[73]  M. Lilley,et al.  Anomalous CH4 and NH4+ concentrations at an unsedimented mid-ocean-ridge hydrothermal system , 1993, Nature.

[74]  T. Jilbert,et al.  Iron and manganese shuttles control the formation of authigenic phosphorus minerals in the euxinic basins of the Baltic Sea , 2013 .

[75]  Peter A. Cawood,et al.  Earth’s middle age , 2014 .

[76]  L. Gardner,et al.  Contrasting lithium and magnesium isotope fractionation during continental weathering , 2010 .

[77]  A. Knoll,et al.  Proterozoic Ocean Chemistry and Evolution: A Bioinorganic Bridge? , 2002, Science.

[78]  M. Fogel,et al.  High phosphate availability as a possible cause for massive cyanobacterial production of oxygen in the Paleoproterozoic atmosphere , 2013 .

[79]  D. Sverjensky,et al.  The relationship between mantle pH and the deep nitrogen cycle , 2017 .

[80]  J. Korenaga,et al.  Rapid crustal growth and efficient crustal recycling in the early Earth: Implications for Hadean and Archean geodynamics , 2018, Earth and Planetary Science Letters.

[81]  A. Bekker,et al.  Onset of the aerobic nitrogen cycle during the Great Oxidation Event , 2017, Nature.

[82]  L. Heaman.  Global mafic magmatism at 2.45 Ga: Remnants of an ancient large igneous province? , 1997 .

[83]  C. Goldblatt,et al.  A secular increase in continental crust nitrogen during the Precambrian , 2017, 1709.02412.

[84]  R. Dahlgren,et al.  Convergent evidence for widespread rock nitrogen sources in Earth’s surface environment , 2018, Science.