Biotic enhancement of weathering and surface temperatures on earth since the origin of life

Global and Planetary Change

Volumn 4, Issue 4, 1991, Pages 357-371

  Schwartzman, David W ^a   Volk, Tyler ^b  

^a HOWARD UNIVERSITY   (United States)

^b NEW YORK UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 44949276643     PISSN: 09218181     EISSN: None     Source Type: Journal    
DOI: 10.1016/0921-8181(91)90002-E     Document Type: Article

References (65)

1. Age of oceanic plates at subduction and volatile recycling
2. REE and Nd isotope data in BIF from Hammersley, Western Australia: implications for the composition of early Proterozoic seawater
3. Continental tectonics and continental kinetics
4. A model for Sr and Pb isotopic evolution in a dynamic earth
5. Radiogenic isotopes the case for crustal recycling on a near-steady-state no-continental-growth earth
6. The persistent myth of crustal growth
7. The hydrologic cycle: a major variable during Earth history
8. Atmospheric carbon dioxide levels over Phanerozoic time
9. 2 degassing and the carbon cycle: Comment on “Cretaceous ocean crust at DSDP sites 417 and 418: carbon uptake from weathering versus loss by magmatic outgassing”
10. The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years
11. 3.96 Ga gneisses from the Slave province, Northwest Territories, Canada
12. Introduction: an overview of the thermophiles
13. Soll stabilization by a prokaryotic desert crust: implications for Precambrian land biota
14. Chemical weathering in Central Iceland: An analog of pre-Silurian weathering
15. Cometary delivery of organic molecules to the early Earth
16. Carbon exchange between the mantle and crust, and its effect upon the atmosphere: Today compared to Archean time
17. Reply E0S
18. Reply., E0S
19. Neutralization of atmospheric acidity by chemical weathering in an alpine basin in the North Cascade Mountains
20. Geochemical cycles: the continental crust and the oceans
21. Correlation of radiometric ages of Nipissing diabase and Huronian metasediments with Proterozoic orogenic events in Ontario
22. The warm Cretaceous climate role of the long-term carbon cycle
23. A comparative study of the role of lichens and inorganic processes in the chemical weathering of recent Hawaiian lava flows
24. Isotopic and chemical constraints on mantle-crust evolution
25. Nd isotopic variations in Precambrian banded iron formations
26. A Nd isotopic study of the Hamersley and Michipicoten banded iron formations: The source of REE and Fe in Archean oceans
27. Theoretical constraints on oxygen and carbon dioxide concentrations In the Precambrian atmosphere
28. Long-term stability of the Earth's climate
29. 2 levels in Earth's early atmosphere
30. Climate evolution on the terrestrial planet
31. The effect on Earth's surface temperature from variations in rotation rate continent formation solar luminosity and carbon dioxide
32. Geologic and geographic effects on paleoclimate
33. Natural occurrence of silicon carbide in a diamondiferous kimberlite from Fuxian
34. Natural occurrence of silicon carbide in a diamondiferous kimberlite from Fuxian
35. Distribution, chemistry, mineralogy and cycling of the Phanerozoic carbonate mass
36. Impact frustration of the origin of life
37. Longterm climate change and the geochemical cycle of carbon
38. On mantle carbon flux calculated
39. 3He in volatile fluxes from the solid Earth: implications for carbon geodynamics
40. The case for a wet, warm climate on early Mars
41. Earth and Mars: evolution of atmospheres and surface temperatures
42. Isotopic inferences of ancient biochemistries: carbon, sulfur, hydrogen, and nitrogen
43. Biotic enhancement of weathering and the habitability of Earth
44. From abiotic to biotic Earth; the carbon cycle's climatic consequences
45. Cretaceous ocean crust at DSDP Sites417 and 418: carbon uptake from weathering versus loss by magmatic outgassing
46. 2 degassing and the carbon cycle”: A comment by R.A. Berner
47. A new kinetic approach to modeling water-rock interaction: The role of nucleation, precursors and Ostwald ripening
48. Weathering of primary silicate minerals in the natural soil environment in relation to a chemical weathering model
49. The evolution of the terrestrial environment
50. Geochemistry of Precambrian carbonates: I. Archean hydrothermal systems
51. Geochemistry of Precambrian carbonates: II. Archean greenstone belts and Archean sea water
52. 2 to deep-ocean and shallow-ocean carbonate burial
53. Rise of angiosperms as a factor in long-term cooling
54. Climatic factors on the Archean Earth
55. Possible limits on the composition of the Archean ocean
56. Carbon dioxide on the early Earth
57. A negative feedback mechanism for the long-term stabilization of Earth's surface temperature
58. Bacterial Evolution
59. Carbon redox and climate control through Earth history: a speculative reconstruction