Depth to pedogenic carbonate horizon as a paleoprecipitation indicator?: Comment and Reply: Comment

Geology

Volumn 28, Issue 6, 2000, Pages 572-

  Retallack, Gregory J ^a  

^a UNIVERSITY OF OREGON   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CARBONATE; PEDOGENESIS;

EID: 80053986322     PISSN: 00917613     EISSN: 19432682     Source Type: Journal    
DOI: 10.1130/0091-7613(2000)28<572a:DTPCHA>2.0.CO;2     Document Type: Article

References (6)

1. Arkley, R.J., 1963, Calculation of carbonate and water movement in soil from climatic data: Soil Science, v. 96, p. 239-248.
2. Birkeland, P.W., 1984, Soils and geomorphology: New York, Oxford University Press, 372 p.
3. Jenny, H., 1941, Factors in soil formation: New York, McGraw-Hill, 281 p.
4. Retallack, G.J., 1994, The environmental factor approach to the interpretation of paleosols, in Amundson, R., et al., eds., Factors of soil formation: A fiftieth anniversary retrospective: Soil Science Society of America Special Publication 33, p. 31-64.
5. Royer, D.L., 1999, Depth to pedogenic carbonate horizon as a paleoprecipitation indicator?: Geology, v. 27, p. 1123-1126.
6. Yaalon, G.H., 1983, Climate, time and soil development, inWilding, L.P., et al., eds., Pedogenesis and soil taxonomy: Concepts and interactions: Amsterdam, Elsevier, p. 233-251.