Other Relevant References

• Koski, R. A., Pichler, T., and Foster, A. L. 2001. The fate of arsenic in submarine hydrothermal environments: A summary of recent data. USGS Workshop on Arsenic in the Environment, Denver, Colorado (peer reviewed extended abstract).


• McCarthy, K. T., Pichler, T., and Price, R. E. 2005. Geochemistry of Champagne Hot Springs shallow hydrothermal vent field and associated sediments, Dominica, Lesser Antilles. Chemical Geology (accepted).


• Pichler, T. 2001. The use of ⁸⁷Sr/⁸⁶Sr ratios to document physico-chemical changes in shallow-water hydrothermal systems. In Cidu, R. (Ed.) Water-Rock Interaction, Volume 2: Villasimus, Italy, Balkema, p. 1565-1568. (PDF)


• Pichler, T. 2005. Stable and radiogenic isotopes as tracers for the origin, mixing and subsurface history of fluids in shallow-water hydrothermal systems. Journal of Volcanology and Geothermal Research, 139(3-4):211-226. (PDF)


• Pichler, T. and Dix, G. R. 1996. Hydrothermal venting within a coral reef ecosystem, Ambitle Island, Papua New Guinea. Geology, 20(5):435-438. (PDF)


• Pichler, T., Giggenbach, W. F., McInnes, B. I. A., and Duck, B. 1999. Fe-sulfide formation due to seawater-gas-sediment interaction in a shallow-water hydrothermal system, Lihir Island, Papua New Guinea. Economic Geology, 94(2):281-288. (PDF)


• Pichler, T., Heikoop, J., Risk, M., Veizer, J., and Cambell, I. 2000. Hydrothermal effects on isotope and trace element records in modern reef corals: An introductory study of Porites lobata from Tutum Bay, Ambitle Island, Papua New Guinea. Palaios, 15(3):225-234. (PDF)


• Pichler, T. and Humphrey, J. D. 2001. The formation dolomite in island-arc sediments due to gas-seawater-sediment interaction. Journal of Sedimentary Research, 71(3):394-399. (PDF)


• Pichler, T. and Veizer, J. 1999. Precipitation of Fe(III) oxyhydroxide deposits from shallow-water hydrothermal fluids in Tutum Bay, Ambitle Island, Papua New Guinea. Chemical Geology 162(1):15-31. (PDF)


• Pichler, T. and Veizer, J. 2004. The precipitation of aragonite from shallow-water hydrothermal fluids in a coral reef, Tutum Bay, Ambitle Island, Papua New Guinea. Chemical Geology, 207(1-2):31-45. (PDF)


• Pichler, T., Veizer, J., and Hall, G. E. M. 1999. The chemical composition of shallow-water hydrothermal fluids in Tutum Bay, Ambitle Island, Papua New Guinea and their effect on ambient seawater. Marine Chemistry, 64(3):229-252. (PDF)


• Pichler, T., Veizer, J., and Hall, G. E. M. 1999. Natural input of arsenic into a coral-reef ecosystem by hydrothermal fluids and its removal by Fe(III) oxyhydroxides. Environmental Science & Technology, 33(9):1373-1378. (PDF)


• Rancourt, D. G., Fortin, D., Pichler, T., and Lamarche, G. 2001. Mineralogical characterization of a natural very As-rich hydrous ferric oxide coprecipitate formed by mixing of hydrothermal fluid and sea water. American Mineralogist, 86:834-851. (PDF)