Bassett,K.N., Gordon,H.W., Nobes,D.C., & Jacomb,C., “Gardening at the edge: Documenting the limits of tropical Polynesian kumara horticulture in southern New Zealand.” Geoarchaeology 19(3) 2004, 185–218

The original article to which this Erratum refers was published in Geoarchaeology 19(3), 2004, 185–218. Due to an oversight, authorship of the paper by Bassett, K.N., Gordon, H.W., Nobes, D.C., & Jacomb, C. (2004), “Gardening at the edge: Documenting the limits of tropical Polynesian kumara horticulture in southern New Zealand” (Geoarchaeology 19, No. 3, pp. 185–218), was assigned incorrectly. The correct authorship is Hamish W. Gordon, Kari N. Bassett, David C. Nobes, and Chris Jacomb. The authors apologize for this error.     

Comment on “207Pb–206Pb single-zircon evaporation ages of some granitoid rocks reveal continent-oceanic island arc collision during the Cretaceous geodynamic evolution of the Central Anatolian crust, Turkey” – Boztug, D., Tichomirowa, M. & Bombach, K., 2007, JAES 31, 71–86

A continent-oceanic island arc collision model was proposed as a new geodynamic scenario for the evolution of the Cretaceous Central Anatolian granitoids in the Central Anatolian crystalline complex (CACC) by Boztug et al. (2007b) [Boztug, D., Tichomirowa, M., Bombach, K., 2007b. 207Pb–206Pb single-zircon evaporation ages of some granitoid rocks reveal continent-oceanic island arc collision during the Cretaceous geodynamic evolution of the central Anatolian crust, Turkey. Journal of Asian Earth Sciences 31, 71–86]. The key aspects of this model include an intra-oceanic subduction in the Neotethyan Izmir-Ankara Ocean, formation of an island arc and its subsequent collision with the northern margin of the Tauride–Anatolide Platform. The identical scenario was initially proposed by Göncüoglu et al. (1992) [Göncüoglu, M.C., Erler, A., Toprak, V., Yalınız, K., Olgun, E., Rojay, B., 1992. Geology of the western Central Anatolian Massif, Part II: Central Areas. TPAO Report No: 3155, 76 p] . Moreover, the weighted mean values of the reported 207Pb–206Pb single-zircon evaporation ages by Boztug et al. (2007b) [Boztug, D., Tichomirowa, M., Bombach, K., 2007b. 207Pb–206Pb single-zircon evaporation ages of some granitoid rocks reveal continent-oceanic island arc collision during the Cretaceous geodynamic evolution of the central Anatolian crust: Turkey. Journal of Asian Earth Sciences 31, 71–86] from A-type granitoids in the CACC seem to be miscalculated and contrast with the field data.