 An example of this is the Sajama ice core (Bolivia), for which the timing of the DCR has been pinned to that of the GISP2 ice core record (central Greenland).Climatic change in the central Andes during the DCR, however, was significant and was characterized by a shift to much wetter and likely colder conditions.The magnitude and abruptness of the changes would suggest that low latitude climate did not respond passively during the YD/DCR.