Towards a climate event stratigraphy for New Zealand over the past 30 000 years (NZ‐INTIMATE project)

• Published in: Journal of Quaternary Science
• Main Authors: Alloway, Brent V., Lowe, David J., Barrell, David J. A., Newnham, Rewi M., Almond, Peter C., Augustinus, Paul C., Bertler, Nancy A. N., Carter, Lionel, Litchfield, Nicola J., McGlone, Matt S., Shulmeister, Jamie, Vandergoes, Marcus J., Williams, Paul W.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2006
• Subjects: Antarctic; New Zealand; Antarc*
• Online Access: http://dx.doi.org/10.1002/jqs.1079; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1079; https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1079

Abstract It is widely recognised that the acquisition of high‐resolution palaeoclimate records from southern mid‐latitude sites is essential for establishing a coherent picture of inter‐hemispheric climate change and for better understanding of the role of Antarctic climate dynamics in the global climate system. New Zealand is considered to be a sensitive monitor of climate change because it is one of a few sizeable landmasses in the Southern Hemisphere westerly circulation zone, a critical transition zone between subtropical and Antarctic influences. New Zealand has mountainous axial ranges that amplify the climate signals and, consequently, the environmental gradients are highly sensitive to subtle changes in atmospheric and oceanic conditions. Since 1995, INTIMATE has, through a series of international workshops, sought ways to improve procedures for establishing the precise ages of climate events, and to correlate them with high precision, for the last 30 000 calendar years. The NZ‐INTIMATE project commenced in late 2003, and has involved virtually the entire New Zealand palaeoclimate community. Its aim is to develop an event stratigraphy for the New Zealand region over the past 30 000 years, and to reconcile these events against the established climatostratigraphy of the last glacial cycle which has largely been developed from Northern Hemisphere records (e.g. Last Glacial Maximum (LGM), Termination I, Younger Dryas). An initial outcome of NZ‐INTIMATE has been the identification of a series of well‐dated, high‐resolution onshore and offshore proxy records from a variety of latitudes and elevations on a common calendar timescale from 30 000 cal. yr BP to the present day. High‐resolution records for the last glacial coldest period (LGCP) (including the LGM sensu stricto ) and last glacial–interglacial transition (LGIT) from Auckland maars, Kaipo and Otamangakau wetlands on eastern and central North Island, marine core MD97‐2121 east of southern North Island, speleothems on northwest South Island, Okarito ...