Mean annual temperature in New Zealand during the last glacial maximum derived from dissolved noble gases in groundwater
详细信息 查看全文
- 作者：A.M. Seltzera ; b ; aseltzer@ucsd.edu" class="auth_mail" title="E-mail the corresponding author ; M. Stutea ; c ; d ; U. Morgensterne ; M.K. Stewarte ; f ; J.M. Schaefera ; c
- 关键词：last glacial maximum ; LGM ; New Zealand ; noble gas ; paleotemperature ; groundwater
- 刊名：Earth and Planetary Science Letters
- 出版年：2015
- 出版时间：1 December 2015
- 年：2015
- 卷：431
- 期：Complete
- 页码：206-216
- 全文大小：884 K
文摘
- •
Dissolved noble gases in groundwater imply New Zealand was 3.7–6.2 °C colder during the LGM.
- •
This value is close to most terrestrial and marine New Zealand LGM reconstructions.
- •
Noble gases also successfully reproduce measured soil temperatures in modern samples.