English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

Dating ice cores drilled in the high mountain glaciers is difficult\udbecause seasonal variations cannot be traced at depth due to rapid thinning\udof the ice layers. Here we provide the first luminescence dating of the basal\udsediment of the Chongce ice cap in the north-western Tibetan Plateau. Assuming\udthe sediment is of similar (or older) age as the surrounding ice, the\udluminescence dating of 42 ± 4 ka provides an upper constraint for the\udage of the bottom ice at the drilling site. This result is more than 1\udorder of magnitude younger than the previously suggested age of the basal ice\udof the nearby Guliya ice cap (∼ 40 km in distance)

The first luminescence dating of Tibetan glacier basal sediment