Sentence examples for proxy evidence from inspiring English sources

Hetzinger, S. et al. Marine proxy evidence linking decadal North Pacific and Atlantic climate.

In some standardized cases we can appeal to proxy evidence provided by audits and inspections or to readily-available evidence of an institution or agent's track record.

In recent years a growing number of studies have reported proxy evidence for Holocene climatic and environmental change on the Loess Plateau of north-central China.

However, the proxy evidence presented here, supported by model results, suggests that external forcing by solar variability has a considerable impact on multidecadal to centennial ocean atmospheric dynamics, with important effects on regional climate such as European winters.

Here we study hydrological conditions with proxy evidence from marine sediment core NBP0602A-3C, adjacentothetip tip of the Antarctic Peninsula, with sediments dated to 35.9±1.1Ma providing a snapshot of conditions prior to the EOT.

A warm climate is also indicated by a diverse suite of qualitative proxy evidence in E. Beringia, including high frequencies of thaw lake and peatland initiation9; a multi-proxy 'all-temperature' composite record that depicts the dominant mode of variability of all-temperature-sensitive marine and terrestrial records (Fig. 5b); and warmer SSTs as discussed above.

The predicted regional climate changes are highly uncertain, but we note that increasing temperature (T) and monsoon (S) proxy evidences, and lower than average glacial accumulation, are related to higher plague estimates (Y).

We present a novel climate field reconstruction for East Asia using selected multi-proxy evidence.

Kaufman, D. S. et al. Holocene climate changes in eastern Beringia (NW North America)—a systematic review of multi-proxy evidence.

The absence of multi-proxy evidence for a strong climatic reversal during the Younger Dryas from Burial Lake sediments contrasts with some paleorecords showing cooler temperatures and/or dry conditions in northern Alaska at this time.

This episode, marked at the base by a sharp negative carbon-isotope excursion of about 4‰17,18, is documented by multi-proxy evidence of increased rainfall as a sudden increase of coarse and immature siliciclastics into the basin, humid paleosols, hygrophytic pollen assemblages, and massive resin production60,61.