This study provides a comprehensive and quantitative estimate of how global temperatures
have changed during the last 540 million years. It combines paleotemperature …

Throughout Earth's history, CO2 is thought to have exerted a fundamental control on
environmental change. Here we review and revise CO2 reconstructions from boron isotopes …

Much of our understanding of Earth's past climate comes from the measurement of oxygen
and carbon isotope variations in deep-sea benthic foraminifera. Yet, long intervals in …

Using Pacific benthic foraminiferal δ18O and Mg/Ca records, we derive a Cenozoic (66 Ma)
global mean sea level (GMSL) estimate that records evolution from an ice-free Early Eocene …

The advent of molecular data has transformed the science of organizing and studying life on
Earth. Genetics-based evidence provides fundamental insights into the diversity, ecology …

The replication crisis facing the psychological sciences is widely regarded as rooted in
methodological or statistical shortcomings. We argue that a large part of the problem is the …

Reorganization of the Asian climate from one dominated by global planetary wind systems
to a regional monsoon climate is closely related to the surface uplift of the Tibetan Plateau …

In recent years, the use of ecological niche models (ENMs) and species distribution models
(SDMs) to explore the patterns and processes behind observed distribution of species has …

Abstract The Miocene epoch (23.03–5.33 Ma) was a time interval of global warmth, relative
to today. Continental configurations and mountain topography transitioned toward modern …

摘要青藏高原晚新生代的扩展和隆升对周边环境演变产生重大影响, 确定扩展和隆升的起始年代
是一个重要的科学问题. 近年来在六盘山, 积石山和祁连山及其相邻盆地的研究表明 …