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 …

Since 65 million years ago (Ma), Earth's climate has undergone a significant and complex
evolution, the finer details of which are now coming to light through investigations of deep …

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 …

We present here a new solution for the astronomical computation of the orbital motion of the
Earth spanning from 0 to− 250 Myr. The main improvement with respect to our previous …

We present here a new solution for the astronomical computation of the insolation quantities
on Earth spanning from-250 Myr to 250 Myr. This solution has been improved with respect to …

The S outh A merican continent is composed of several biogeographical regions harbouring
the highest biodiversity on the globe, encompassing five of the world's biodiversity 'hot …

Variations in the 13C/12C value of total dissolved inorganic carbon (DIC) in the world's
oceans through time have been documented through stratigraphic study of marine …

The evolution and subsequent ecological expansion of grasses (Poaceae) since the Late
Cretaceous have resulted in the establishment of one of Earth's dominant biomes, the …

摘要在过去!) 余年中旋回地层学研究得到了极大发展% 对理解和解决地球科学领域众多科学
问题做出了很大贡献& 旋回地层学$9= 2% $</.-/3O.-Q0= & 已被定义为(对地层记录的$ 准& …

A 13-million-year continuous record of Oligocene climate from the equatorial Pacific reveals
a pronounced “heartbeat” in the global carbon cycle and periodicity of glaciations. This …