paleoclimate

The oxygen and carbon isotopes in biogenic carbonate have been extensively used in paleoclimate and paleoenvironment studies.

The main control factors created by the sequence and the domain include tectonic movement and the changes of base level and paleoclimate.

Jingyuan loess deposition thickness, Information of paleoclimate evolution was high resolution.

Clay minerals are widely applied in reconstructing paleoclimate , and many analysis methods are involved .

The whole Jurassic represented a complete shallow-deep-shallow palaeogeography and dry-moist-dry paleoclimate cycle.

Rapid climate changes at millennial and centennial scales are one of the most important aspects in Paleoclimate study.

Chaoshui basin experienced paleoclimate evolution period from arid, relatively humid, arid-humid during Early Cretaceous.

Paleoclimate in the Cretaceous period was characterized by space -time inhomogeneity.

The humid to semi-humid paleoclimate in the sedimentation epoch of Yaojia formation was favorite for the formation of uranium rich strata.

my paleoclimate model to track the next events.

This investigation is very significant for the further studies on paleoclimate and paleoceanography in the Bering Sea.

Paleoclimate The climate conditions of geologic periods in the ancient past.

Present use of biomarkers to reconstruct paleoclimate and ancient human activities has become an important part of molecular stratigraphy.

The study of aragonite stalagmites is important to reconstruct the paleoclimate and know mineralization in both theory and practice.

Pollen analysis helped to find out the paleoclimate information.

Quantitative research is necessary for the paleoclimate reconstruction on the Chinese Loess Plateau.

Organic carbon isotope records of the Poyang Lake sediments and their implications for the paleoclimate during the last 8 ka

In particular, Cave dropstones stalagmites offered us a kind of distinctive data source as continental paleoclimate archives.

Simulation of the last glacial inception with the green McGill Paleoclimate Model

Study of the Paleoclimate Based on the Comparison Between Thermal Ionization Mass Spectrometry Uranium Series Dating and Oxygen Isotopes

Advances in East Asian Paleoclimate Modelling for the Last Glacial Maximum by China

Oxygen isotope records for carbonates from closed-basin lakes as environmental archives for paleoclimate reconstruction

Paleoclimate Indicator and Quantitative Determination of Paleotemperature in the Cretaceous Red Beds

Basin Tectonic Setting and Paleoclimate Revealed from Minerals and Geochemistry of the Sediments

Size Distribution of Chinese Loess and Its Paleoclimate Implication

carbon , hydrogen oxygen isotope studies on imbedded old tree ring and paleoclimate reconstruction

An Analysis for Sedimentary System, Evolution, and Paleoclimate in the Litang Basin in West Sichuan in Quaternary

Application of Historical Document in the Study of Holocene Geographical Environment Change--A case study of paleoclimate

Application of Oxygen Isotope to High-Resolution Paleoclimate Researches

Numerical modeling in paleoclimate study: Progress and problems

Paleoclimate Characteristics in Xinjiang in Geologic Time

A Millennial Scale Mid-Pleistocene Paleoclimate Record of Planktonic Foraminifera from the Northern South China Sea Site 1144

Last Glacial Maximum in South America: Paleoclimate proxies and model results

The Loess Deposition Features and Paleoclimate in Westerly Region of Xinjiang

Petrogeochemical characteristics of Lower Cretaceous and Pliocene rocks and paleoclimate evolution in Wulanhua region

An Approach to Paleoclimate-Reconstruction by Clay Minerals

Research on the Quaternary Laterite and Paleoclimate in the Dongting Basin

Early Tertiary fossil plants and paleoclimate of Lanzhou Basin

Clay minerals as indicators of paleoclimate

Loess and Evolution of Paleoclimate

It is important to note the isolation of the paleoclimate community;

The Development and Application of Climate Model in Paleoclimate Simulation

Study on the Batting and Paleoclimate of Stalagmites from Cave in China