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      Climatically driven formation of the Tangxian planation surface in North China: An example from northwestern Zhongtiao Shan of the Shanxi Graben System

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          Trends, rhythms, and aberrations in global climate 65 Ma to present.

          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-sea sediment cores. This evolution includes gradual trends of warming and cooling driven by tectonic processes on time scales of 10(5) to 10(7) years, rhythmic or periodic cycles driven by orbital processes with 10(4)- to 10(6)-year cyclicity, and rare rapid aberrant shifts and extreme climate transients with durations of 10(3) to 10(5) years. Here, recent progress in defining the evolution of global climate over the Cenozoic Era is reviewed. We focus primarily on the periodic and anomalous components of variability over the early portion of this era, as constrained by the latest generation of deep-sea isotope records. We also consider how this improved perspective has led to the recognition of previously unforeseen mechanisms for altering climate.
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            The least-squares line and plane and the analysis of palaeomagnetic data

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              A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records

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                Author and article information

                Journal
                Lithosphere
                Geological Society of America
                1941-8264
                May 16 2018
                August 01 2018
                May 16 2018
                August 01 2018
                : 10
                : 4
                : 530-544
                Affiliations
                [1 ]Guangdong Provincial Key Laboratory of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou, 510275, China
                [2 ]Key Laboratory of Earth Surface Processes of Ministry of Education, Peking University, Beijing 100871, China
                [3 ]Department of Earth Sciences, ETH Zurich, Sonneggstrasse 5, 8092 Zurich, Switzerland
                [4 ]College of Urban and Environmental Sciences, Peking University, Beijing 100871, China
                Article
                10.1130/L720.1
                9f4dbee5-6468-428e-bdcf-9ca76d8c535b
                © 2018
                History

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