The middle Pleistocene transition: characteristics, mechanisms, and implications for long-term changes in atmospheric pCO2

PU Clark, D Archer, D Pollard, JD Blum, JA Rial… - Quaternary Science …, 2006 - Elsevier
The emergence of low-frequency, high-amplitude, quasi-periodic (∼ 100-kyr) glacial
variability during the middle Pleistocene in the absence of any significant change in orbital …

Radiogenic isotopes: Tracers of past ocean circulation and erosional input

M Frank - Reviews of geophysics, 2002 - Wiley Online Library
The radiogenic isotope composition of dissolved trace metals in the ocean represents a set
of relatively new and not yet fully exploited tracers with a large potential for oceanographic …

A Late Pleistocene sea level stack

RM Spratt, LE Lisiecki - Climate of the Past, 2016 - cp.copernicus.org
Late Pleistocene sea level has been reconstructed from ocean sediment core data using a
wide variety of proxies and models. However, the accuracy of individual reconstructions is …

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

LE Lisiecki, ME Raymo - Paleoceanography, 2005 - Wiley Online Library
We present a 5.3‐Myr stack (the “LR04” stack) of benthic δ18O records from 57 globally
distributed sites aligned by an automated graphic correlation algorithm. This is the first …

[图书][B] Global physical climatology

DL Hartmann - 2015 - books.google.com
Global Physical Climatology, Second Edition, provides an introduction to the science of
climate and climate change that spans the atmosphere, ocean, and land surface, and the …

African climate change and faunal evolution during the Pliocene–Pleistocene

BM Peter - Earth and Planetary Science Letters, 2004 - Elsevier
Environmental theories of African faunal evolution state that important evolutionary changes
during the Pliocene–Pleistocene interval (the last ca. 5.3 million years) were mediated by …

Plio-pleistocene African climate

PB Demenocal - Science, 1995 - science.org
Marine records of African climate variability document a shift toward more arid conditions
after 2.8 million years ago (Ma), evidently resulting from remote forcing by cold North Atlantic …

[PDF][PDF] 黄土高原红粘土成因及上新世北方干旱化问题

丁仲礼, 孙继敏, 朱日祥, 郭斌 - 第四纪研究, 1997 - dsjyj.com.cn
黄土高原红粘土成因及上新世北方干旱化问题3 Page 1 1997 年5 月 第四纪研究 QUA T ERNA
RY SC IEN CES 第2 期 第一作者简介: 丁仲礼男40 岁研究员第四纪地质学专业 3 国家自然科学 …

Climate signal detection using wavelet transform: How to make a time series sing

KM Lau, H Weng - Bulletin of the American meteorological …, 1995 - journals.ametsoc.org
In this paper, the application of the wavelet transform (WT) to climate time series analyses is
introduced. A tutorial description of the basic concept of WT, compared with similar concepts …

On the structure and origin of major glaciation cycles 2. The 100,000‐year cycle

J Imbrie, A Berger, EA Boyle, SC Clemens… - …, 1993 - Wiley Online Library
Climate over the past million years has been dominated by glaciation cycles with periods
near 23,000, 41,000, and 100,000 years. In a linear version of the Milankovitch theory, the …