Quantitative reconstruction of mid- to late-Holocene climate in NE China from peat cellulose stable oxygen and carbon isotope records and mechanistic models

Quantitative reconstructions in palaeolimnology: new paradigm or sick science?

(2013) Steve Juggins   QUATERNARY SCIENCE REVIEWS

Representation of flora and vegetation in Quaternary fossil assemblages: known and unknown knowns and unknowns

(2012) Stephen T. Jackson   QUATERNARY SCIENCE REVIEWS

Integrating models with data in ecology and palaeoecology: advances towards a model-data fusion approach

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Quantitative palaeoclimate reconstruction as an inverse problem: A Bayesian inference of late-Holocene climate on the eastern Tibetan Plateau from a peat cellulose δ18O record

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Comments on “Anti-phase oscillation of Asian monsoons during the Younger Dryas period: Evidence from peat cellulose δ13C of Hani, Northeast China” by B. Hong, Y.T. Hong, Q.H. Lin, Yasuyuki Shibata, Masao Uchida, Y.X. Zhu, X.T. Leng, Y. Wang and C.C. Cai [Palaeogeography, Palaeoclimatology, Palaeoecology 297 (2010) 214–222]

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Anti-phase oscillation of Asian monsoons during the Younger Dryas period: Evidence from peat cellulose δ13C of Hani, Northeast China

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A method for climate and vegetation reconstruction through the inversion of a dynamic vegetation model

(2009) Vincent Garreta et al.   CLIMATE DYNAMICS

Three-dimensional simulation and inversion of borehole temperatures for reconstructing past climate in complex settings

(2009) Peter O. Hopcroft et al.   JOURNAL OF GEOPHYSICAL RESEARCH

Stable isotope constraints on Holocene carbon cycle changes from an Antarctic ice core

(2009) Joachim Elsig et al.   NATURE

Temperature evolution from the δ 18O record of Hani peat, Northeast China, in the last 14000 years

(2009) Bing Hong et al.   Science in China. Series D, Earth sciences / Chinese Academy of Sciences