A Rapid Cooling Event Over the Western Pacific Region During the Middle Bronze Age

scientific article published in 2021

A comparison of the climates of the Medieval Climate Anomaly, Little Ice Age, and Current Warm Period reconstructed using coral records from the northern South China Sea

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Assessment of coral δ44/40Ca as a paleoclimate proxy in the Great Barrier Reef of Australia

scholarly article

Biological controls on diurnal variations in seawater trace element concentrations and carbonate chemistry on a coral reef

scholarly article by Xuefei Chen published in November 2015

Carbon and oxygen isotopic analyses of calcite in calcite-dolomite mixtures: optimization of selective acid extraction

scientific article published on 01 March 2019

Carbon isotopic disequilibrium between seawater and air in the coastal Northern South China Sea over the past century

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Chemical weathering controls on variations in the molybdenum isotopic composition of river water: Evidence from large rivers in China

scholarly article

Clumped isotopic signatures in land-snail shells revisited: Possible palaeoenvironmental implications

scientific article published in 2019

Daily δ18O and δD of precipitations from 2007 to 2009 in Guangzhou, South China: Implications for changes of moisture sources

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Decadal variability in seawater pH in the West Pacific: Evidence from coral δ11 B records

article by Gangjian Wei et al published November 2015 in Journal of Geophysical Research: Oceans

Decadal variations in trace metal concentrations on a coral reef: Evidence from a 159 year record of Mn, Cu, and V in aPoritescoral from the northern South China Sea

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Decoupling of coral skeletal δ13C and solar irradiance over the past millennium caused by the oceanic Suess effect

Decoupling of seasonal temperature and precipitation over the western Pacific during the early mid-Holocene

ENSO variability around 2000 years ago recorded by Tridacna gigas δ 18 O from the South China Sea

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El Niño–Southern Oscillation variability recorded in estuarine sediments of the Changjiang River, China

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Environmental controls on coral skeletal δ13C in the northern South China Sea

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Evaluation of annual resolution coral geochemical records as climate proxies in the Great Barrier Reef of Australia

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High-precision analysis of Sr/Ca and Mg/Ca ratios in corals by laser ablationinductively coupled plasma optical emission spectrometry

High-resolution sea surface temperature records derived from foraminiferal Mg/Ca ratios during the last 260 ka in the northern South China Sea

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Influence of redox conditions on animal distribution and soft-bodied fossil preservation of the Lower Cambrian Chengjiang Biota

scholarly article by Changshi Qi published in October 2018

Local origins of interdecadal Pacific variability in the tropical and North Pacific Ocean: evidence from a comparative study of coral oxygen isotope records

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Natural and anthropogenic impacts on environmental changes over the past 7500 years based on the multi-proxy study of shelf sediments in the northern South China Sea

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Nd, Sr isotopes and elemental geochemistry of surface sediments from the South China Sea: Implications for Provenance Tracing

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Saltier sea surface water conditions recorded by multiple mid-Holocene corals in the northern South China Sea

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Sea surface temperature records in the northern South China Sea from mid-Holocene coral Sr/Ca ratios

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Seasonal changes in the radiogenic and stable strontium isotopic composition of Xijiang River water: Implications for chemical weathering

scholarly article

Sources and distribution of sedimentary organic matter in the Beibu Gulf, China: Application of multiple proxies

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Super instrumental El Niño events recorded by a Porites coral from the South China Sea

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Surface water δ18O in the marginal China seas and its hydrological implications

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Variations in the Pacific Decadal Oscillation since 1853 in a coral record from the northern South China Sea

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Variations in the timing of the rainy season in the northern South China Sea during the middle to late Holocene

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Wet and cold climate conditions recorded by coral geochemical proxies during the beginning of the first millennium CE in the northern South China Sea

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