Chinese stalagmite paleoclimate researches: A review and perspective

H Cheng, H Zhang, J Zhao, H Li, Y Ning… - Science China Earth …, 2019 - Springer
Stalagmite is one kind of secondary carbonates formed in limestone caves (speleothem).
After cave water droplets containing Ca 2+ and HCO _3^-HCO 3− drip onto floor, carbonate …

Formal subdivision of the Quaternary System/Period: Present status and future directions

MJ Head - Quaternary International, 2019 - Elsevier
Abstract The Quaternary System/Period and Pleistocene Series/Epoch were defined in 2009
by the Global boundary Stratotype Section and Point (GSSP) for the Gelasian Stage/Age …

The 4.2 ka event is not remarkable in the context of Holocene climate variability

NP McKay, DS Kaufman, SH Arcusa, HR Kolus… - Nature …, 2024 - nature.com
Abstract The “4.2 ka event” is a commonly described abrupt climate excursion that occurred
about 4200 years ago. However, the extent to which this event is coherent across regional …

Timing and structure of the Younger Dryas event and its underlying climate dynamics

H Cheng, H Zhang, C Spötl, J Baker… - Proceedings of the …, 2020 - National Acad Sciences
The Younger Dryas (YD), arguably the most widely studied millennial-scale extreme climate
event, was characterized by diverse hydroclimate shifts globally and severe cooling at high …

[PDF][PDF] **石笋古气候研究的回顾与展望

程海, 张海伟, 赵景耀, **瀚瑛, 宁有丰… - **科学: 地球 …, 2019 - academia.edu
摘要石笋是洞穴次生碳酸盐的一种, 是由含Ca 2+ 和HCO3 的洞穴滴水滴到洞穴地面后,
水中碳酸钙在一定条件下过饱和析出, 经年复一年沉积形成. 石笋是古气候研究的重要地质材料 …

Holocene monsoon change and abrupt events on the western Chinese Loess Plateau as revealed by accurately dated stalagmites

L Tan, Y Li, X Wang, Y Cai, F Lin… - Geophysical …, 2020 - Wiley Online Library
Here we present, to date, the highest‐resolved (~ 5 years) and most precisely dated
Holocene monsoon climate reconstruction for the western Chinese Loess Plateau based on …

[HTML][HTML] 湖北玉龙洞石笋多指标记录的4.2 ka 事件

白雨洁, 吴江滢, 梁怡佳, 邵庆丰 - 第四纪研究, 2020 - html.rhhz.net
利用湖北神农架利川市玉龙洞一支长约400 mm 的石笋(TCL), 结合稳定同位素,
微量元素以及灰度等多指标重建了14.4 ka BP~ 2012 AD 时段十年际分辨率的东亚地区气候与 …

SISALv2: a comprehensive speleothem isotope database with multiple age–depth models

L Comas-Bru, K Rehfeld, C Roesch… - Earth System …, 2020 - essd.copernicus.org
Characterizing the temporal uncertainty in palaeoclimate records is crucial for analysing
past climate change, correlating climate events between records, assessing climate …

Recurring summer and winter droughts from 4.2-3.97 thousand years ago in north India

A Giesche, DA Hodell, CA Petrie, GH Haug… - … Earth & Environment, 2023 - nature.com
Abstract The 4.2-kiloyear event has been described as a global megadrought that
transformed multiple Bronze Age complex societies, including the Indus Civilization, located …

Atmospheric blocking induced by the strengthened Siberian High led to drying in west Asia during the 4.2 ka BP event–a hypothesis

A Perşoiu, M Ionita, H Weiss - Climate of the Past, 2019 - cp.copernicus.org
Causal explanations for the 4.2 ka BP event are based on the amalgamation of seasonal
and annual records of climate variability that was manifest across global regions dominated …