Articles | Volume 10, issue 5
https://doi.org/10.5194/cp-10-1803-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/cp-10-1803-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
01 Oct 2014
Research article |
| 01 Oct 2014
Variation in the Asian monsoon intensity and dry–wet conditions since the Little Ice Age in central China revealed by an aragonite stalagmite
J.-J. Yin
Key Laboratory of Karst Dynamics, MLR and Guangxi, Guilin, Guangxi 541004, China
School of Geographical Sciences, Southwest University, Chongqing 400715, China
Institute of Karst Geology, CAGS, Guilin, Guangxi 541004, China
D.-X. Yuan
Key Laboratory of Karst Dynamics, MLR and Guangxi, Guilin, Guangxi 541004, China
School of Geographical Sciences, Southwest University, Chongqing 400715, China
Institute of Karst Geology, CAGS, Guilin, Guangxi 541004, China
Key Laboratory of Karst Dynamics, MLR and Guangxi, Guilin, Guangxi 541004, China
Institute of Karst Geology, CAGS, Guilin, Guangxi 541004, China
Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan
H. Cheng
Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an 710049, China
Department of Earth Sciences, University of Minnesota, Minneapolis 55455, USA
School of Geographical Sciences, Southwest University, Chongqing 400715, China
R. L. Edwards
Department of Earth Sciences, University of Minnesota, Minneapolis 55455, USA
Y.-S. Lin
Key Laboratory of Karst Dynamics, MLR and Guangxi, Guilin, Guangxi 541004, China
Institute of Karst Geology, CAGS, Guilin, Guangxi 541004, China
J.-M. Qin
Key Laboratory of Karst Dynamics, MLR and Guangxi, Guilin, Guangxi 541004, China
Institute of Karst Geology, CAGS, Guilin, Guangxi 541004, China
W. Tang
Institute of Karst Geology, CAGS, Guilin, Guangxi 541004, China
Z.-Y. Zhao
School of Geographical Sciences, Southwest University, Chongqing 400715, China
Department of Environmental and Resource Sciences, LiuPanShui Normal University, Liupanshui 553004, China
H.-S. Mii
Department of Earth Sciences, National Taiwan Normal University, Taipei 11677, Taiwan
Viewed
Total article views: 6,237 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 03 Apr 2014)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 2,908 | 3,018 | 311 | 6,237 | 195 | 189 |
- HTML: 2,908
- PDF: 3,018
- XML: 311
- Total: 6,237
- BibTeX: 195
- EndNote: 189
Total article views: 4,876 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 01 Oct 2014)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 2,416 | 2,259 | 201 | 4,876 | 179 | 180 |
- HTML: 2,416
- PDF: 2,259
- XML: 201
- Total: 4,876
- BibTeX: 179
- EndNote: 180
Total article views: 1,361 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 03 Apr 2014)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 492 | 759 | 110 | 1,361 | 16 | 9 |
- HTML: 492
- PDF: 759
- XML: 110
- Total: 1,361
- BibTeX: 16
- EndNote: 9
Cited
26 citations as recorded by crossref.
- A novel application of triple oxygen isotope ratios of speleothems L. Sha et al. 10.1016/j.gca.2019.12.003
- Interannual Variations of D14CTOC and Elemental Contents in the Laminated Sediments of the Santa Barbara Basin During the Past 200 Years H. Li et al. 10.3389/fmars.2022.823793
- Variations in triple oxygen isotope of speleothems from the Asian monsoon region reveal moisture sources over the past 300 years L. Sha et al. 10.1038/s43247-023-01043-6
- East Asian Monsoon Variability Since the Sixteenth Century N. Goodkin et al. 10.1029/2019GL081939
- High-resolution δ18O and δ13C records of an AMS 14C and 230Th/U dated stalagmite from Xinya Cave in Chongqing: Climate and vegetation change during the late Holocene J. Li et al. 10.1016/j.quaint.2017.06.075
- δ18O, δ13C, elemental content and depositional features of a stalagmite from Yelang Cave reflecting climate and vegetation changes since late Pleistocene in central Guizhou, China M. Zhao et al. 10.1016/j.quaint.2016.07.022
- Spatial pattern and cause of centennial-scale hydroclimatic variability over eastern China during the last millennium J. Yin et al. 10.1016/j.palaeo.2023.111753
- The severe drought event of 2009–2010 over southwest China as recorded by a cave stalagmite from southeast Yunnan: Implication for stalagmite δ18O interpretation in the Asian monsoon region J. Yin et al. 10.1016/j.quascirev.2023.107967
- Past decadal climate variability of East Asian summer monsoon: Characteristics and mechanisms K. Wang et al. 10.1360/TB-2024-0161
- Changes in climate and vegetation of central Guizhou in southwest China since the last glacial reflected by stalagmite records from Yelang Cave M. Zhao et al. 10.1016/j.jseaes.2015.07.021
- A new stalagmite oxygen isotope record over the last 1350 years: Insights into spatial variation in Asian summer monsoon and temperature forcing F. Duan et al. 10.1016/j.quascirev.2022.107499
- Stalagmite-based long-term and multi-centennial hydroclimatic variations in southwestern China during the Holocene and relations to global climate change F. Duan et al. 10.1016/j.quascirev.2023.108327
- Role of the Summer Monsoon Variability in the Collapse of the Ming Dynasty: Evidences From Speleothem Records J. Zhao et al. 10.1029/2021GL093071
- Variations of the global annual mean surface temperature during the past 2000 years: results from the CESM1 Z. Wang et al. 10.1007/s00704-019-02775-2
- The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ18O Records H. Zhang et al. 10.3390/quat2030026
- Precipitation variability over Northwest Himalaya from ∼4.0 to 1.9 ka BP with likely impact on civilization in the foreland areas B. Kotlia et al. 10.1016/j.jseaes.2017.11.025
- New insights on Chinese cave δ18O records and their paleoclimatic significance X. Liu et al. 10.1016/j.earscirev.2020.103216
- Modern aragonite formation at near-freezing conditions in an alpine cave, Carnic Alps, Austria C. Spötl et al. 10.1016/j.chemgeo.2016.04.017
- High-resolution δ 18 O and δ 13 C records during the past 65 ka from Fengyu Cave in Guilin: Variation of monsoonal climates in south China H. Li et al. 10.1016/j.quaint.2016.08.048
- The first high-resolution stalagmite record from Taiwan: Climate and environmental changes during the past 1300 years H. Li et al. 10.1016/j.jseaes.2015.07.025
- Sedimentary rhythm of Mn-carbonate laminae induced by East Asian summer monsoon variability and human activity in Lake Ohnuma, southwest Hokkaido, northern Japan N. Katsuta et al. 10.1016/j.quascirev.2020.106576
- Precipitation in eastern China over the past millennium varied with large-scale climate patterns M. Wang et al. 10.1038/s43247-022-00664-7
- Are aragonite stalagmites reliable paleoclimate proxies? Tests for oxygen isotope time-series replication and equilibrium M. Lachniet 10.1130/B31161.1
- A framework for triple oxygen isotopes in speleothem paleoclimatology T. Huth et al. 10.1016/j.gca.2021.11.002
- Variations of monsoonal rain and vegetation during the past millennium in Tiangui Mountain, North China reflected by stalagmite δ18O and δ13C records from Zhenzhu Cave J. Yin et al. 10.1016/j.quaint.2017.06.039
- A Meta‐Analysis of Studies Attributing Significance to Solar Irradiance R. Vachula & A. Cheung 10.1029/2022EA002466
26 citations as recorded by crossref.
- A novel application of triple oxygen isotope ratios of speleothems L. Sha et al. 10.1016/j.gca.2019.12.003
- Interannual Variations of D14CTOC and Elemental Contents in the Laminated Sediments of the Santa Barbara Basin During the Past 200 Years H. Li et al. 10.3389/fmars.2022.823793
- Variations in triple oxygen isotope of speleothems from the Asian monsoon region reveal moisture sources over the past 300 years L. Sha et al. 10.1038/s43247-023-01043-6
- East Asian Monsoon Variability Since the Sixteenth Century N. Goodkin et al. 10.1029/2019GL081939
- High-resolution δ18O and δ13C records of an AMS 14C and 230Th/U dated stalagmite from Xinya Cave in Chongqing: Climate and vegetation change during the late Holocene J. Li et al. 10.1016/j.quaint.2017.06.075
- δ18O, δ13C, elemental content and depositional features of a stalagmite from Yelang Cave reflecting climate and vegetation changes since late Pleistocene in central Guizhou, China M. Zhao et al. 10.1016/j.quaint.2016.07.022
- Spatial pattern and cause of centennial-scale hydroclimatic variability over eastern China during the last millennium J. Yin et al. 10.1016/j.palaeo.2023.111753
- The severe drought event of 2009–2010 over southwest China as recorded by a cave stalagmite from southeast Yunnan: Implication for stalagmite δ18O interpretation in the Asian monsoon region J. Yin et al. 10.1016/j.quascirev.2023.107967
- Past decadal climate variability of East Asian summer monsoon: Characteristics and mechanisms K. Wang et al. 10.1360/TB-2024-0161
- Changes in climate and vegetation of central Guizhou in southwest China since the last glacial reflected by stalagmite records from Yelang Cave M. Zhao et al. 10.1016/j.jseaes.2015.07.021
- A new stalagmite oxygen isotope record over the last 1350 years: Insights into spatial variation in Asian summer monsoon and temperature forcing F. Duan et al. 10.1016/j.quascirev.2022.107499
- Stalagmite-based long-term and multi-centennial hydroclimatic variations in southwestern China during the Holocene and relations to global climate change F. Duan et al. 10.1016/j.quascirev.2023.108327
- Role of the Summer Monsoon Variability in the Collapse of the Ming Dynasty: Evidences From Speleothem Records J. Zhao et al. 10.1029/2021GL093071
- Variations of the global annual mean surface temperature during the past 2000 years: results from the CESM1 Z. Wang et al. 10.1007/s00704-019-02775-2
- The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ18O Records H. Zhang et al. 10.3390/quat2030026
- Precipitation variability over Northwest Himalaya from ∼4.0 to 1.9 ka BP with likely impact on civilization in the foreland areas B. Kotlia et al. 10.1016/j.jseaes.2017.11.025
- New insights on Chinese cave δ18O records and their paleoclimatic significance X. Liu et al. 10.1016/j.earscirev.2020.103216
- Modern aragonite formation at near-freezing conditions in an alpine cave, Carnic Alps, Austria C. Spötl et al. 10.1016/j.chemgeo.2016.04.017
- High-resolution δ 18 O and δ 13 C records during the past 65 ka from Fengyu Cave in Guilin: Variation of monsoonal climates in south China H. Li et al. 10.1016/j.quaint.2016.08.048
- The first high-resolution stalagmite record from Taiwan: Climate and environmental changes during the past 1300 years H. Li et al. 10.1016/j.jseaes.2015.07.025
- Sedimentary rhythm of Mn-carbonate laminae induced by East Asian summer monsoon variability and human activity in Lake Ohnuma, southwest Hokkaido, northern Japan N. Katsuta et al. 10.1016/j.quascirev.2020.106576
- Precipitation in eastern China over the past millennium varied with large-scale climate patterns M. Wang et al. 10.1038/s43247-022-00664-7
- Are aragonite stalagmites reliable paleoclimate proxies? Tests for oxygen isotope time-series replication and equilibrium M. Lachniet 10.1130/B31161.1
- A framework for triple oxygen isotopes in speleothem paleoclimatology T. Huth et al. 10.1016/j.gca.2021.11.002
- Variations of monsoonal rain and vegetation during the past millennium in Tiangui Mountain, North China reflected by stalagmite δ18O and δ13C records from Zhenzhu Cave J. Yin et al. 10.1016/j.quaint.2017.06.039
- A Meta‐Analysis of Studies Attributing Significance to Solar Irradiance R. Vachula & A. Cheung 10.1029/2022EA002466
Saved (final revised paper)
Saved (final revised paper)
Saved (preprint)
Discussed (preprint)
Latest update: 02 Nov 2024
Special issue