Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics (2021)
- Authors:
- Cheng, Hai
- Xu, Yao
- Dong, Xiyu
- Zhao, Jingyao
- Li, Hanying
- Baker, Jonathan
- Sinha, Ashish
- Spötl, Christoph
- Zhang, Haiwei
- Du, Wenjing
- Zong, Baoyun
- Jia, Xue
- Kathayat, Gayatri
- Liu, Dianbing
- Cai, Yanjun
- Wang, Xianfeng
- Stríkis, Nicolás Misailidis
- Cruz, Francisco W
- Auler, Augusto S.
- Gupta, Anil K.
- Singh, Raj Kumar
- Jaglan, Sonu
- Dutt, Som
- Liu, Zhengyu
- Edwards, R. Lawrence
- Cheng, Hai
- Autor USP: CRUZ JÚNIOR, FRANCISCO WILLIAM DA - IGC
- Unidade: IGC
- DOI: 10.1038/s43247-021-00304-6
- Subjects: PALEOCLIMATOLOGIA; ESPELEOTEMAS; ÚLTIMO MÁXIMO GLACIAL
- Agências de fomento:
- Language: Inglês
- Imprenta:
- Publisher: Springer Science and Business Media LLC
- Date published: 2021
- Source:
- Título: Communications Earth & Environment
- ISSN: 2662-4435
- Volume/Número/Paginação/Ano: v. 2, n. 230, p. 1-11, 2021
- Este periódico é de acesso aberto
- Este artigo é de acesso aberto
- URL de acesso aberto
- Cor do Acesso Aberto: gold
- Licença: cc-by
-
ABNT
CHENG, Hai et al. Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics. Communications Earth & Environment, v. 2, n. 230, p. 1-11, 2021Tradução . . Disponível em: https://doi.org/10.1038/s43247-021-00304-6. Acesso em: 29 dez. 2025. -
APA
Cheng, H., Xu, Y., Dong, X., Zhao, J., Li, H., Baker, J., et al. (2021). Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics. Communications Earth & Environment, 2( 230), 1-11. doi:10.1038/s43247-021-00304-6 -
NLM
Cheng H, Xu Y, Dong X, Zhao J, Li H, Baker J, Sinha A, Spötl C, Zhang H, Du W, Zong B, Jia X, Kathayat G, Liu D, Cai Y, Wang X, Stríkis NM, Cruz FW, Auler AS, Gupta AK, Singh RK, Jaglan S, Dutt S, Liu Z, Edwards RL. Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics [Internet]. Communications Earth & Environment. 2021 ; 2( 230): 1-11.[citado 2025 dez. 29 ] Available from: https://doi.org/10.1038/s43247-021-00304-6 -
Vancouver
Cheng H, Xu Y, Dong X, Zhao J, Li H, Baker J, Sinha A, Spötl C, Zhang H, Du W, Zong B, Jia X, Kathayat G, Liu D, Cai Y, Wang X, Stríkis NM, Cruz FW, Auler AS, Gupta AK, Singh RK, Jaglan S, Dutt S, Liu Z, Edwards RL. Onset and termination of Heinrich Stadial 4 and the underlying climate dynamics [Internet]. Communications Earth & Environment. 2021 ; 2( 230): 1-11.[citado 2025 dez. 29 ] Available from: https://doi.org/10.1038/s43247-021-00304-6 - Hydro-climate variability during the last two millennia in Morocco, ingerred from high resolution speleothem records
- Holocene precipitation changes in the deep tropics recorded by Speleothems(Invited)
- South American Monsoon variability during the last 1000 years inferred from Northeastern Peruvian speleothems
- Variabilidad del Monzón sudamericano durante los últimos 1000 años inferidos a partir de estudios isotópicos en espeleotemas recolectados en los andes orientales del Perú y Bolivia
- The spatiotemporal extent of the Green Sahara during the last glacial period
- Evaluating model outputs using integrated global speleothem records of climate change since the last glacial
- Millennial-scale climate variability recorded in Brazilian speleothems
- Hydroclimate changes across the Amazon lowland over the past 45,000 years
- Elucidating the climate and topographic controls on stable isotope composition of meteoric waters in Morocco, using station-based and spatially-interpolated data
- Speleothem records decadal to multidecadal hydroclimate variations in southwestern Morocco during the last millennium
Informações sobre o DOI: 10.1038/s43247-021-00304-6 (Fonte: oaDOI API)
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