Climatic variability and human impact during the last 2000 years in western Mesoamerica: evidence of late Classic (AD 600–900) and Little Ice Age drought events

Rodríguez-Ramírez, A.; Caballero, M.; Roy, P.; Ortega, B.; Vázquez-Castro, G.; Lozano-García, S.

doi:https://doi.org/10.5194/cp-11-1239-2015

Articles | Volume 11, issue 9

Clim. Past, 11, 1239–1248, 2015

https://doi.org/10.5194/cp-11-1239-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Climate change and human impact in Central and South America...

Clim. Past, 11, 1239–1248, 2015

https://doi.org/10.5194/cp-11-1239-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 11, issue 9

Research article 30 Sep 2015

Research article | 30 Sep 2015

Climatic variability and human impact during the last 2000 years in western Mesoamerica: evidence of late Classic (AD 600–900) and Little Ice Age drought events

A. Rodríguez-Ramírez et al.

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Final revised paper (published on 30 Sep 2015)
Preprint (discussion started on 20 May 2015)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC C719: 'very good', Mark Brenner, 16 Jun 2015
RC C759: 'Review of Rodriguez et al', Sarah Davies, 22 Jun 2015
- AC C1397: 'Reply to Reviewer 2, Sarah Davies:', Margarita Caballero, 17 Aug 2015
AC C1395: 'Reviewer 1, Mark Brenner:', Margarita Caballero, 17 Aug 2015

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish subject to minor revisions (review by Editor) (27 Aug 2015) by Martin Grosjean

AR by Margarita Caballero on behalf of the Authors (04 Sep 2015) Author's response

ED: Publish subject to technical corrections (09 Sep 2015) by Martin Grosjean

Short summary

We present results from western Mexico, where very few palaeoclimatic research sites exist. The record has good chronological resolution (ca. 20 years) and clear climatic trends during the last 2ka. The most important signals are: dry conditions during the late Classic (AD 500 to 1000), especially from AD 600 to 800, and low lake levels during the LIA, in two phases that follow Spörer and Maunder solar minima. Drier conditions are related with a lower intensity of the North American monsoon.