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Analyses of fossil records of molluscs, stable isotopes of carbon and oxygen, diatoms and palynomorphs from alluvial deposits at Arroyo Claromecó, in the southern Pampa region of Argentina, provide an integrated reconstruction of rapid Holocene environmental change related to marine and palaeoclimate influences. The major events recorded include: (i) disturbances produced by marine influences in close...
The Trans‐Mexican Volcanic Belt (TMVB) provides an excellent setting for reconstruction of late Quaternary climate from different natural archives. Moreover, human impact on the landscape since the mid‐Holocene provides a good opportunity to investigate the complex interplay of natural and anthropogenic forcing of landscape change. However, despite the wealth of records, understanding of the environmental...
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