The Jáchal River Valley displays a number of significant Holocene sedimentary accumulations made up of fine-grained materials. These deposits are interpreted as the sedimentary infill of shallow temporary lakes that were generated by slow growing episodes of alluvial fans that obstructed the Jáchal River Valley. The association of fossil remains through the Holocene sedimentary sequence suggests that the accumulation of lacustrine sediments was affected by climate variations. The predominant aridity was punctuated by very few humid episodes characterised by fresh-water gastropoda and the intercalations of muddy sediments. The high proportion of charcoal particles in some samples indicates periodic forest fires. Abundant non-pollen forest re...
Laguna Mar Chiquita (LMC, 30°54′S – 62°51′W) is a highly variable and shallow saline lake, located i...
Hydrological changes that occurred during the last 4700 years have been reconstructed using multi-pr...
The climatic changes that occurred during the late Pleistocene-early Holocene in Patagonia generated...
Late Holocene environmental conditions are reconstructed from a sedimentary core (LCTF2) retrieved f...
This paper reconstructs the vegetation history of the Lake Pueyrredón area during the Holocene and c...
Changes in trophic status of the shallow Lake La Brava (southeastern Pampa plain of Argentina) are e...
This work constitutes an integration of geological, archaeological and palynological data from Santa...
This study presents new paleoenvironmental data obtained from sedimentary cores from Lago Fagnano, a...
Multiproxy investigations, including XRF core-scanning, sedimentology, stable isotopes, pollen and d...
This paper presents a multi-proxy record and its paleoenvironmental interpretation from Pastos Chico...
In this paper, we analyze the paleoclimatic and paleoenvironmental evolution of Laguna Yema in semi-...
This study presents a paleolimnological and paleoclimatological reconstruction based on diatoms and ...
This paper presents the paleogeographic reconstructions of flooded areas of the Tar - San Martín lac...
Using an interdisciplinary perspective that integrates archaeological, geomorphological, and palynol...
Hydrological changes that occurred during the last 4700 years have been reconstructed using multi-pr...
Laguna Mar Chiquita (LMC, 30°54′S – 62°51′W) is a highly variable and shallow saline lake, located i...
Hydrological changes that occurred during the last 4700 years have been reconstructed using multi-pr...
The climatic changes that occurred during the late Pleistocene-early Holocene in Patagonia generated...
Late Holocene environmental conditions are reconstructed from a sedimentary core (LCTF2) retrieved f...
This paper reconstructs the vegetation history of the Lake Pueyrredón area during the Holocene and c...
Changes in trophic status of the shallow Lake La Brava (southeastern Pampa plain of Argentina) are e...
This work constitutes an integration of geological, archaeological and palynological data from Santa...
This study presents new paleoenvironmental data obtained from sedimentary cores from Lago Fagnano, a...
Multiproxy investigations, including XRF core-scanning, sedimentology, stable isotopes, pollen and d...
This paper presents a multi-proxy record and its paleoenvironmental interpretation from Pastos Chico...
In this paper, we analyze the paleoclimatic and paleoenvironmental evolution of Laguna Yema in semi-...
This study presents a paleolimnological and paleoclimatological reconstruction based on diatoms and ...
This paper presents the paleogeographic reconstructions of flooded areas of the Tar - San Martín lac...
Using an interdisciplinary perspective that integrates archaeological, geomorphological, and palynol...
Hydrological changes that occurred during the last 4700 years have been reconstructed using multi-pr...
Laguna Mar Chiquita (LMC, 30°54′S – 62°51′W) is a highly variable and shallow saline lake, located i...
Hydrological changes that occurred during the last 4700 years have been reconstructed using multi-pr...
The climatic changes that occurred during the late Pleistocene-early Holocene in Patagonia generated...