Here we present a reconstruction of vegetation history and environmental changes at the central zone of Bahía Samborombón during the Late Holocene sea-level regressive phase (last 2.7 Ka) corresponding to MIS 1. This study is an integrative approach based on the combination of geomorphological and micropaleontological (pollen, non-pollen palynomorphs and foraminifera) proxy data. We found agreement among the environmental inferences from each proxy, which clearly show the evolution of the estuarine saltmarsh from an intertidal environment under significant marine influence towards a supratidal brackish-freshwater environment as sea-level was falling. The evidence of this evolution is (1) coastal progradation encompassing at least 5.7 km as ...
This paper presents the main palaeoenvironmental results obtained from a site located in the western...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
The present work describes land cover changes in the inner section of Canal Principal, in the Bahía ...
We present a high resolution multi-proxy study about environmental changes that occurred during the ...
In this study we examine the distribution patterns of modern palynological assemblages from differen...
Sedimentary descriptions and radiocarbon ages from two cores obtained from coastal plains along the ...
Here we present palynological records from alluvial deposits in four outcrop sequences along the low...
In the present contribution, we studied assemblages of benthic foraminifers, ostracods and charophyt...
We report the sedimentology, palynology, geochemistry, and diatom assemblages of a well-dated succes...
A sedimentary record spanning 5792-5511 cal yr BP and 3188-2854 cal yr BP was recovered at 36° 45′ 4...
El análisis palinológico de una sucesión sedimentaria expuesta en la margen derecha del Río Salado (...
In this investigation, we carried out a Mid-Holocene paleoenvironmental reconstruction based on foss...
Analyses of fossil records of molluscs, stable isotopes of carbon and oxygen, diatoms and palynomorp...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
Holocene paleoenvironmental changes have been interpreted on the basis of benthic foraminifera recov...
This paper presents the main palaeoenvironmental results obtained from a site located in the western...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
The present work describes land cover changes in the inner section of Canal Principal, in the Bahía ...
We present a high resolution multi-proxy study about environmental changes that occurred during the ...
In this study we examine the distribution patterns of modern palynological assemblages from differen...
Sedimentary descriptions and radiocarbon ages from two cores obtained from coastal plains along the ...
Here we present palynological records from alluvial deposits in four outcrop sequences along the low...
In the present contribution, we studied assemblages of benthic foraminifers, ostracods and charophyt...
We report the sedimentology, palynology, geochemistry, and diatom assemblages of a well-dated succes...
A sedimentary record spanning 5792-5511 cal yr BP and 3188-2854 cal yr BP was recovered at 36° 45′ 4...
El análisis palinológico de una sucesión sedimentaria expuesta en la margen derecha del Río Salado (...
In this investigation, we carried out a Mid-Holocene paleoenvironmental reconstruction based on foss...
Analyses of fossil records of molluscs, stable isotopes of carbon and oxygen, diatoms and palynomorp...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
Holocene paleoenvironmental changes have been interpreted on the basis of benthic foraminifera recov...
This paper presents the main palaeoenvironmental results obtained from a site located in the western...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
The present work describes land cover changes in the inner section of Canal Principal, in the Bahía ...