The aim of this study was to improve our understanding of the relationship between modem pollen rain, vegetation and climate in Bolivia, and to provide a link to interpret the fossil pollen record. Ten ecoregions were investigated: southern Puna, northern Puna, Yungas, pre-Puna, Gran Chaco, Chaco Chiquitano, Tucuman forest, inter-Andean dry forest, flooded savanna, and southwest Amazon forest. Forty soil surface samples were collected along an elevational transect from 4588 m to 160 m in 10 ecoregions and 16 sub-ecoregions. The vegetation in each sampling plot was described and the statistical analyses were performed on the pollen data set. Each ecoregion was distinguished by its pollen content and indicators. Statistical analysis performed...
Pollen, a regular component of tropical ice cores, has been shown to have great potential as a sensi...
An ongoing controversy in Amazonian palaeoecology is the manner in which Amazonian rainforest commun...
The biomisation method is used to reconstruct Latin American vegetation at 6000±500 and 18 000±1000 ...
The aim of this study was to improve our understanding of the relationship between modem pollen rain...
The majority of vegetation reconstructions from the Neotropics are derived from fossil pollen record...
At present there is uncertainty over the response of neotropical ecosystems to the climatic changes ...
Aim To provide a greater understanding of the modern pollen rain for the central Andes region of Sou...
Steppes and grasslands of semiarid environments in the Central Andes are poorly understood in fossil...
To analyse the relationships between potential natural vegetation, pollen and climate in order to im...
Accurate differentiation between tropical forest and savannah ecosystems in the fossil pollen record...
Controversy surrounds the Quaternary palaeoenvironmental history of Amazonia. It is unclear whether...
We used fossil pollen to investigate the response of the eastern Chiquitano seasonally-dry tropical ...
Quantitative estimates of temperature and precipitation change during the late Pleistocene and Holoc...
Aim To improve knowledge of the distribution of species and modern pollen dispersal in the puna vege...
We present the results of pollen analysis performed on an ice core recovered from Nevado Sajama, Bol...
Pollen, a regular component of tropical ice cores, has been shown to have great potential as a sensi...
An ongoing controversy in Amazonian palaeoecology is the manner in which Amazonian rainforest commun...
The biomisation method is used to reconstruct Latin American vegetation at 6000±500 and 18 000±1000 ...
The aim of this study was to improve our understanding of the relationship between modem pollen rain...
The majority of vegetation reconstructions from the Neotropics are derived from fossil pollen record...
At present there is uncertainty over the response of neotropical ecosystems to the climatic changes ...
Aim To provide a greater understanding of the modern pollen rain for the central Andes region of Sou...
Steppes and grasslands of semiarid environments in the Central Andes are poorly understood in fossil...
To analyse the relationships between potential natural vegetation, pollen and climate in order to im...
Accurate differentiation between tropical forest and savannah ecosystems in the fossil pollen record...
Controversy surrounds the Quaternary palaeoenvironmental history of Amazonia. It is unclear whether...
We used fossil pollen to investigate the response of the eastern Chiquitano seasonally-dry tropical ...
Quantitative estimates of temperature and precipitation change during the late Pleistocene and Holoc...
Aim To improve knowledge of the distribution of species and modern pollen dispersal in the puna vege...
We present the results of pollen analysis performed on an ice core recovered from Nevado Sajama, Bol...
Pollen, a regular component of tropical ice cores, has been shown to have great potential as a sensi...
An ongoing controversy in Amazonian palaeoecology is the manner in which Amazonian rainforest commun...
The biomisation method is used to reconstruct Latin American vegetation at 6000±500 and 18 000±1000 ...