Vegetation forms the major living characteristic of a landscape that solicits inquiry into the history of its changes during the late Quaternary and the major factors that have influenced the changes. Early studies considered ecological factors would cause vegetation to develop until a stable climatic climax formation was attained (Clements 1936). The concept of an area developing a potential natural vegetation in the absence of humans was similar (Tüxen 1956). Both ideas held that the vegetation of an area would develop to a stable condition that would change little. However, the vegetation of a region never remains in stasis, but develops dynamically through time, influenced by changing dominant factors (Chiarucci et al. 2010)
Aim To test competing hypotheses about the timing and extent of Holocene landscape opening using pol...
Accumulations of plant macrofossils in lake sediments provide useful tools for identifying past loc...
Macro- and micro-fossil plants are described from Early to Middle Pleistocene sediments at Regatta P...
This thesis contains the results and conclusions of the first research in Tasmania using pollen ana...
Artículo de publicación ISIAim To reconstruct the Late Glacial and Holocene vegetation history of we...
Macrofossils from Pleistocene sediments in western Tasmania are investigated in order to reconstruct...
Tasmania’s dry, inland east is ideally positioned to inform models of late Quaternary environmental ...
The study of fossil pollen grains (palynology) is an extremely useful tool for understanding past Qu...
A record of vegetation and environmental change over the past 3000 years was obtained through pollen...
The results of contemporary research suggest that vegetation varies continuously with environment, e...
Introduction Almost all palaeoecological and paleoenvironmental research ultimately depends on an u...
Plant communities are largely reshaped by climate and the environment over millennia, providing a po...
Pollen analysis of a core taken from a reed marsh in northeastern Tasmania near Bass Strait highligh...
Some 83% of the area of native vegetation of the Tasmanian Midlands has been replaced after 170 yr o...
Pollen analysis of a 2 m core from the floor of Crown Lagoon in the Midlands of Tasmania indicates t...
Aim To test competing hypotheses about the timing and extent of Holocene landscape opening using pol...
Accumulations of plant macrofossils in lake sediments provide useful tools for identifying past loc...
Macro- and micro-fossil plants are described from Early to Middle Pleistocene sediments at Regatta P...
This thesis contains the results and conclusions of the first research in Tasmania using pollen ana...
Artículo de publicación ISIAim To reconstruct the Late Glacial and Holocene vegetation history of we...
Macrofossils from Pleistocene sediments in western Tasmania are investigated in order to reconstruct...
Tasmania’s dry, inland east is ideally positioned to inform models of late Quaternary environmental ...
The study of fossil pollen grains (palynology) is an extremely useful tool for understanding past Qu...
A record of vegetation and environmental change over the past 3000 years was obtained through pollen...
The results of contemporary research suggest that vegetation varies continuously with environment, e...
Introduction Almost all palaeoecological and paleoenvironmental research ultimately depends on an u...
Plant communities are largely reshaped by climate and the environment over millennia, providing a po...
Pollen analysis of a core taken from a reed marsh in northeastern Tasmania near Bass Strait highligh...
Some 83% of the area of native vegetation of the Tasmanian Midlands has been replaced after 170 yr o...
Pollen analysis of a 2 m core from the floor of Crown Lagoon in the Midlands of Tasmania indicates t...
Aim To test competing hypotheses about the timing and extent of Holocene landscape opening using pol...
Accumulations of plant macrofossils in lake sediments provide useful tools for identifying past loc...
Macro- and micro-fossil plants are described from Early to Middle Pleistocene sediments at Regatta P...