BIOME Model of Vegetation Reconstruction

2007 ◽  
pp. 2551-2561
Author(s):  
M EDWARDS
2007 ◽  
Vol 20 (1) ◽  
pp. 21-32 ◽  
Author(s):  
Vanessa C. Thorn

AbstractPhytoliths in the modern vegetation of sub-Antarctic Campbell Island are compared with those in the soil beneath to assess the accuracy of vegetation reconstructions made from dispersed phytolith assemblages. The soil phytoliths alone suggest the source vegetation is a grassland association for all study sites, which reflects none of the herb, fern or shrub component of the overlying vegetation. It is concluded that at this locality dispersed phytoliths on their own are not reliable indicators of source vegetation and should be used with caution in this context for palaeoecological studies. However, they can provide useful botanical information where all other organic material is absent. With further research, based on the abundance and diversity of Poaceae phytoliths observed in this and other studies, dispersed phytoliths from the fossil record have the potential to contribute significantly to the understanding of grassland ecosystem development in the geological past.


2009 ◽  
Vol 35 (2-3) ◽  
pp. 371-389 ◽  
Author(s):  
Vincent Garreta ◽  
Paul A. Miller ◽  
Joël Guiot ◽  
Christelle Hély ◽  
Simon Brewer ◽  
...  

1989 ◽  
Vol 2 (4) ◽  
pp. 387 ◽  
Author(s):  
PM Wells ◽  
RS Hill

Fifteen new species belonging to five genera (one, Mesibovia, newly described) of the Podocarpaceae with imbricate leaves are described from Oligocene–Early Miocene localities in Tasmania. Nine of these species belong to Dacrycarpus, which is now extinct in Australia, and their living affinities are widespread in latitude and altitude from New Zealand to New Guinea. Three species of Dacrydium s. str. demonstrate that this genus was diverse in Tasmania in the Tertiary, although it is now extinct in Australia. A species of Microstrobos, which is very similar to the extant alpine/subalpine Tasmanian endemic M. niphophilus, occurs in both high- and low-altitude sites, and suggests that this type was once more widespread. The Oligocene Lagarostrobos marginata is intermediate between the two extant species of Lagarostrobos, and suggests a closer relationship between them than do other lines of evidence. Mesibovia rhomboideu, recovered from three localities, shares features with several extant genera, and is of importance in understanding evolution within this group. The significance of the fossils for climatic and vegetation reconstruction is discussed.


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