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OFR 151.pdf - CRC LEME

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phenology. The method also provides an ecological basis for comparing plants from different<br />

regions and times without having to assume phylogenetic relationships (cf. NLR<br />

methodology). However, like many modern plants, fossil taxa are likely to have occurred in<br />

more than one biome. In almost all instances the abundance of the parent plants will have<br />

differed from one biome to another but this may or may not be reflected by pollen abundance<br />

expressed in relative terms. Also, at least one major biome (Austral Conifer Forest) is extinct<br />

and, during the Cretaceous and Early Tertiary, ferns may have dominated niches that are now<br />

dominated by herbs such as grasses.<br />

Palaeoecological research is often criticised for a "suck-it-and-see" descriptive approach that<br />

is at variance with the hypothetico-deductive methodology, which underpins the physical<br />

sciences. The generation of quantitative data and the application of innovative statistical<br />

techniques developed for the Quaternary seems to provide an opportunity to objectively mine<br />

the extant palaeobotanical database in ways that may assist end-users such as <strong>CRC</strong>-<strong>LEME</strong>.<br />

121

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