Author:
Askin Rosemary A.,Baldoni Alicia M.
Abstract
Proteaceous plants were an important component of the high-latitude Late
Cretaceous–Paleogene podocarpaceous conifer and
Nothofagus forest vegetation growing in high-rainfall
temperate conditions. In the southern South America–Antarctic Peninsula
region the fossil record of the Proteaceae comprises pollen, leaves, fruits
and wood with affinities to the extant subfamilies Grevilleoideae,
Proteoideae, and possibly Carnarvonioideae and Persoonioideae. The oldest
reported occurrences of Proteaceae in this region are in the middle–late
Santonian of the Antarctic Peninsula and include pollen of
Proteacidites subscabratus Couper, with the addition in
the Campanian of other species of Proteacidites and
Propylipollis, Cranwellipollis
spp. and Peninsulapollis spp. Diversity of proteaceous
pollen increased through the Campanian and Maastrichtian, reflecting the
spread of Proteaceae along the Antarctic Peninsula and into South America.
Both endemic species and species derived from the Australian region are
represented. Compared to coeval Australian assemblages, however, proteaceous
diversity remained relatively low. Interestingly,
Beauprea-type species
(Beaupreaidites spp.,
Peninsulapollis spp.) are common and varied in the
Antarctic Peninsula from Campanian into the Eocene, yet the South American
pollen record does not include these forms, except for rare
Peninsulapollis gillii. Possibly drier conditions may
have discouraged northward migration of this group. South American fossil
proteaceous taxa are primarily related to Grevilleoideae, a trend that
continues into the modern flora on that continent.
Subject
Plant Science,Ecology, Evolution, Behavior and Systematics
Cited by
27 articles.
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