November 11, 2009
Fossil Plant Discovery Links Patagonia To New Guinea In A Warmer Past
How revising an ancient species can change what we know of a lineage's historical distribution and the climate in which it lived
Fossil plants are windows to the past, providing us with clues as to what our planet looked like millions of years ago. Not only do fossils tell us which species were present before human-recorded history, but they can provide information about the climate and how and when lineages may have dispersed around the world. Identifying fossil plants can be tricky, however, when plant organs fail to be preserved or when only a few sparse parts can be found.
However, numerous characteristics of the leaves, including their distinctive shape and stomatal arrangements, as well as seed cone details of the newly discovered specimens entirely match those of extant Papuacedrus, a closely related genus, currently found only in tropical, montane New Guinea and the Moluccas.
Based on the newly discovered fossil specimens from 52 and 47 million years ago, Wilf and colleagues reassigned the fossil species to Papuacedrus, under the new name combination Papuacedrus prechilensis. One of the major implications of this reassignment is that, because Papuacedrus is known from tropical montane habitats and is physiologically limited to extremely wet climates, it adds to the emerging evidence that Patagonia in the Eocene was a warm, wet tropical place and not a cold, dry steppe as much of it is today. It also adds a tropical West Pacific connection for Papuacedrus, further establishing the interchange of flora with Australia and neighboring areas via a warm and forested Antarctic land connection during the Eocene. Indeed, less complete Papuacedrus fossils have previously been found in Australia and Antarctica.
"This is a wonderful example of how securely identifying well-preserved and well-dated fossils can have many impacts," Wilf noted. "These fossils contribute critical information about conifer evolution as well as the biogeographic history of the Southern Hemisphere. Combined with the robust site geology we have generated, they also contribute to an important environmental reinterpretation of a large area in the past. Papuacedrus physiologically requires lots of moisture and cannot withstand prolonged droughts."
Another important consequence of this find is how it relates to the great diversity of other fossil plant as well as insect species known from the Patagonian fossil sites. The lush, possibly montane, rainforest environment indicated by Papuacedrus helps to explain this stunning richness from the Eocene. "The revision [of this species] not only forces a major shift in biogeographic affinity (Patagonia to New Guinea), but also provides a decisive boost to important hypotheses of rainforest climates during the Eocene in Patagonia that had not been fully substantiated in previous work," Wilf said. "This in turn helps to explain the remarkable plant and insect diversity found in Eocene Patagonia."
Image Caption: This is foliage of Papuacedrus prechilensis (Berry) Wilf et al., comb. nov. (Cupressaceae), from the middle Eocene RÃo PichileufÃº flora of RÃo Negro Province, Patagonia, Argentina. The monotypic genus Papuacedrus is today restricted to montane rainforests of New Guinea and the Moluccas, but its scarce fossil record includes Tasmania and Antarctica. Wilf et al. describe a suite of well-preserved specimens excavated from early and middle Eocene sites in Patagonia, including an immature seed cone attached to foliage with organic preservation, bearing numerous characters diagnostic of Papuacedrus. The fossils represent the first fossil cone, the oldest record, and the only South American record of Papuacedrus, greatly expanding its history of widespread distribution across Gondwana before cooling and drying conditions forced its extinction in southern South America and retreat to its current range in the equatorial West Pacific. Before the revision here to Papuacedrus, the only previously known fossil of this species was described as a close relative of Austrocedrus chilensis, a dry- and cold-tolerant conifer that grows near the fossil sites. Thus, the revision removes a link to southern South American biomes and puts in its place a link to Australasian montane rainforests. Along with other emerging and consistent data from these floras, this result suggests that a rainforest biome was present in Eocene Patagonia, possibly including topographic relief. High Eocene rainfall, topography, and land connections both to the rest of South America and to Australasia via Antaractica are viable explanations for the extraordinary plant and insect-feeding richness found at the fossil sites. The specimen shown is coalified with light patches of facial leaf cuticle visible overlying coal. Note opposite branching, enlarged lateral leaves, and light-colored amber in foliar resin canals. Credit: Image credit: P. Wilf.
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