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. 2009 Nov 3;106(44):18627-32.
doi: 10.1073/pnas.0905130106. Epub 2009 Oct 15.

Late Paleocene fossils from the Cerrejon Formation, Colombia, are the earliest record of Neotropical rainforest

Affiliations

Late Paleocene fossils from the Cerrejon Formation, Colombia, are the earliest record of Neotropical rainforest

Scott L Wing et al. Proc Natl Acad Sci U S A. .

Abstract

Neotropical rainforests have a very poor fossil record, making hypotheses concerning their origins difficult to evaluate. Nevertheless, some of their most important characteristics can be preserved in the fossil record: high plant diversity, dominance by a distinctive combination of angiosperm families, a preponderance of plant species with large, smooth-margined leaves, and evidence for a high diversity of herbivorous insects. Here, we report on an approximately 58-my-old flora from the Cerrejón Formation of Colombia (paleolatitude approximately 5 degrees N) that is the earliest megafossil record of Neotropical rainforest. The flora has abundant, diverse palms and legumes and similar family composition to extant Neotropical rainforest. Three-quarters of the leaf types are large and entire-margined, indicating rainfall >2,500 mm/year and mean annual temperature >25 degrees C. Despite modern family composition and tropical paleoclimate, the diversity of fossil pollen and leaf samples is 60-80% that of comparable samples from extant and Quaternary Neotropical rainforest from similar climates. Insect feeding damage on Cerrejón fossil leaves, representing primary consumers, is abundant, but also of low diversity, and overwhelmingly made by generalist feeders rather than specialized herbivores. Cerrejón megafossils provide strong evidence that the same Neotropical rainforest families have characterized the biome since the Paleocene, maintaining their importance through climatic phases warmer and cooler than present. The low diversity of both plants and herbivorous insects in this Paleocene Neotropical rainforest may reflect an early stage in the diversification of the lineages that inhabit this biome, and/or a long recovery period from the terminal Cretaceous extinction.

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Conflict of interest statement

The authors declare no conflict of interest.

Figures

Fig. 1.
Fig. 1.
Location of Cerrejón fossil flora and comparative modern samples. (Upper) Cerrejón fossil flora location (★). (Lower) Comparative modern samples are indicated by: □, Quaternary pollen cores; ■, modern leaf litter samples; ●, modern forest transects. See SI Appendix (Tables S1–S4) for details on comparative samples. Base map of Cerrejón region courtesy of National Aeronautics and Space Administration Jet Propulsion Laboratory, California Institute of Technology.
Fig. 2.
Fig. 2.
Cerrejón megafossils identifiable to various higher taxa. (Scale bar: 5 cm, except where noted in parentheses after taxon.) (A) Coniferales (CJ60, 3 cm); (B) Stenochlaena (CJ81); (C and D) undetermined flowers (CJ77, CJ78); (E) fruit of Fabaceae (CJ100); (F) winged seed of Fabaceae (CJ79); (G) Arecaceae, possibly Nypa (CJ68, hammer ≈30 cm); (H) Zingiberales (CJ65, 10 cm); (I–K) leaves and leaflets of Fabaceae (CJ76, CJ1, and CJ19); (L) Malvales with hole feeding (CJ11); (M) Lauraceae (CJ22); (N) closeup of M showing laminar resin glands (1 mm); (O) Malvaceae (CJ26); (P) Euphorbiaceae (CJ24); (Q) Sapotaceae with margin and hole feeding (CJ8). See SI Appendix (Table S10 and Figs. S2–S98) for descriptions and photographs of all morphotypes.
Fig. 3.
Fig. 3.
Similarity of the Cerrejón megaflora to living Neotropical forests. Histograms are the frequency distributions of Spearman rank order correlation coefficients derived from all pairwise comparisons of 72 living forest sites [SI Appendix (see Table S5)]. Arrows show the mean similarity of the Cerrejón flora to all living sites (red, conservative identifications of fossils; green, best-guess identifications). Black lines represent 95% confidence intervals. See SI Appendix (Table S5) for additional information.

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