Pross, Jörg; Contreras, Lineth; Bijl, Peter K; Greenwood, David R; Bohaty, Steven M; Schouten, Stefan; Bendle, James A; Röhl, Ursula; Tauxe, Lisa; Raine, J Ian; Huck, Claire E; van de Flierdt, Tina; Jamieson, Stewart S R; Stickley, Catherine E; van de Schootbrugge, Bas; Escutia Dotti, Carlota; Brinkhuis, Henk; IODP Expedition 318 Scientists (2012): Pollen and spores, calculated temperature and precipitation of IODP Hole 318-U1356A. PANGAEA, https://doi.org/10.1594/PANGAEA.786960, Supplement to: Pross, J et al. (2012): Persistent near-tropical warmth on the Antarctic continent during the early Eocene epoch. Nature, 488(7409), 73-77, https://doi.org/10.1038/nature11300
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The warmest global climates of the past 65 million years occurred during the early Eocene epoch (about 55 to 48 million years ago), when the Equator-to-pole temperature gradients were much smaller than today (doi:10.1130/0091-7613(1995)023<1044:ECCALT>2.3.CO;2, doi:10.1038/nature08399) and atmospheric carbon dioxide levels were in excess of one thousand parts per million by volume (doi:10.1016/j.gca.2003.09.002, doi:10.1038/ngeo1186). Recently the early Eocene has received considerable interest because it may provide insight into the response of Earth's climate and biosphere to the high atmospheric carbon dioxide levels that are expected in the near future (doi:10.1007/s10584-011-0156-z) as a consequence of unabated anthropogenic carbon emissions (doi:10.1038/ngeo1186, doi:10.1038/nature06588). Climatic conditions of the early Eocene 'greenhouse world', however, are poorly constrained in critical regions, particularly Antarctica. Here we present a well-dated record of early Eocene climate on Antarctica from an ocean sediment core recovered off the Wilkes Land coast of East Antarctica. The information from biotic climate proxies (pollen and spores) and independent organic geochemical climate proxies (indices based on branched tetraether lipids) yields quantitative, seasonal temperature reconstructions for the early Eocene greenhouse world on Antarctica. We show that the climate in lowland settings along the Wilkes Land coast (at a palaeolatitude of about 70° south) supported the growth of highly diverse, near-tropical forests characterized by mesothermal to megathermal floral elements including palms and Bombacoideae. Notably, winters were extremely mild (warmer than 10 °C) and essentially frost-free despite polar darkness, which provides a critical new constraint for the validation of climate models and for understanding the response of high-latitude terrestrial ecosystems to increased carbon dioxide forcing.
Latitude: -63.310230 * Longitude: 135.998960
Datasets listed in this publication series
- Pross, J; Contreras, L; Bijl, PK et al. (2012): (Table S1) Pollen and spores of IODP Hole 318-U1356A. https://doi.org/10.1594/PANGAEA.786954
- Pross, J; Contreras, L; Bijl, PK et al. (2012): (Table S2) Bioclimatic analysis for IODP Hole 318-U1356A based on Greenwood et al., 2005. https://doi.org/10.1594/PANGAEA.786955
- Pross, J; Contreras, L; Bijl, PK et al. (2012): (Table S3) Bioclimatic analysis for IODP Hole 318-U1356A based on Mosbrugger and Utescher, 1997. https://doi.org/10.1594/PANGAEA.786956
- Pross, J; Contreras, L; Bijl, PK et al. (2012): (Table S4) Taxa defining the upper and lower limits in the application of the coexistence approach for paratropical rainforest biome. https://doi.org/10.1594/PANGAEA.786957
- Pross, J; Contreras, L; Bijl, PK et al. (2012): (Table S5) Taxa defining the upper and lower limits in the application of the coexistence approach for temperate rainforest biome. https://doi.org/10.1594/PANGAEA.786958
- Pross, J; Contreras, L; Bijl, PK et al. (2012): (Table S6) Calculated annual mean air temperature of IODP Hole 318-U1356A. https://doi.org/10.1594/PANGAEA.786959