Planktonic foraminifera distribution during the mid-Piacenzian warm period in the North Atlantic ...
The mid-Piacenzian (MP) warm period (3.264-3.025 Ma) has been identified as the most recent time in geologic history during which mean global surface temperatures were considerably warmer than today for a sustained period. This interval has therefore been proposed as a potential (albeit imperfect) a...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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PANGAEA
2011
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| Online Access: | https://dx.doi.org/10.1594/pangaea.774590 https://doi.pangaea.de/10.1594/PANGAEA.774590 |
| Summary: | The mid-Piacenzian (MP) warm period (3.264-3.025 Ma) has been identified as the most recent time in geologic history during which mean global surface temperatures were considerably warmer than today for a sustained period. This interval has therefore been proposed as a potential (albeit imperfect) analog for future climate change and as such, has received much scientific attention over the past two decades. Central to this research effort is the Pliocene Research, Interpretation, and Synoptic Mapping (PRISM) project, an iterative paleoenvironmental reconstruction of the MP focused on increasing our understanding of warm-period climate forcings, dynamics, and feedbacks by providing three-dimensional data sets for general circulation models. A mainstay of the PRISM project has been the development of a global sea surface temperature (SST) data set based primarily upon quantitative analyses of planktic foraminifer assemblages, supplemented with geochemical SST estimates wherever possible. In order to improve ... : Supplement to: Lutz, Brendan P (2011): Shifts in North Atlantic planktic foraminifer biogeography and subtropical gyre circulation during the mid-Piacenzian warm period. Marine Micropaleontology, 80(3-4), 125-149 ... |
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