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Cenozoic plant diversity in the neotropics
Carlos Jaramillo1, Milton J Rueda, Germán Mora
1Center for Tropical Paleoecology and Archeology, Smithsonian Tropical Research Institute, Unit 0948, Army Post Office AA 34002-0948, USA. jaramilloc@si.edu
Neotropical plant diversity fluctuated significantly over 65 million years, with early Eocene flora exceeding modern levels. Climate change appears to be a key driver of these ancient tropical plant diversity patterns.
Area of Science:
- Paleobotany
- Palynology
- Neotropical Paleontology
Background:
- Understanding Neotropical plant diversity requires insights into geological time.
- Previous studies lack long-term diversification patterns for Neotropical floras.
Observation:
- A palynological record from Colombia and Venezuela spans the Paleocene to early Miocene (65-20 million years ago).
- The dataset includes 15 stratigraphic sections, 1530 samples, 1411 morphospecies, and 287,736 occurrences.
- This study presents the longest time series of Neotropical palynological plant diversity.
Findings:
- The Paleocene flora exhibited low diversity.
- The early to middle Eocene flora showed significantly higher diversity than present-day levels.
- Diversity declined at the end of the Eocene and into the early Oligocene.
Implications:
- Plant diversity fluctuations correlate strongly with global temperature changes.
- Tropical climate change may directly influence Neotropical plant diversity.
- Climate may control the available area for tropical plant growth, impacting diversity.
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