Abstract
For a short time interval (c. 1.2. Myr) during the early middle Eocene (~. 49. Myr), the central Arctic Ocean was episodically densely covered by the freshwater fern Azolla, implying sustained freshening of surface waters. Coeval Azolla fossils in neighboring Nordic seas were thought to have been sourced from the Arctic. The recognition of a different Azolla species in the North Sea raised doubts about this hypothesis. Here we show that no less than five Azolla species had coeval blooms and spread in the Arctic and NW European regions. A likely trigger for these unexpected Azolla blooms is high precipitation prevailing by the end of the warmest climates of the Early Eocene Climatic Optimum (EECO).
Original language | English |
---|---|
Pages (from-to) | 108-119 |
Number of pages | 12 |
Journal | Palaeogeography, Palaeoclimatology, Palaeoecology |
Volume | 337-338 |
DOIs | |
Publication status | Published - 15 Jun 2012 |
Funding
We thank L. Bik and N. Welters for their great support. We would like to thank J. van Tongeren in Utrecht and B.J. van Heuven in Leiden for technical support with the SEM work; and T. Brain in Kings College London for his extensive support with both TEM and SEM work during this study. We thank Nora Radionova for discussion of the palaeogeography of Western Siberia. JB thanks Arthur R. Sweet for many fruitful discussions. The samples and accompanying data for Azolla arctica ( Collinson et al., 2009 ), were provided by the Integrated Ocean Drilling Program (IODP). We thank Statoil and the Canadian Geological Survey for providing samples for this study. We thank the Darwin Centre , LPP Foundation and Statoil for their financial support.
Keywords
- Arctic ocean
- Azolla
- Early middle eocene
- EECO (early eocene climatic optimum)
- Fresh ocean surface waters
- Nordic seas