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Fossil woods from the Late Cretaceous Aachen Formation
1Laboratory of Palaeobotany and Palynology, University of Utrecht, Budapestlaan 4, 3584 CD, Utrecht, The Netherlands
Fossil woods from the Late Cretaceous (Santonian) Aachen Formation reveal a diverse gymnosperm flora, indicating a warm, humid, and seasonal climate during this period.
Area of Science:
- Paleobotany
- Stratigraphy
- Paleoclimatology
Background:
- The Aachen Formation in Belgium, Netherlands, and Germany preserves Late Cretaceous (Santonian) fossil woods.
- Understanding the paleoflora and paleoclimate of this region provides insights into Cretaceous ecosystems.
Purpose of the Study:
- To investigate the composition and paleoecological significance of silicified fossil woods from the Aachen Formation.
- To reconstruct the paleoclimate based on the identified flora.
Main Methods:
- Systematic identification of silicified fossil wood specimens.
- Anatomical analysis of wood structure.
- Paleobotanical and paleoecological interpretation.
Main Results:
- The assemblage is dominated by gymnosperms, including Taxodiaceae (Taxodioxylon), Araucariaceae (Dammaroxylon), Pinaceae (Pinuxylon), and Cycad or Cycadeoid (Scalaroxylon).
- Angiosperms are present but less abundant, identified as Nyssoxylon, Mastixioxylon, Plataninium, and Paraphyllanthoxylon.
- The identified flora and wood anatomy suggest a warm, humid, and seasonal climate, likely warm-temperate to subtropical.
Conclusions:
- The Late Cretaceous Aachen Formation flora is predominantly gymnospermous.
- The fossil woods provide evidence for a warm, humid, and seasonal climate during the Santonian in this region.
- This study contributes to the understanding of Late Cretaceous paleoflora and paleoclimates in Western Europe.
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