Description and interpretation of a fossil beetle assemblage from marine isotope stage 6 from Banks Peninsula, New Zealand

Abstract

A penultimate glaciation‐age beetle fauna is described from a core record from Banks Peninsula, South Island, New Zealand. A total of 19 beetle species belonging to 5 families was recorded. The fossil beetles indicate a forest environment of montane affinity but in a coastal setting. The assemblage is dominated by phytophagous species, mainly weevils, associated with forest habitats. The beetle fauna includes Rhicnobelus metallicus, which is a forest canopy species; forest floor and swamp forest taxa; and Cecyropa modesta, which is specific to coastal dune systems. Fossil seeds were also identified. They include species from salt marsh and tidal flats, indicating an estuarine setting, which suggests that the beetle remains were washed into an estuary from an adjacent forest. The fossil beetle assemblage indicates cooler than modern conditions but not full glacial. This interpretation is consistent with the regional pollen record for this interval.

Keywords:

• fossil beetles
• paleoclimate
• environmental reconstruction
• paleoecology
• penultimate glaciation