Abstract. Marine microorganisms trapped in amber are
extremely rare in the fossil record, and the few existing inclusions
recovered so far originate from very few pieces of Cretaceous amber from
France. Marine macroscopic inclusions are also very rare and were recently
described from Cretaceous Burmese amber and Early Miocene Mexican amber.
Whereas a coastal setting for the amber source forests is generally proposed,
different scenarios have been suggested to explain how these marine
inclusions can become trapped in a resin of terrestrial origin. These
scenarios include an introduction of marine organisms (i) through high tides,
(ii) from storms and resulting in flooding of the littoral/estuarine forest
floor, (iii) in resin dropped into the sea in mangrove-type settings, or
(iv) by wind and sea spray. We investigated the possibility of a wind-driven
introduction of marine microorganisms into tree resins using modern coastal
conifer forests with the highly resinous Cook pine (Araucaria columnaris) in New Caledonia as a model for the Cretaceous amber forests
from France. By exposing fresh resin surfaces on the seaward side of the
trees and the collection of older in situ resins, we confirmed that marine
microorganisms can become trapped on sea-exposed resin, along with remnants
from terrestrial organisms, and salt crystals. We suggest that, for cases
where only a few marine inclusions are discovered in an amber deposit, an
origin from aeolian background deposition is feasible. However, a more
energetic but possibly still aeolian event is likely needed to explain the
high numbers of marine microorganisms embedded in pieces of Cretaceous amber
from France.