Abstract

A new Turonian amber occurrence, representing the oldest in situ amber locality in Australia and the southern-most locality in Gondwana, has recently been discovered in the Otway Basin of Victoria. The amber was collected from petroleum cores and many pieces contain a range of inclusions that can provide information on the depositional history of the resin. To date, one species of fern spore (Cyathidites minor) and one species of lycophyte spore (Kraeuselisporites sp?) have been conclusively identified in the amber, along with filamentous microorganisms and degraded plant matter. Several samples are also rife with pseudoinclusions as reported recently in other ambers. The abundance of preserved particulate debris and wind dispersed spores suggest that the Otway amber formed subaerially. Furthermore, based on the range of bioinclusions and forms of pseudoinclusions preserved within a single piece of amber, the locus of hardening for individual samples is variably interpreted as occurring in the tree tops, on the tree trunk or on the ground surface. Notably, specific inclusion assemblages are associated with certain colours of amber. By extension, and in accordance with recent studies, amber colour may be indicative of depositional environment. Variation in the environment of solidification may, therefore, be sufficient to account for the broad range of morphological characteristics preserved in a single amber deposit.

Highlights

  • The first occurrence of Mesozoic amber from Australia has recently been discovered in Late Cretaceous (Turonian) rocks from offshore and onshore petroleum cores drilled in the Otway Basin, Victoria

  • Amber is extremely rare in Australia and in situ occurrences have only been reported from the Mio–Pliocene Latrobe Valley Coal exposed at Yallourn, Allendale and Lal lal in Victoria [1,2,3], and in the Eocene lignites exposed at Strahan in Tasmania [4]

  • The Turonian amber collected from the Otway Basin represents the oldest amber occurrence from Australia and the southern-most occurrence from Gondwana

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Summary

Introduction

The first occurrence of Mesozoic amber from Australia has recently been discovered in Late Cretaceous (Turonian) rocks from offshore and onshore petroleum cores drilled in the Otway Basin, Victoria. Both spores occur within the same piece of amber, along with mutually aligned filamentous microorganisms, decayed organic matter, irregular filamentous and amorphous inclusions. Aligned filaments (Fig 4D) are common and likely represent inclusions entrained in liquid resin and oriented in the direction of flow, e.g.

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