Microbial Beachrock Formation: Implications for Island Stability in the Great Barrier Reef JENINE MCCUTCHEON*1 LUKE NOTHDURFT2, GREGORY E

Microbial Beachrock Formation: Implications for Island Stability in the Great Barrier Reef JENINE MCCUTCHEON*1 LUKE NOTHDURFT2, GREGORY E

Goldschmidt Conference Abstracts 2027 Microbial beachrock formation: Implications for island stability in the Great Barrier Reef JENINE MCCUTCHEON*1 LUKE NOTHDURFT2, GREGORY E. WEBB1, JEREMIAH SHUSTER1, LINDA NOTHDURFT1,2, DAVID PATERSON3, AND GORDON SOUTHAM1 1 School of Earth Sciences, The University of Queensland, St Lucia, QLD 4072, Australia 2 Earth, Environmental and Biological Sciences School, Queensland University of Technology, Brisbane, QLD 4000, Australia 3 Australian Synchrotron, Clayton, Melbourne, VIC 3168, Australia Beachrock forms through carbonate cementation of sediments in the intertidal zone of low-latitude beach environments. These lithified units play a key role in stabilizing sand cays in reef environments, and may become increasingly important to the existence of these islands as sea level rises. Although beachrock formation is influenced by many chemical and biological factors, the primary cause of this contemporary geological process has not been identified. In this study, the role of microorganisms in beachrock cement precipitation was investigated by synthesizing new beachrock using samples of beach sand, beachrock and associated microbial communities from Heron Island, Great Barrier Reef, Australia. Cements in natural and synthesized beachrock were characterized using synchrotron- based, X-ray fluorescence microscopy (XFM). The results of this study suggest that microbial recycling of ions within beach sediments plays an important role in cement precipitation. Dissolution of sand grains via boring by endolithic cyanobacteria generates high concentrations of soluble calcium and other cations. Cation enrichment combined with the highly alkaline microenvironments generated through cyanobacterial photosynthesis results in supersaturation conditions with respect to carbonate minerals. The microbial community also aids cement formation through the generation of extracellular polymeric substances that provide nucleation sites for carbonate mineral precipitation. Examination of this microbe-mineral interaction using high-resolution microscopy has allowed for the characterization of previously undetected features of beachrock cements. Understanding, and potentially accelerating, the processes responsible for early marine diagenesis and cementation may become vital to reef island stability and preservation in the near future. .

View Full Text

Details

  • File Type
    pdf
  • Upload Time
    -
  • Content Languages
    English
  • Upload User
    Anonymous/Not logged-in
  • File Pages
    1 Page
  • File Size
    -

Download

Channel Download Status
Express Download Enable

Copyright

We respect the copyrights and intellectual property rights of all users. All uploaded documents are either original works of the uploader or authorized works of the rightful owners.

  • Not to be reproduced or distributed without explicit permission.
  • Not used for commercial purposes outside of approved use cases.
  • Not used to infringe on the rights of the original creators.
  • If you believe any content infringes your copyright, please contact us immediately.

Support

For help with questions, suggestions, or problems, please contact us