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It’s not just Sand

Collecting and analyzing sediments is a key procedure in the field of Marine Geology. It may seem trivial to give so much attention to “sand”; however, the trained sedimentologist can learn a lot from a sample of ‘sand’, or sediment. We can understand something about the amount of energy coming into an area just by looking at the size of grains in the sediment.

 

Sediment Samples: An example of coarse grained sediment predominately found on the reef slope.   Note the larger grains, pieces of coral fragments, and calcified algal chips
An example of coarse grained sediment predominately found on the reef slope. Note the larger grains, pieces of coral fragments, and calcified algal chips

 

A sediment sample collected in low energy environments, like lagoons and deep offshore water, would have very fine grained, or small, sediments. A sample collected beside a reef would be expected to have coarser or larger grains.

 

An example of fine sediment found within a deep lagoon. Note the powder like consistency of the sand grains
An example of fine sediment found within a deep lagoon. Note the powder like consistency of the sand grains

 

We can also examine sediment samples to see what they are made of. Close examination of a sample under a microscope reveals if the grains come from coral, shell, or sea urchin fragments for example. A sample made mostly of coral fragments would likely have originated from a reef.

 

Close up view of a sediment sample
Close up view of a sediment sample

 

Recently we have been collecting sediment samples from lagoons and along barrier shelf reefs within the Gambier Archipelago. Preliminary evidence shows that sediments are more fine grained in the protected lagoon environment and coarser grained in the exposed barrier/shelf reef environment.

Microscopic view of an echinoderm spine found in a sediment sample
Microscopic view of an echinoderm spine found in a sediment sample

 

Ultimately, the results from the collected sediment samples will help us to better understand how physical forces like winds, waves and currents affect the distribution of sediment in this region.

Photos by Alexandra Dempsey

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