| Literature DB >> 29939174 |
Tiffany Playter1, Kurt Konhauser2, George W Owttrim3, Denise S Whitford3, Tyler Warchola2, Cheryl Hodgson4, Aleksandra M Mloszewska5, Bruce Sutherland2, J-P Zonneveld2, S George Pemberton2, Murray K Gingras2.
Abstract
The mechanisms underpinning the deposition of fine-grained, organic-rich sediments are still largely debated. Specifically, the impact of the interaction of clay particles with reactive, planktonic cyanobacterial cells to the sedimentary record is under studied. This interaction is a potentially major contributor to shale depositional models. Within a lab setting, the flocculation and sedimentation rates of these materials can be examined and measured in a controlled environment. Here, we detail a protocol for measuring the sedimentation rate of cyanobacterial/clay mixtures. This methodology is demonstrated through the description of two sample experiments: the first uses kaolin (a dehydrated form of kaolinite) and Synechococcus sp. PCC 7002 (a marine coccoid cyanobacteria), and the second uses kaolin and Synechocystis sp. PCC 6803 (a freshwater coccoid cyanobacteria). Cyanobacterial cultures are mixed with varying amounts of clay within a specially designed tank apparatus optimized to allow continuous, real-time video and photographic recording. The sampling procedures are detailed as well as a post-collection protocol for precise measurement of chlorophyll a from which the concentration of cyanobacterial cells remaining in suspension can be determined. Through experimental replication, a profile is constructed that displays sedimentation rate.Entities:
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Year: 2018 PMID: 29939174 PMCID: PMC6101692 DOI: 10.3791/57176
Source DB: PubMed Journal: J Vis Exp ISSN: 1940-087X Impact factor: 1.355