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Among the participants at Friday’s meeting were Inyo County Chief Administrative Official Kevin Carunchio, Inyo County Supervisors Jeff Griffiths and Mark Tillemans, Mammoth Mayor John Wentworth, Town Manager Dan Holler, TOML Public Works Director Grady Dutton, Mammoth Yosemite Airport Manager Brian Picken, Inyo County Public Works Director Clint Quilter, and Pat Foster of Hot Creek Aviation.

Mono County Supervisors Stacy Corless and Bob Gardner were present as “members of the public.” At the outset of the meeting, there was some confusion expressed about whether or not the meeting was subject to the Brown Act.

The RFQ cites high cancellation rates as a result of inclement weather as a major reason for reassessing existing air service.

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Sequencing of 16S r RNA gene libraries revealed that the dendrolitic cone tips were enriched in OTUs most closely related to the genera Phormidium, Leptolyngbya, and Leptospira, whereas mats at the base and adjacent to the dendrolitic cones were enriched in Synechococcus.

We hypothesize that the consumption of nutrients during autotrophic and heterotrophic growth may promote movement of microbes along diffusive nutrient gradients, and thus microbialite growth.

Dutton also announced that Mammoth Lakes Tourism had issued a Request for Qualifications (RFQ) on May 25 for a five to ten year “Eastern Sierra Air Service Strategic Plan.” The RFQ indicated that the TOML was interested in working with the operators of Bishop Airport to provide “reliable regional air service.” Dutton said that, as part of that project, consultants will assume that the “Design Aircraft” for Mammoth Yosemite Airport could change.

The Federal Aviation Administration (FAA) defines the Design Aircraft or Critical Aircraft of a given airport as the “aircraft type with the most demanding facility needs that has regular use if the runway [at least 500 flights per year].” The FAA also sets the Design Aircraft for a given airport, which is effectively a limit on the size of the planes that make regular use of the airport.

The microbial composition of the dendrolitic cones, underlying microbial mat, and the layered microbial mat from an adjacent outflow pool (LHC Outflow pool) were determined by sequencing amplified libraries of small subunit ribosomal 16S r RNA genes.

The autotrophic growth rates of the community were measured by C-bicarbonate uptake from dissected samples of the tips of dendrolitic cones.

It is useful to characterize these and other modern conical analogs of ancient microbialites to support the development of a formation model and to better understand their preservation potential in rock over geological timescales.

Here, we present a detailed physical, geochemical, and genomic characterization of semi-lithified carbonate, dendrolitic conical microbial structures (i.e.

Thus, we provide a new model system to address how microbial mats may be preserved over geological timescales.

However, as structures that have undergone lithification and post-depositional diagenetic alteration, most ancient microbialites lack preserved microfossils or unobscured information concerning their formation and the chemistry of their environments.

Hour-glass shaped filamentous structures present in the dendrolitic cones may have formed around photosynthetically-produced oxygen bubbles—suggesting that mineralization occurs rapidly and on timescales of the lifetime of a bubble.

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