A molecular phylogenetic approach was used to characterize the composition of microbial communities from two gas hydrate sedimentary systems in the Gulf of Mexico. Nucleic acids, extracted from sediments directly overlying surface-breaching gas hydrate mounds collected from a research submersible (water depth 550-575 m), were amplified with nine different 16S rDNA gene primer sets. The polymerase chain reaction primers targeted microorganisms at the domain-specific (Bacteria and Archaea) and group-specific (sulfate-reducing bacteria (SRB) and putative anaerobic methane-oxidizing (ANME) archaea) level. Amplicons were obtained with five of the nine primer sets including two of the six SRB Groups (SRB Group 5 and Group 6) and used to generate five different clone libraries. Analysis of 126 clones from the Archaea library revealed that the sediments associated with naturally occurring gas hydrate harbored a low diversity. Sequence analysis indicated the majority of archaeal clones were most closely related to Methanosarcinales, Methanomicrobiales and distinct phylogenetic lineages within the ANME groups. The most frequently recovered phylotypes in the ANME library were related to either ANME-2 or Methanomicrobiales. In contrast to the two archaeal libraries, bacterial diversity was higher with the majority of the 126 bacterial clones most closely related to uncultured clones dominated by the delta- and epsilon-Proteobacteria. Interestingly, while 82% of the clones in the SRB Group 5 library were affiliated with delta-Proteobacteria, the vast majority (83%) of clones in the SRB Group 6 library was affiliated with the Firmicutes. This is the first phylogenetic-based description of microbial communities extant in methane-rich hydrate-associated sediments from a hydrocarbon seep region in the Gulf of Mexico.

Salt pools are water-filled depressions common to north-temperate salt marshes. In Wells, ME, USA, cores reveal a unique salt pool signature consisting of watersaturated dark-gray mud often containing fragments of Ruppia maritima. Cores through pool sediment reenter salt marsh peat, not tidal flat sediment, demonstrating that most pools are of secondary origin. A principal component analysis of attribute data collected from 119 pools defines three distinct pool types: those with (1) surrounding highmarsh vegetation and thick heavily undercut banks (40% of the variance), (2) surrounding low-marsh vegetation and thicker slightly undercut banks (18% of the variance), and (3) surrounding low-marsh vegetation and less thick moderately undercut banks, containing R. maritima and a surficial drainage (15% of the variance). Cores and spatiotemporal analyses of aerial photographs between 1962 and 2003 reveal dramatic salt marsh surface dynamism suggesting that salt pools influence the geomorphological evolution of coastal marshes.

The mtDNA variation of 198 Aleuts, as well as North American and Asian populations drawn from the literature, were analyzed to reconstruct the Aleuts' genetic prehistory and to investigate their role in the peopling of the Circumarctic region. From median-joining network analysis, three star-like clusters were identified in the Aleuts within the following subhaplogroups: A3, A7 (an Aleut-specific subclade of A3), and D2. Mismatch analyses, neutrality test scores, and coalescent time estimates for these three components provided evidence of two expansion events, one occurring at approximately 19,900 B.P. and the other at 5,400 B.P. Based on these findings and evidence from the archaeological data, four general models for the genetic prehistory of the Aleutian Island chain are proposed: 1) biological continuity involving a kin-structured peopling of the archipelago; 2) intrusion and expansion of a non-native biface-producing population dominated by subhaplogroup D2; 3) amalgamation of Arctic Small Tool tradition peoples characterized by D2 with an older Anangula substratum; and 4) biological continuity with significant gene flow from neighboring populations of the Alaskan mainland and Kodiak Island. The Aleut mtDNAs are consistent with the Circumarctic pattern by the fixation of A3 and D2, and the exhibition of depressed diversity levels relative to Amerind and Siberian groups. The results of this study indicate a broad postglacial reexpansion of Na-Dene and Esko-Aleuts from reduced populations within northern North America, with D2 representing a later infusion of Siberian mtDNAs into the Beringian gene pool.

No abstract