Sentence examples for saline sediments from inspiring English sources

The lacustrine saline sediments of the Lagoa Feia Formation (source rock) were interpreted as the source for the typical "Campos oils", including the samples P1 (Coquinas reservoir in Lagoa Feia Formation, classified as not biodegraded) and P2 (Calcarenites reservoir in Macaé formation, classified as biodegraded) (Mello et al. 1988; Mohriak et al. 1989), see Figure 2.

P. diplantherae branches robustly within phagomyxids, sister to two environmental sequences which were found in clone libraries of deep-sea/anoxic saline sediments [ 9, 10].

(2011) examined the distribution of OTUs in different habitats such as soils, lakewater, and saline sediments and found that no OTU was ubiquitous in any habitat even when the sequence identity threshold was set as low as 89%.

One sample from the transition between normoxic, normal saline sediments and the upper halocline of Urania (607-608cC; Fig.  1c) had numerous specimens of what appear to be a single bryozoan morphotype (Fig.  6).

These fossils only found in the freshwater-less saline sediment, reflecting low temperature conditions, are the division of the Quaternary and the Neogene in Qaidam Basin (Xie and Guan 2000).

The strain FAS23 isolated from saline sediment collected from Tunisian arid ecosystems was identified as an actinobacterium belonging to the genus Janibacter sp., with respect to morphological and biochemical tests and 16S rRNA gene sequence.

We constructed a nucleosome occupancy map of the halophilic archaeon Haloferax volcanii, a member of the phylum euryarchaeota, originally discovered in the highly saline sediment of the Dead Sea (Mullakhanbhai and Larsen, 1975).

Using that same rationale, while we found Spinoloricus cinziae in L'Atalante control and L'Atalante lower halocline samples, the likelihood that the same species of Spinoloricus inhabits both the normoxic, normal saline control sediments and thalassohaline lower halocline sediments is low due to substantial differences in the chemistry of bottom waters overlying sediments and pore waters.

From previous studies of the Sr/Ba ratio of continental basins in China, the Sr/Ba ratio is more than 1 in saline lake sediments and less than 1 in freshwater sediments (e.g., 1.0 0.6 in semi-saline water facies and < 0.6 in brackish-water facies) (Deng and Qian 1993; Wang et al. 1979; Zheng and Liu 1999).

Herein, we report results of visually-guided sediment coring on the metazoan assemblages in DHAB halocline and adjacent normoxic, normal saline (control) sediments, providing additional information on whether observed metazoa represent living eukaryotic populations.

The members of this genus have been isolated from various environments such as soil and saline lake sediments (An et al. 2007 and Liu et al. 2010).