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Subseafloor structures and high methane concentrations of up to 30 μmol/l in sediment pore water samples suggest a source of shallow biogenic methane from the decomposition of postglacial deposits in a paleo river valley.
Whaling records suggest that Antarctic sea ice extent decreased by approximately 25percentt between the mid-1950s and early 1970s, whereas ice core samples suggest a 20percentt decrease in sea ice extent since 1950.
Indeed, two meta-analyses have now shown that the effect sizes in BD samples suggest a moderate impairment in MMN, compared to the large effect sizes shown in schizophrenia.
The patterns observed in these and other samples suggest a fractionation process where residual congener pools can become progressively enriched while the congeners produced from degradation are more depleted.
Small Angle Neutron Scattering patterns of the pressed samples suggest a preferential orientation of the vermiculite particles for which the basal planes were arranged perpendicular to the compaction axis.
Soil samples suggest a date of 1850 BC, but they are unique to St Kilda, and their purpose is unknown.
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The n-alkanes distribution profiles observed for the studied samples suggest an abundance of low molecular weight compounds in the Upper Eocene sequence, which is consistent with higher marine input.
But the presence of some unmetabolized DDT in the samples suggests a fresh source.
For many pairs we found at least one mutation with high VAF in both samples suggesting a common founding clone.
Generally, there was a separation between the SHR and Wistar samples, suggesting a unifying transcriptomal trend amongst the biological replicates from each strain.
Addition of R‐138727 reduced prothrombin cleavage in eptifibatide‐treated samples, suggesting a novel mechanism for potential benefit from combined prasugrel and eptifibatide treatment.
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