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A fine-grained pumice fall deposit (unit 1) is overlain by a fine-grained grey ash interpreted as of phreatomagmatic origin (unit 2).
Single channels are formed by repeated gravity-flow deposits along one channel over a period of time, a major origin unit in turbidite channels.
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For each individual, age in 2007, sex, country of origin, units of antidepressants from the NO6A subgroup in the ATC classification system [ 5] dispensed at pharmacies, the active ingredient, and month and year of dispensation were recorded.
Based on visual comparison of banding intensity, there is higher rDNA expression of T. dubius-origin units than of T. porrifolius-origin units in all plants from all populations examined, except for individuals from the Palouse population (Additional file 3).
The Southern blot and FISH data further show that this was mainly caused by underrepresentation of T. dubius-origin units.
There was little or no variation in the gene ratios among the individuals analyzed, and all individuals had reduced Southern hybridization signal against the T. dubius-origin units.
In synthetic T. miscellus, three individuals (4%) had balanced gene ratios while 65 individuals (92%) inherited more T. pratensis-origin units than expected.
All individuals from eight lineages showed relatively uniform Southern hybridization profiles, with band ratios highly skewed towards the T. porrifolius-origin units.
Only two allotetraploid individuals were recovered from this cross, and both had gene ratios highly skewed away from T. dubius-origin units.
While both lineages 135-1 and 135-2 had gene ratios skewed towards T. porrifolius-origin units, the gene ratios were balanced in the 135-5 individuals.
It is also difficult to exclude explicitly the tsunami origin of unit 3; however, the laminations in its fine-grained part (units 3A and 3C) indicate recurring, more regular events (Palinkas et al., 2006) in the past.
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