Exact(1)
Fossil evidence from diatoms and oomycetes was used to calibrate the molecular clock analyses; all calibrations were modeled with a gamma prior distribution (shape 2.0) with the offset value set as the uppermost boundary of the time interval (stage) containing the relevant fossil.
Similar(59)
However, its validity is supported by a large positive shift in δO close to the lower/middle Ottnangian boundary (uppermost Neuhofen Beds; Janz and Vennemann, 2005).
At the uppermost part of the plate boundary, though, the figure was closer to a hundred feet.
Correspondingly, rlk902 seedling roots displayed a reduced meristem size compared to wild type visualized by the root meristem boundary marking the uppermost cortical meristem cell showing no signs of rapid elongation (Figure 1c,d).
However, since the late 1950s, micropaleontologists have recognized that calcareous marine plankton (foraminiferans and coccolith-bearing nannoplankton) exhibit a major taxonomic change at the boundary between the Maastrichtian (uppermost Cretaceous) Stage and the Danian (lowermost Tertiary) Stage.
Deep and difficult to reach IODP scientific targets, such as the plate-boundary seismogenic zone, Moho and uppermost mantle, and deep sedimentary sections theorized as the limit of the deep biosphere, all demonstrated the need for a riser drilling system.
The nanoscale mixture also decorates the grain boundaries and cavities of the uppermost 100 250 μm of the rock-atmosphere interface, strongly altering the color of the red stone to lustrous black despite the relatively small mass of the deposits.
Seneca sandstone on the Smithsonian Castle and gateposts is discolored in patches owing to the Mn-rich phase being deposited into two zones: (1) a vanishingly thin patina, and (2) nanoparticles coating grain boundaries and pores in the uppermost ~200 250 μm of the stone.
Cells in the uppermost focal plane and/or intersecting the exclusion boundaries of the counting frame were not counted.
The uppermost mantle structure beneath this arc is an important boundary condition for evolutionary processes of the volcanoes and crustal structures.
Three samples have been taken within a few metres of the section from the uppermost Neuhofen Beds (lower Ottnangian; HM 2) and the boundary interval (HM 3, HM 4; transition from lower Ottnangian Neuhofen Beds to middle Ottnangian Glaukonitsande & Blättermergel; Pippèrr, 2011).
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