Sentence examples for sedimentary surface from inspiring English sources
The latter include likely microbial sedimentary surface textures, the enigmatic matground "pseudofossils" Aristophycus and Arumberia, and probable mat fragments and mat-related microtextures preserved in argillaceous sediment.
We also extrapolated the path taken by each body part of the tracemaker that did not interact directly with the sedimentary surface.
We propose that the mouth is the most likely part of teleost anatomy that could have interacted with the sedimentary surface and produced such a series.
Furthermore, the caudal and pelvic fins of N. osculus extended ventrally enough to have incised the sedimentary surface while swimming within a few centimeters of that surface, while minimizing contact of the anal fin with forward movement.
The single, high-amplitude trail is ascribed to the caudal fin, which was formed as an incision of the sedimentary surface by the ventral (distal end) of the fin as it moved the fish along the bottom.
Furthermore, our mathematical extrapolations of the incomplete waveforms define, with high probability, the locations of each tracemaking appendage above the sedimentary surface, even where no traces were made, as well as the size of the fish (Figure 5).
Also known as sand snakes, streamers are a familiar manifestation of pronounced spatial and temporal variability in wind-blown sand over beaches, dunes, and other sedimentary surfaces.
The intrinsic characteristic of filamentous microbes to form cohesive layers at sedimentary surfaces is also known to substantially decrease wind and water erosion in modern arid and semiarid areas of the world (Belnap and Gillette 1998; Belnap and Lange 2001).
Within the coastal plains and lowlands of the North Pacific Region, repeating transgressions and regressions and lateral river channel migration constantly disturbed environments and provided fresh sedimentary surfaces that were colonised by angiosperms more readily than by other plants.
Two types of sequence boundaries (regional unconformities and regional exposed non-sedimentary surfaces) and double systems tract boundaries (maximum flooding and first flooding surfaces) are identified.
In spite of its notable sedimentary volume (surface area = 1200 km2), the MICCSC lacks a clear sediment source, or supply mechanism, to explain its presence today.
