Our results indicate grassland expansion between 2.0 and 1.75 Ma, coincident with major shifts in basin-wide sedimentation and hydrology.
The configuration of the earliest Karoo foreland system accounts for a forebulge elevated above the base level during Dwyka times, representing the early underfilled stage followed by a time of system-wide sedimentation during Ecca times (late underfilled stage), when the forebulge subsided below the base level under the influence of dynamic subsidence.
Experimental studies using particle image velocimetry have demonstrated that this reactor provides good fluid mixing, and is able to suspend catalyst particles with a wide range of sedimentation velocities.
Lee et al. (2014b)'s work at another GSF site near Suwolbong (hereafter referred to as GSSW; see Fig. 1b) has also yielded a line of AMS 14C dates, suggesting a wide range of the GSF sedimentation age from 24 to 16 cal.
In some cases, the basins contained extremely thick accumulations of sediment, had high sedimentation rates, and contained formations with abnormally high organic carbon contents; The basins overlie a wide range of rift structures of different ages in their basement complexes and were subject to intense heat and mass transfer associated with rifting.
Some of these features are: In some cases, the basins contained extremely thick accumulations of sediment, had high sedimentation rates, and contained formations with abnormally high organic carbon contents; The basins overlie a wide range of rift structures of different ages in their basement complexes and were subject to intense heat and mass transfer associated with rifting.
The former architecture is interpreted as the product of flow containment of incoming flows by lateral basinal slopes with consequent deposition under confined accommodation space, whereas the latter would record sedimentation within a wider depocentre allowing for free flow expansion and lateral migration of lobes.
Coral skeletal morphology can be remarkably phenotypically plastic, responding to a wide variety of parameters such as light, sedimentation, water motion, water chemistry, and ecological interactions [ 2, 4].
Solid liquid separation by filtration and sedimentation are important operations used in a wide range of industries.
This conclusion is further supported by the sucrose gradient fractionation data presented in Fig. 1, showing a spread distribution of Bcl-xL over a wide range of molecular weights, without discrete peaks of sedimentation.
