Sentence examples for study succession from inspiring English sources
A predicted model of the linkage between the study succession on SW Trinidad and its eastward continuation offshore towards the outer shelf and shelf edge in the Columbus Basin is suggested.
Succession from bare ground to a semi-stable old-field community occurs quickly – on the order of a few years – making it an ideal system to study succession.
The termination of whole study successions by a major incised valley and unconformity (Fig. 7, 1 3) coincides with all published papers on the Arabian plate margin (Lawa et al. 1998; Ali et al. 2014; Sharland et al. 2004).
Joseph Fan of the Chinese University of Hong Kong studied succession in 250 family firms in Hong Kong, Taiwan and Singapore and found that on average the firms lost 60% of their value in the period spanning five years before succession and three years afterwards.
Diagenesis, facies and palaeontology of the studied succession suggest a dominantly semiarid climate during the Triassic.
The studied succession can be subdivided into three unconformity-bounded sequences.
Four types of depositional systems are identified in the studied succession.
This might not be sufficient for studying succession mechanisms, including natural regeneration and changes in species composition over several centuries ([Strigul et al. 2008]).
The studied succession is grouped into two facies associations: (1) submarine gravity-flow sandstones and conglomerates; and (2) suspension-deposited shales and mudstones.
Accordingly, the studied succession is composed of five third-order sequences mostly controlled by tectonics, the most recent of which display complex patterns due to the interfingering of sedimentary bodies showing contrasting directions of progradation and pinch-out.
The marked environmental changes from subaqueous to continental and vice versa documented by the studied succession are inferred to be the expression of basin-scale tectonics, leading to uplift and exposure, superposed on the Mediterranean-scale base-level rise that followed the acme of the Messinian Salinity Crisis.
