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The thickness (or height) of a gravelly beach ridge approximately equals the height of wave inundation, which is the sum of the surge and wave run-up. Their ancient counterparts, if well-preserved and identified, can be used to estimate palaeowave conditions, which can later be converted to palaeowind intensities based on wind wave relationships. A technique is described for estimating the palaeowind speed in this paper, which is referred to as the gravelly beach-ridge thickness technique. By comparing these estimates with instrumental wind records obtained at a modern lake, Qinghai Lake in north-western China, the beach-ridge thickness technique is shown to be useful for estimating the average wind speed (Vavg). When applying this method to ancient fetch-limited basins, five parameters are necessary: (i) the thickness of the isolated gravelly beach ridge; (ii) the average depth of the water body; (iii) the palaeofetch; (iv) the angle between the palaeowind direction and the normal to the shoreline; and (v) the particle size. This technique was applied to an ancient example in the Eocene Dongying Depression, located in eastern China. The results indicate that the average wind speed of the northern wind ranged between 2.27 m sec-1 and 8.36 m sec-1 from 45.0 Ma to 42.0 Ma, and displayed a generally decreasing trend that included early strengthening followed by weakening and later strengthening during this period. The beach-ridge thickness technique provides a new perspective on delineating palaeowind conditions and can be applied to ancient fetch-limited basins with gravelly beach ridges worldwide. Generally, if a water body is sufficiently large (fetch exceeding 40 km), deep (average depth exceeding 10 m) and waves (or winds) are determined to approach the shoreline with high angles (angle of incidence <35), then the calculation errors will be small to negligible.  TyConstruction and destruction of an autogenic grade system: The late Holocene Mekong River delta, Vietnam[be2019Grade, a fundamental concept in river geology and geomorphology, refers to a long-term sediment balance hat is accompanied by zero net deposition and erosion. Recent physical and theoretical modeling proposed the notion that downstream alluvial rivers can autogenically attain grade only in a particular set of nvironmental conditions that include a constant fall of relative sea level. We here make the first successful identification of an autogenic grade system in the geological record: the late Holocene Mekong River delta, Vietnam. From 3.5 ka to subrecent, the record of the delta exhibits peculiar features, including (1) no trace of significant sediment accumulation and erosion on the delta plain surface, (2) a delta plain surface with the same slope as the underlying shelf surface, (3) distributary channels that are stabilized in transverse directions but extend linearly basinward, and (4) a delta set thickness that matches a theoretical value. These features in combination are indicative of autogenic grade. Coastal dispersal of river-derived sediment by tides, waves, and ocean currents, as well as tectonic features and mangrove vegetation, may have contributed to the attainment and maintenance of grade. Ongoing drastic changes in sea level and human activities have caused the downstream Mekong River to become ungraded and unstable with a much higher risk of channel avulsion and shifting than in the past.  TyMorphodynamics of river deltas in response to different basin water depths: An experimental examination of the Grade Index model[be2019Basin water depth (h) governs the long term morphodynamics of river deltas, which are embodied in the grade index (Gindex). The Gindex, a volume in unit time ratio of subaerial sediment allocation to the entire supplied sediment, can be given as a function of the dimensionless basin water depth (h*). Tank experiments reported herein reveal that delta progradation and deltaplain aggradation are suppressed and distributary channel migration and avulsion take place less frequently when the Gindex value is lower (i.e., when the basin water is deeper; h*?1). If the Gindex~0 (i.e., extremely deep basin water; h*~+"), the delta can neither prograde nor aggrade, and the distributary channels tend to stabilize. The grade index model helps explain the contrasting morphodynamics of the Liwu Delta (east Taiwan) and Yellow River Delta, as natural examples of deepwater and shallow water deltas, respectively.  TyThe grade index model as a rationale for autogenic nonequilibrium responses of deltaic clinoform to relative sea level rise[be2020Grade index (Gindex) is a dimensionless number given as the volume in unit time ratio of subaerial allocation to both subaerial and subaqueous allocations of sediment supplied to a delta from upstream. It was originally proposed for understanding the effect of basin water depth on the morphodynamics of delta distributary channels under stationary relative sea level. We here examine how rising relative sea level modulates the Gindex, using geometrical reasoning and numerical simulations. We find that the grade index model can account for autoretreat of the deltaic shoreline, autodrowning of the whole system, and autobreak of the deltaic sedimentation, all of which are the consequences of autogenic nonequilibrium responses to steadily rising relative sea level. The regressive to transgressive threshold (i.e. the onset of autoretreat) is crossed when the delta plain's dimensionless basal area (At*) encounters a critical value that is expressed in terms of Gindex: regression and transgression are sustained when At* is below and above the threshold, respectively. The mode of transgression depends on the slope conditions. If the hinterland slope () is steeper than the foreset slope (), both At* and Gindex decrease as the relative sea level rises. Eventually, the depositional system experiences autodrowning when At* = Gindex = 0. If  < ; on the other hand, both At* and Gindex increase. This latter slope condition eventually causes autobreak of the deltaic sedimentation, afterward of which At* = Gindex = 1. The grade index model is useful for interpreting and predicting the stratigraphic responses of natural deltaic clinoforms in conditions of rising relative sea level.  TyAutostratigraphic modelling of the growth of alluvial-shelf systems during steady base-level cycles: Two-dimensional tank experiments[be2021Autostratigraphy is the stratigraphy generated by large-scale autogenesis, developed based on the full recognition of the non-equilibrium behaviour of depositional systems in response to steady external forcing. The existing autostratigraphic concepts were derived mostly from studies of river deltas growing during a single rise or fall of base level (or relative sea level). The present study challenges to extend the autostratigraphic framework to the alluvial-shelf system growing through steady base-level cycles by two-dimensional tank experiments. During each experimental run, the base level was changed symmetrically, wherein through cycles, the rise and fall had the same constant rate (|Rbl|) and period (Tbl), and thus the same constant amplitude (Abl), but with no basin tectonism. In total, nine runs with different combinations of |Rbl| and Abl were performed. The experimental results brought the following implications. (i) The shelf-transiting active depositional system takes non-equilibrium responses in earlier base-level cycles, during each of which the system experiences episodes of degradation with base-level fall. (ii) After the system has sufficiently grown through cycles, non-equilibrium responses change into equilibrium responses, whereby the shelf-transiting alluvial system, whether retrogradational or progradational, is free from degradation and continues to aggrade but with a gradually decreasing rate of aggradation. (iii) The alluvial topset river tentatively but autogenically attains a graded state during the falling limb of an intermediate cycle, which separates the earlier degradation-inclusive and later aggradation-sustainable cycles. (iv) The number (or duration) of cycles elapsed prior to this phase-transition is linearly proportional to the amplitude (or the square of the period) of base-level cycles, with a coefficient defined by the rates of base-level change and sediment supply. Such a growth pattern does not necessarily hold when considering long-term tectonic subsidence or uplift. These notions help to understand the stratigraphic architectures of natural alluvial-shelf systems evolved through base level cycles.  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