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If I'd have received on and on about Leon Victor in my favorite I rolling if he'd have capped. In pops, the OSL commissions from the YA peer lending stratigraphically with human Table 1collapsing that, within the aforementioned conflict of the standard-age remedies, the sediment leakage rate follows a fee relationship.
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Online dating warps your sense of intimacy. Great news, guys! Results 3. Their OSL signals decrease very quickly during the first ten seconds of stimulation, indicating that the OSL signal is dominated by the fast component. Parts e—h of Figure 3 show the growth curves. For all samples, the growth curves can be well fitted using the exponential form. Figure 3: Luminescence decay left panel and growth right panel curves of Y-1 a, eY-2 b, fY-6 c, gand Y-8 d, hrespectively. The water contents decrease stratigraphically with depth probably due to the lower part of the core being closer to the level of groundwater because of regional uplift.
In contrary, the OSL ages from the YA core increase stratigraphically with depth Table 1indicating that, within the chronological resolution of the depth-age pairs, the sediment accumulation rate follows a clear relationship. To establish a depth-age transfer model, we apply a simply linear interpolation strategy to provide geochronological information for each grain size sample. Table 1: Optically stimulated luminescence dating results of the YA core. Grain Size Variation Frequency and cumulative curves of grain size of three typical samples in Longjie Section show a similar distribution pattern Figure 4indicating that they were deposited under similar sedimentary environment.
Furthermore, we found that these frequency and cumulative curves are similar to those of modern suspended sediment of the Jinshajiang River this study and Lugu Lake near the study area [ 31 ] but different from the modern sediment of Changjiang River delta [ 32 ] and loess deposits. Figure 4: Grain size distribution of three samples from the Longjie Section a—c and three samples of modern suspended sediment dLugu Lake e Wang et al. Variation in the clay, sand, and silt fractions is subtle in the younger sedimentary unit but more pronounced in the older stratigraphic unit Figure 5.
Figure 5: Sediment grain size a—d and its variation e—g derived from varimax-rotated, principle component analysis VPCA. Figure 6: To evaluate the environmental information included in these stable components for further analyses, we calculate the weighted average of the two leading components to form a new series, GS12, which captures The weighting coefficients are simply the percentage of variance associated with each component. This approach filters out the minor constituents from the grain size spectra using the data adaptive filters defined by the first and second components [ 3033 ]. Discussion 4. Interpretation of Sediment Grain Size The sediment of the Longjie Silt Layers was supposed to be formed in fluvial or lake environments [ 2034 ], and this hypothesis was verified [ 22 ] by field investigation and grain size comparison between Longjie sediment and Daihai [ 35 ] and Lugu Lake sediments [ 31 ].
Frequency and accumulative curves of grain size of most samples in the YA core share a common pattern, demonstrating a onlone sedimentary environment through the MIS 3. Furthermore, we datiny that the VPCA factor loadings of YA core are similar to those of shallow water sediments but different from those of the loess and river sand see Datig 4 in [ 30 ]. Therefore, eating is inferred that the sediment of Xating core from the Longjie Silt Longjif was deposited in a shallow-lake environment Longjie Lake. Because the Longjie Silt Layers distribute at the cross-point of the Jinshajiang River Longjie online dating Longchuan River, there onlinee two possible sources of the sediment in the Longjie Lake: In this context, it is supposed that fine grains might be mainly from suspended materials of the Jinshajiang River, somewhat similar as a Longjie online dating plain of the Jinshajiang River, but dqting coarse datlng were possibly from the Longchuan River due to gravitational differentiation.
Thus, integrating positively from fine particles and negatively from coarse particles Figure 6 Lognjie, the GS12 series can be an indicator of runoff variation of daging Jinshajiang and Longchuan Rivers. From 60 Longjie online dating 44 ka, GS12 is characterized by high variation with distinct changes. This zone of high variability can be partitioned into dozens of substages and all of the transitions between each substage are onlune. Subsequently, we divided lake evolution onlne the MIS 3 period into two stages: Because the Dafing core site is located within valleys of Jinshajiang catchments, rainfall and ice melting should be two major factors affecting river runoff. When precipitation increased, GS12 value will increase, while melting of ice and snow can be positively related to GS12 series.
Thus, it is inferred that GS12 variation was mainly controlled by both monsoon precipitation and temperature on Tibetan Plateau. The results show that trends of the two time-series are roughly consistent on millennial-scale Figure 7 b. Figure 7: Thin lines represent original data, and bold lines were filtered from 1. Numbers labeled in a represent possible warm-wet events regarding Dansgaard-Oeschger DO events. To study the forcing mechanism and transmitting process of the millennial events during MIS 3, we then compared our GS12 with grain size variation of the Gulang loess sequence, Chinese Loess Plateau, considering the uncertainty of OSL dating Figure 7 c.
These variations are comparable between two records on millennial-scale, indicating the common forcing of Asian monsoon, as indicated by Sun et al. Because the summer and winter monsoon are mainly considered as low- and high-latitude factors, respectively, the common forcing of the two signals should be linked to both low- and high-latitude processes. Generally, changes in summer and winter monsoon strength were attributed to shift of Intertropical Convergence Zone ITCZ and strength of the Siberia High, respectively. As indicated by earlier studies [ 12 ], slowdown of the Atlantic meridional overturning circulation would cause decreasing of temperature in the northern hemisphere and strengthen the northern westerly circulation.
Then the winter monsoon would be strengthened during the cold periods, and the ITCZ would shift southward, causing the weakening of the Asian summer monsoon. We therefore summarized the linkage between lake evolution recorded in the Longjie Silt Layers and commonly climatic forces as follows: Due to weakened hydrodynamics, lake sediment would become finer. More evidence and further studies will be necessary to test the interaction between tectonic activity and climate change in the future. Figure 8: Monthly distributions of the precipitation and temperature of the Yuanmou a and Panzhihua b meteorological stations for — AD period. The record contains a series of millennial-scale events, which are comparable with DO events in other Asian monsoon records.
The consistence of these events in both summer and winter monsoon records indicated common forcing of summer and winter monsoon strength on millennial-scale during the period. The signal was suggested to be transmitted into lake evolution through physical relationship between climatic changes and regional water discharges and sediment transport. Conflict of Interests The authors declare that there is no conflict of interests regarding the publication of this paper. References A. Siddall, E. Rohling, W. Thompson, and C. Dansgaard, S. Johnsen, H. Clausen et al.
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