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Schmidt-hammer exposure ages from periglacial patterned ground (sorted circles) in Jotunheimen, Norway, and their interpretative problems

机译:挪威Jotunheimen的沿冰川纹地面(分类圆)施密特锤的暴露年龄及其解释性问题

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摘要

Periglacial patterned ground (sorted circles and polygons) along an altitudinal profile at Juvflya in central Jotunheimen, southern Norway, is investigated using Schmidt-hammer exposure-age dating (SHD). The patterned ground surfaces exhibit R-value distributions with platycurtic modes, broad plateaus, thin tails , and a negative skew. Sample sites located between 1500 and 1925 m a.s.l. indicate a distinct altitudinal gradient of increasing mean R-values towards higher altitudes interpreted as a chronological function. An established regional SHD-calibration curve for Jotunheimen yielded mean boulder exposure ages in the range 6910 ± 510 to 8240 ± 495 years ago. These SHD ages are indicative of the timing of patterned ground formation, representing minimum ages for active boulder upfreezing and maximum ages for the stabilization of boulders in the encircling gutters. Despite uncertainties associated with the calibration curve and the age distribution of the boulders, the early-Holocene age of the patterned ground surfaces, the apparent cessation of major activity during the Holocene Thermal Maximum (HTM) and continuing lack of late-Holocene activity, clarify existing understanding of the process dynamics and palaeoclimatic significance of large-scale sorted patterned ground as an indicator of a permafrost environment. The interpretation of SHD ages from patterned ground surfaces remains challenging, however, owing to their diachronous nature, the potential for a complex history of formation, and the influence of local, non-climatic factors.
机译:使用施密特锤击曝光年龄测年法(SHD)研究了挪威南部中部Jotunheimen的Juvflya沿高度剖面的沿冰点图案化地面(分类的圆形和多边形)。图案化的地面表现出具有R值的分布,并具有platycurtic模式,宽平台期,细尾巴和负偏斜。采样点位于1500和1925 m a.s.l.表示平均R值朝着较高的高度增加的明显的海拔梯度,这被解释为按时间顺序的函数。已建立的Jotunheimen区域SHD校准曲线得出的平均巨石暴露年龄在6910±510至8240±495年前。这些SHD年龄表示图案化地面形成的时间,表示主动砾石冻结的最小年龄和稳定沟中巨石稳定的最大年龄。尽管校准曲线和巨石的年龄分布,图案化地面的全新世早期年龄,全新世热最大值(HTM)期间主要活动的明显停止以及晚全新世活动的持续缺乏等不确定因素都可以澄清现有对大型分类花纹地面的过程动力学和古气候意义的了解,作为永久冻土环境的指标。然而,由于图案化的地表年代性,形成的复杂历史的可能性以及当地非气候因素的影响,从带图案的地表解释SHD年龄仍然具有挑战性。

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