Abstract Middle-to-late Holocene palaeoenvironmental reconstruction from the A294 ice-cave record (Central Pyrenees, northern Spain)
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Middle-to-late Holocene palaeoenvironmental reconstruction from the A294 ice-cave record (Central Pyrenees, northern Spain)

机译:来自A294冰洞纪录(中央比利牛斯,北西班牙)的中期全新世古环境重建

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AbstractPerennial ice deposits in caves represent unique, but underexplored, terrestrial sequences that potentially contain outstanding palaeoclimatic records. Here, we present a pioneer palaeoenvironmental study of an ice deposit preserved in a small sag-type cave (A294) in the Central Pyrenees (northern Iberian Peninsula). The 9.25-m-thick sequence, which is dated from 6100 ± 107 to 1888 ± 64 cal BP, represents the oldest known firn ice record worldwide. The stratigraphy (detrital layers, unconformities, and cross stratification), plant macrofossils, and isotopic signature (similarity between the ice linear distribution,δ2H=7.83δ18O+8.4, and the Global Meteoric Water Line) of the ice point to the diagenesis of snow introduced to the cave by winter snowstorms. Four phases of rapid ice accumulation (6100–5515, 4945–4250, 3810–3155, and 2450–1890 cal BP) are related to wetter and colder winters. Comparison of the isotopic composition (δ18Oand deuterium excess) of the ice with other paleoclimate records show that both source eff
机译:<![cdata [ Abstract 洞穴中的多年生冰沉积代表独特,但潜在的陆地序列,可能包含优秀的古信风。在这里,我们提出了在中央比利牛斯(北伊比利亚半岛)的小凹凸型洞穴(A294)中保存的冰盖的先驱古环境研究。 9.25米厚的序列,其6100±107至1888±64磅BP代表全球最古老的已知FiRN冰录。地层(碎屑层,不整合面,和交叉分层),植物大化石,并且冰线性分布, Δ 2 H = 7.83 Δ 18 o + 8.4 ,以及全球变幻水线)冰点通过冬季暴风雪引入洞穴的积雪成岩作用。快速冰积累的四个阶段(6100-5515,4945-4250,3810-3155和2450-1890 Cal BP)与湿润和较冷的冬季有关。同位素组成的比较( < MML:MSUP> Δ 18 o 和氘多余的冰与其他古气候记录显示,源效果

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