The climate change over the past 1000 years by humification records of a peat core from Meihua Mountain in Fujian Province
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摘要:
全球变暖背景下频发的极端气候事件, 严重影响了经济社会可持续发展。研究过去人类活动背景下的气候变化特征可为预测气候变化趋势、制定应对策略提供历史借鉴。本研究选取福建梅花山国家级自然保护区山间泥炭岩芯(长度238cm)119个沉积物进行腐殖化度分析, 结合粒度和烧失量记录, 重建近千年来福建地区高分辨率气候历史。研究结果显示, 在东亚季风区的低纬亚高山山间盆地, 泥炭沉积物腐殖化度越高, 指示气候越冷干; 腐殖化度越低, 指示气候越暖湿。梅花山泥炭腐殖化度在980~1529A.D.呈现低值(均值8.4%), 指示中世纪暖期较强的东亚季风和暖湿气候; 1529~1926A.D.呈显著高值(均值24.8%), 指示明清小冰期较弱的季风和冷干气候; 1926A.D.以来波动下降(均值22.8%), 对应了现代暖期。梅花山泥炭腐殖化度记录与区域沉积记录显示出对东亚季风的同步响应。研究结果记录了小冰期的第二次和第三次冷期, 分别为1589~1757A.D.和1842~1926A.D.。梅花山泥炭腐殖化度记录的近千年气候变化可能受太阳辐射、热带辐合带和厄尔尼诺/南方涛动等的共同驱动。
Abstract:Climate extremes are increasing induced by global warming, which threaten the sustainability of economic and social development. The study of past climate changes under the background of increasing human activities can provide suggestions for forecast and response of future climate change. In this study, we obtained a peat core(25°20.94'N, 116°48.92'E; altitude 1450m)in a subalpine basin from Meihua Mountain National Nature Reserve in Fujian Province, Southeast China. The length of the core is 238cm and 119 sediment samples of the peat core were used to measure the grain size, loss on ignition and humification to reconstruct the high-resolution climate variations over the past 1000 years in Fujian Province. The results show that higher(lower)content of humification from peat sediments indicates colder and drier(warmer and wetter)climate in the low-latitude subalpine basin of the East Asian summer monsoon area. The low content of peat humification(with the average value of 8.4 %)from 980A.D. to 1529A.D. indicated that the climate was warm and humid with stronger East Asian summer monsoon during the Medieval Warm Period, whereas significantly high content humification(with the average value of 24.8 %)from 1529A.D. to 1926A.D. indicated a cold and dry climate with weaker East Asian summer monsoon during the Little Ice Age of Ming and Qing Dynasties. The humification decreased(with the average value of 22.8 %)with fluctuations since 1926A.D., reflecting the Current Warm Period. The humification records from Meihua Mountain and nearby sedimentary records indicate the synchronous response of regional sedimentary records to the East Asian summer monsoon. Two cold periods were recorded in the peat core during the Little Ice Age: 1589~1757A.D. and 1842~1926A.D., which correspond to the second and third cold periods of the Little Ice Age in China. The climate change recorded by humification from Meihua Mountain over the past 1000 years may be driven by the variation of solar radiation, intertropical convergence zone and El Nino/Southern Oscillation.
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Key words:
- Meihua Mountain in Fujian Province /
- peat /
- humification /
- Little Ice Age /
- climate change
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图 3
MHS1孔沉积年代-深度模式和地层剖面
Figure 3.
The age-depth model and stratigraphic profile of core MHS1
图 4
MHS1孔沉积物的粒度、烧失量和腐殖化度
Figure 4.
The grain size, loss on ignition and humification of sediments from core MHS1
图 5
过去1000 a沉积记录对比
Figure 5.
Comparison of different sedimentary records over the last ca.1000 years.
图 7
MHS1泥炭腐殖化度记录与其他代用指标对比
Figure 7.
Comparison of the records of MHS1 humification and other records over the last ca.1000 years.
表 1
MHS1孔AMS 14C常规年龄及校正年龄
Table 1.
AMS 14C ages and their calibrations for sediment core MHS1
深度(cm) 材料 δ13C(‰) 常规年龄(a B. P.) 校正年龄(cal.a B. P.) 年龄(A. D.) 实验室编号 年龄 误差 2 sigma 概率(%) 中值 45 叶片 -26.2 70 30 44~58 95.4 52 1968 Beta-624349 78 叶片 -12.6 360 30 320~494 95.4 409 1611 Beta-615275 126 炭屑 -24.8 560 30 526~642 95.4 578 1442 Beta-615276 220 小木块 -22.1 1060 30 930~1048 95.4 973 1047 Beta-615277 
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表 2
MHS1孔粒度参数均值和范围
Table 2.
Average value and range of grain size of sediments from core MHS1
阶段 年代(A. D.) 粘土(%) 粉砂(%) 砂(%) 平均粒径(μm) 中值粒径(μm) 分选系数 Ⅰ 980~1036 均值 15.8 52.9 31.4 30.2 28.5 6.0 范围 12.0~20.4 40.1~60.3 23.3~47.8 19.0~57.1 16.3~53.9 5.0~7.8 Ⅱ 1036~1211 均值 23.5 65.9 10.5 12.5 12.8 4.1 范围 18.3~28.5 54.4~73.5 3.5~22.1 8.4~17.8 8.9~19.1 3.3~5.3 Ⅲ 1211~1327 均值 10.4 59.2 30.5 32.4 34.4 3.9 范围 5.9~21.6 44.3~73.2 5.4~43.5 10.7~51.3 10.9~58.0 3.3~4.6 Ⅳ 1327~1594 均值 21.9 63.3 14.8 14.6 14.6 4.2 范围 13.3~31.3 53.4~71.3 3.2~25.3 9.5~21.7 9.2~23.3 3.3~4.9 Ⅴ 1594~2020 均值 20.4 69.2 10.3 14.0 14.2 3.5 范围 7.2~30.5 54.4~75.9 1.2~38.4 7.4~39.5 7.3~42.2 3.0~4.2
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表 3
MHS1孔烧失量和腐殖化度的平均值和范围
Table 3.
Average value and range of loss on ignition and humification of sediments from core MHS1
阶段 年代
(A. D.)烧失量(%) 吸光度(%) 均值 范围 均值 范围 Ⅰ 980~1036 10.39 3.88~14.53 0.29 0~1.55 Ⅱ 1036~1529 28.99 7.13~60.21 9.48 1.80~17.02 Ⅲ 1529~1753 52.23 30.90~68.26 26.96 5.63~53.55 Ⅳ 1753~1926 44.38 35.33~59.87 19.86 13.25~29.19 Ⅴ 1926~2020 39.30 29.09~60.28 22.80 11.94~40.67
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