A multi-proxy record of Holocene environmental change, peatland development and carbon accumulation from Staroselsky Moch peatland, Russia
A multi-proxy record of Holocene environmental change, peatland development and carbon accumulation from Staroselsky Moch peatland, Russia
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俄罗斯斯塔罗塞尔斯基莫赫泥炭地全新世环境变化、泥炭地发育和碳积累的多代理记录
DOI：
10.1177/0959683615608692
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发表时间：
2016
期刊：
影响因子：
--
通讯作者：
Y. Mazei
中科院分区：
文献类型：
--
作者：
R. Payne;E. Malysheva;A. Tsyganov;T. Pampura;E. Novenko;E. Volkova;K. Babeshko;Y. Mazei
尽管俄罗斯的泥炭地面积很大，但它是古环境变化数据的一个未充分利用的来源。我们通过对有遗嘱变形虫、泥炭物理特性、植物大化石和花粉的分析，研究了俄罗斯欧洲部分特维尔地区的暗营养泥炭地 Staroselsky Moch 的全新世历史。泥炭地在全新世早期经历了经典的水力演替过程，矿物输入量急剧下降至 6200 卡。随后，大约 5500cal 的温度从沼泽植被突然转变为沼泽植被。公元前。在全新世，泥炭地的平均表观碳积累率为 21.5 g C m−2 yr−1，这表明俄罗斯欧洲部分泥炭地的碳积累率接近全球平均水平，与暗示碳净损失的短序列涡流协方差数据形成鲜明对比。有遗嘱阿米巴记录显示出相当大的变异性，这可能是由气候驱动的，但这些变化并没有在大型化石或花粉数据中得到很好的复制。我们初步推断（1）全新世早期变暖阶段在 7200cal 左右开始。 BC，（2）干燥泥炭地表面条件c． 3700–3900 卡路里。 BC，（3）从 c 转向更潮湿的条件。 3900 卡路里。 BC，和（4）来自c的干燥条件。 400 卡路里。公元前以后。该地区更稳健和更精确的水文气候重建将需要开发区域传递函数以及在核心和站点之间复制结果。
Despite their huge extent, the peatlands of Russia are an under-exploited source of data on palaeoenvironmental change. We investigated the Holocene history of Staroselsky Moch, an ombrotrophic peatland in the Tver Region of European Russia by analysis of testate amoebae, peat physical properties, plant macrofossils and pollen. The peatland developed through a classic hydroseral succession in the early Holocene with a sharp decline in mineral input to 6200 cal. BC followed by an abrupt transition from fen to bog vegetation around 5500 cal. BC. Through the Holocene, the peatland has accumulated carbon at a mean apparent rate of 21.5 g C m−2 yr−1 suggesting that carbon accumulation rates in peatlands of European Russia lie close to the global average, and contrasting with a short sequence of eddy-covariance data which implies a net loss of carbon. The testate amoeba record shows considerable variability which may be driven by climate, but changes are not well replicated in the macrofossil or pollen data. We tentatively infer (1) a phase of early Holocene warming commencing around 7200 cal. BC, (2) dry peatland surface conditions c. 3700–3900 cal. BC, (3) a shift to wetter conditions from c. 3900 cal. BC, and (4) drier conditions from c. 400 cal. BC onwards. More robust and precise hydroclimatic reconstructions for this region will require the development of a regional transfer function and the replication of results between cores and sites.
影响因子：
2.4
作者：
Loisel, Julie;Yu, Zicheng;Zhou, Weijian
通讯作者：
Zhou, Weijian