Holocene Stable Isotope (S13C and S 15 N) record of peatland development in Stavs?kra, southern Sweden
文献类型：期刊论文
| 作者 | Das, Supriyo Kumar4; Ekblad, Alf2; Stojanovic, Ksenija3; Mikusinska, Anna2; Gaillard, Marie-Jose1; Mitrovic, Danica5,7; Cui, Qiao-Yu1,6 |
| 刊名 | CATENA
 |
| 出版日期 | 2024-12-01 |
| 卷号 | 247页码:10 |
| 关键词 | Stable isotopes Carbon Nitrogen Peat Holocene Sweden |
| ISSN号 | 0341-8162 |
| DOI | 10.1016/j.catena.2024.108510 |
| 产权排序 | 6 |
| 英文摘要 | Understanding the environmental and climate influence on the Holocene stable isotope record in peat is essential for applying the proxies in the paleoenvironmental reconstruction of lake and bog ecosystems. Here, we report total organic carbon (TOC), TOC to total nitrogen (N) ratio (C/N), and stable isotope ratios of organic carbon (S13C) and nitrogen (S15N) of bulk sediment and peat organic matter (OM) from a radiocarbon-dated core collected from Stavs & aring;kra bog in southern Sweden. Changes in the TOC, C/N, S13C and S15N between 12 ka and 10.4 ka BP represent shifts in the OM source from aquatic primary producers to terrestrial swamp vegetation and pinpoint the transition of a highly productive water body into a reed swamp. The variation in S13C values and increase in peat accumulation rate (AR) from 10.8 ka BP imply a rapid transition of the aquatic body into a peatforming swamp and a shift from aquatic to atmospheric CO2 as the source of carbon (C) to the vegetation at the site. A sharp drop in N and S15N in the reed swamp peat may indicate fixed-N in the soil as the source of N to the growing vegetation. Heavier S13C and higher C/N ratio at the bottom of wood carr peat may reflect fire events. The rapid increase in peat AR between 7 ka and 6.5 ka BP suggests increased peat deposition under warmer and drier conditions. Lighter S15N and S13C, lower N, and TOC concentrations between 1.1 ka and 0.8 ka BP likely suggest warmer conditions related to the 'Medieval Climate Anomaly'. The research demonstrates the successful application of stable C and N isotope ratios of bulk peat in palaeoenvironment and palaeoecological interpretations. |
| WOS关键词 | LAKE-LEVEL FLUCTUATIONS ; ORGANIC-MATTER ; FIRE HISTORY ; C-N ; NITROGEN ISOTOPES ; CARBON ISOTOPES ; DEPTH PROFILES ; EARLY-STAGE ; BOG PLANTS ; CLIMATE |
| 资助项目 | STINT[IB 2012/4505] ; Faculty of Health and Life Sciences of Linnaeus University, Kalmar, Sweden |
| WOS研究方向 | Geology ; Agriculture ; Water Resources |
| 语种 | 英语 |
| WOS记录号 | WOS:001355257300001 |
| 出版者 | ELSEVIER |
| 资助机构 | STINT ; Faculty of Health and Life Sciences of Linnaeus University, Kalmar, Sweden |
| 源URL | [http://ir.igsnrr.ac.cn/handle/311030/211151]  |
| 专题 | 陆地表层格局与模拟院重点实验室_外文论文 |
| 通讯作者 | Das, Supriyo Kumar |
| 作者单位 | 1.Linnaeus Univ, Dept Biol & Environm Sci, SE-39182 Kalmar, Sweden 2.Orebro Univ, Sch Sci & Technol, SE-70182 Orebro, Sweden 3.Univ Belgrade, Fac Chem, Studentski Trg 12-16, Belgrade 11000, Serbia 4.Presidency Univ, Dept Geol, Coll St 86-1, Kolkata 700073, India 5.Singidunum Univ, Environm & Sustainable Dev, Danijelova 32, Belgrade 11010, Serbia 6.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Land Surface Pattern & Simulat, Beijing 100101, Peoples R China 7.Univ Belgrade, Innovat Ctr, Fac Chem, Studentski Trg 12-16, Belgrade 11000, Serbia |
| 推荐引用方式 GB/T 7714 | Das, Supriyo Kumar,Ekblad, Alf,Stojanovic, Ksenija,et al. Holocene Stable Isotope (S13C and S 15 N) record of peatland development in Stavs?kra, southern Sweden[J]. CATENA,2024,247:10. |
| APA | Das, Supriyo Kumar.,Ekblad, Alf.,Stojanovic, Ksenija.,Mikusinska, Anna.,Gaillard, Marie-Jose.,...&Cui, Qiao-Yu.(2024).Holocene Stable Isotope (S13C and S 15 N) record of peatland development in Stavs?kra, southern Sweden.CATENA,247,10. |
| MLA | Das, Supriyo Kumar,et al."Holocene Stable Isotope (S13C and S 15 N) record of peatland development in Stavs?kra, southern Sweden".CATENA 247(2024):10. |
入库方式： OAI收割
来源：地理科学与资源研究所
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