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Physical growing media characteristics of Sphagnum biomass dominated by Sphagnum fuscum (Schimp.) Klinggr 以褐藻(Sphagnum fuscum)为主的Sphagnum生物量物理生长介质特性Klinggr
IF 1.2 4区 环境科学与生态学 Q4 ENVIRONMENTAL SCIENCES Pub Date : 2018-01-01 DOI: 10.19189/MAP.2017.OMB.278
A. Kämäräinen, A. Simojoki, L. Lindén, K. Jokinen, Niko Silvan
1 Department of Agricultural Sciences, University of Helsinki, Finland 2 Department of Food and Environmental Sciences, University of Helsinki, Finland 3 Natural Resources Institute Finland, Natural Resources and Bioproduction, Helsinki, Finland 4 Natural Resources Institute Finland, Bio-based Business and Industry, Parkano, Finland _______________________________________________________________________________________
1芬兰赫尔辛基大学农业科学系2芬兰赫尔辛基大学食品与环境科学系3芬兰自然资源研究所,自然资源与生物生产,芬兰赫尔辛基4芬兰自然资源研究所,生物基商业与工业,芬兰帕克卡诺_______________________________________________________________________________________
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引用次数: 10
Biodiversity of the Sebangau tropical peat swamp forest, Indonesian Borneo 印尼婆罗洲塞邦高热带泥炭沼泽森林的生物多样性
IF 1.2 4区 环境科学与生态学 Q4 ENVIRONMENTAL SCIENCES Pub Date : 2018-01-01 DOI: 10.19189/MAP.2018.OMB.352
Simon J. Husson, S. Limin, Adul, N. Boyd, J. Brousseau, S. Collier, S. Cheyne, Laura J. d’Arcy, R. Dow, N. Dowds, Marc L. Dragiewicz, D. E. Smith, Iwan, Hendri, Peter R Houlihan, K. Jeffers, Benjamin J. M. Jarrett, I. Kulu, H. Morrogh-Bernard, S. Page, Eric Perlett, A. Purwanto, B. R. Capilla, Salahuddin, Santiano, Stijn J J Schreven, M. Struebig, S. Thornton, C. Tremlett, Z. Yeen, M. Harrison
We thank the Indonesian Ministry of Research and Technology (RISTEK) and UPT LLG CIMTROP UPR for research permissions in the NLPSF. Collection of the species records described here has been made possible through financial support from a large number of sources over the years, among which we are particularly indebted to The Orangutan Project, Arcus Foundation, US Fish & Wildlife Service Great Apes Conservation Fund, the StOLT fund of SaveTheOrangutan and the Orangutan Land Trust, Orangutan Appeal UK, EAZA, Bioparcs Foundation, Orangutan Outreach, Orangutan Conservancy, Taronga Zoo, Riverbanks Zoo, Wallace Global Fund, Ocean Parks Conservation Foundation Hong Kong, Wildlife Conservation Society, Primate Conservation Inc., IFAW, Karen Hanssen Trust, the Rufford Foundation, Point Defiance Zoo and Aquarium, Clouded Leopard Project, Fresno Chafee Zoo, and Panthera and Robertson Foundation (through WildCRU, University of Oxford). A large number of staff, students, volunteers and other visitors from Borneo Nature Foundation and other organisations have contributed to this work, both generally and byWe thank the Indonesian Ministry of Research and Technology (RISTEK) and UPT LLG CIMTROP UPR for research permissions in the NLPSF. Collection of the species records described here has been made possible through financial support from a large number of sources over the years, among which we are particularly indebted to The Orangutan Project, Arcus Foundation, US Fish & Wildlife Service Great Apes Conservation Fund, the StOLT fund of SaveTheOrangutan and the Orangutan Land Trust, Orangutan Appeal UK, EAZA, Bioparcs Foundation, Orangutan Outreach, Orangutan Conservancy, Taronga Zoo, Riverbanks Zoo, Wallace Global Fund, Ocean Parks Conservation Foundation Hong Kong, Wildlife Conservation Society, Primate Conservation Inc., IFAW, Karen Hanssen Trust, the Rufford Foundation, Point Defiance Zoo and Aquarium, Clouded Leopard Project, Fresno Chafee Zoo, and Panthera and Robertson Foundation (through WildCRU, University of Oxford). A large number of staff, students, volunteers and other visitors from Borneo Nature Foundation and other organisations have contributed to this work, both generally and byWe thank the Indonesian Ministry of Research and Technology (RISTEK) and UPT LLG CIMTROP UPR for research permissions in the NLPSF. Collection of the species records described here has been made possible through financial support from a large number of sources over the years, among which we are particularly indebted to The Orangutan Project, Arcus Foundation, US Fish & Wildlife Service Great Apes Conservation Fund, the StOLT fund of SaveTheOrangutan and the Orangutan Land Trust, Orangutan Appeal UK, EAZA, Bioparcs Foundation, Orangutan Outreach, Orangutan Conservancy, Taronga Zoo, Riverbanks Zoo, Wallace Global Fund, Ocean Parks Conservation Foundation Hong Kong, Wildlife Conservation Society, Primate Conservation
我们感谢印度尼西亚研究与技术部(RISTEK)和UPT LLG CIMTROP UPR对NLPSF的研究许可。这里所描述的物种记录的收集是在多年来大量资金的支持下才得以实现的,其中我们特别感谢猩猩项目、Arcus基金会、美国鱼类和野生动物管理局类人猿保护基金、拯救猩猩基金会和猩猩土地信托基金、猩猩呼吁英国、EAZA、Bioparcs基金会、猩猩外展、猩猩保护协会、塔龙加动物园、河岸动物园、华莱士全球基金、香港海洋公园保育基金会、野生动物保育学会、灵长类动物保育公司、IFAW、Karen hansen Trust、ruffford基金会、Point Defiance动物园及水族馆、云豹计划、Fresno Chafee动物园、Panthera and Robertson基金会(透过WildCRU、牛津大学)。来自婆罗洲自然基金会和其他组织的大量工作人员、学生、志愿者和其他访客为这项工作做出了贡献,我们感谢印度尼西亚研究与技术部(RISTEK)和UPT LLG CIMTROP UPR对NLPSF的研究许可。这里所描述的物种记录的收集是在多年来大量资金的支持下才得以实现的,其中我们特别感谢猩猩项目、Arcus基金会、美国鱼类和野生动物管理局类人猿保护基金、拯救猩猩基金会和猩猩土地信托基金、猩猩呼吁英国、EAZA、Bioparcs基金会、猩猩外展、猩猩保护协会、塔龙加动物园、河岸动物园、华莱士全球基金、香港海洋公园保育基金会、野生动物保育学会、灵长类动物保育公司、IFAW、Karen hansen Trust、ruffford基金会、Point Defiance动物园及水族馆、云豹计划、Fresno Chafee动物园、Panthera and Robertson基金会(透过WildCRU、牛津大学)。来自婆罗洲自然基金会和其他组织的大量工作人员、学生、志愿者和其他访客为这项工作做出了贡献,我们感谢印度尼西亚研究与技术部(RISTEK)和UPT LLG CIMTROP UPR对NLPSF的研究许可。这里所描述的物种记录的收集是在多年来大量资金的支持下才得以实现的,其中我们特别感谢猩猩项目、Arcus基金会、美国鱼类和野生动物管理局类人猿保护基金、拯救猩猩基金会和猩猩土地信托基金、猩猩呼吁英国、EAZA、Bioparcs基金会、猩猩外展、猩猩保护协会、塔龙加动物园、河岸动物园、华莱士全球基金、香港海洋公园保育基金会、野生动物保育学会、灵长类动物保育公司、IFAW、Karen hansen Trust、ruffford基金会、Point Defiance动物园及水族馆、云豹计划、Fresno Chafee动物园、Panthera and Robertson基金会(透过WildCRU、牛津大学)。来自婆罗洲自然基金会和其他组织的大量工作人员、学生、志愿者和其他游客都为这项工作做出了贡献,包括提供记录;我们向他们所有人表示诚挚的感谢。
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引用次数: 42
Peat Soils of the Everglades of Florida, USA 美国佛罗里达大沼泽地的泥炭土
IF 1.2 4区 环境科学与生态学 Q4 ENVIRONMENTAL SCIENCES Pub Date : 2017-12-20 DOI: 10.5772/INTECHOPEN.72925
T. Dreschel, S. Hohner, S. Aich, C. Mcvoy
In this chapter, we briefly discuss the development of the Everglades over the past 5 mil - lion years, the modifications made to the Everglades over the past century and a half and the quantification of the changes that have occurred to the peat soils of the Everglades due to natural and anthropogenic causes during this most recent period. Using Geographic Information Systems and historical data sets, we have been able to calculate the origi - nal peat volumes, the remaining peat volumes and thus, the amount lost over the past approximately 150 years. From these volume calculations and peat physical and chemical characterizations by the USEPA over a large area of the Everglades, we have estimated the mass of peat and carbon lost, 900 million metric tons and 300 million metric tons, respectively. The amount of peat lost has implications for hydrological, ecological and landscape restoration and habitat recovery for the Everglades.
在本章中,我们简要地讨论了过去500万年来沼泽地的发展,过去一个半世纪以来对沼泽地的改造,以及最近一段时期内由于自然和人为原因对沼泽地泥炭土发生的变化的量化。利用地理信息系统和历史数据集,我们已经能够计算出原始泥炭体积、剩余泥炭体积以及在过去大约150年中损失的泥炭体积。根据这些体积计算和美国环保署对沼泽地大片地区泥炭的物理和化学特征,我们估计了泥炭和碳损失的质量,分别为9亿吨和3亿吨。泥炭流失的数量对大沼泽地的水文、生态和景观恢复以及栖息地恢复都有影响。
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引用次数: 1
Refining pedotransfer functions for estimating peat bulk density 用于估算泥炭堆积密度的精细土壤传递函数
IF 1.2 4区 环境科学与生态学 Q4 ENVIRONMENTAL SCIENCES Pub Date : 2017-11-25 DOI: 10.19189/MAP.2017.OMB.281
S. Chapman, J. Farmer, A. Main, J. D. Smith
Several previous studies have demonstrated the close relationship between peat dry bulk density and gravimetric moisture content. However, the basis for including peat ash (mineral) content or variation in the specific gravity of peat solids has not been covered. Here we present a theoretical basis for estimating peat dry bulk density for saturated peats from values of moisture content and, where available, ash content. The theory is evaluated using datasets obtained from Scotland, Ireland and Indonesia where both dry bulk density and peat moisture content have been measured. Deviations from theory are discussed in terms of peat gas volume and possible errors in the determination of peat dry bulk density.
先前的几项研究已经证明了泥炭干容重和重量含水量之间的密切关系。然而,包括泥炭灰(矿物)含量或泥炭固体比重变化的依据尚未涵盖。在这里,我们提供了一个理论基础,用于根据水分含量和灰分含量(如有)来估计饱和泥炭的泥炭干容重。该理论是使用从苏格兰、爱尔兰和印度尼西亚获得的数据集进行评估的,这些国家已经测量了干容重和泥炭含水量。讨论了泥炭气体体积与理论的偏差以及泥炭干体积密度测定中可能出现的误差。
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引用次数: 1
The peatland map of Europe 欧洲泥炭地地图
IF 1.2 4区 环境科学与生态学 Q4 ENVIRONMENTAL SCIENCES Pub Date : 2017-11-10 DOI: 10.19189/MAP.2016.OMB.264
F. Tanneberger, C. Tegetmeyer, S. Busse, A. Barthelmes, S. Shumka, A. Mariné, K. Jenderedjian, G. Steiner, F. Essl, J. Etzold, C. Mendes, A. Kozulin, P. Frankard, D. Milanovic, A. Ganeva, I. Apostolova, A. Alegro, P. Delipetrou, J. Navrátilová, M. Risager, A. Leivits, A. Fosaa, S. Tuominen, F. Muller, T. Bakuradze, M. Sommer, K. Christanis, E. Szurdoki, H. Óskarsson, S. Brink, J. Connolly, L. Bragazza, G. Martinelli, O. Aleksans, A. Priede, D. Sungaila, L. Melovski, T. Belous, D. Saveljić, F. D. Vries, A. Moen, W. Dembek, J. Mateus, J. Hanganu, A. Sirin, A. Markina, M. Napreenko, P. Lazarević, V. Stanová, P. Skoberne, P. H. Pérez, X. P. Pombal, J. Lonnstad, M. Küchler, C. Galley, S. Kırca, O. Mykytiuk, R. Lindsay, H. Joosten
Based on the ‘European Mires Book’ of the International Mire Conservation Group (IMCG), this article provides a composite map of national datasets as the first comprehensive peatland map for the whole of Europe. We also present estimates of the extent of peatlands and mires in each European country individually and for the entire continent. A minimum peat thickness criterion has not been strictly applied, to allow for (often historically determined) country-specific definitions. Our ‘peatland’ concept includes all ‘mires’, which are peatlands where peat is being formed. The map was constructed by merging national datasets in GIS while maintaining the mapping scales of the original input data. This ‘bottom-up’ approach indicates that the overall area of peatland in Europe is 593,727 km². Mires were found to cover more than 320,000 km² (around 54 % of the total peatland area). If shallow-peat lands (< 30 cm peat) in European Russia are also taken into account, the total peatland area in Europe is more than 1,000,000 km2, which is almost 10 % of the total surface area. Composite inventories of national peatland information, as presented here for Europe, may serve to identify gaps and priority areas for field survey, and help to cross-check and calibrate remote sensing based mapping approaches.
基于国际泥炭保护组织(IMCG)的“欧洲泥炭书”,本文提供了一个国家数据集的合成地图,作为整个欧洲的第一个综合泥炭地地图。我们还对每个欧洲国家单独和整个欧洲大陆的泥炭地和泥潭的范围进行了估计。最低泥炭厚度标准尚未严格适用,以允许(通常是历史上确定的)具体国家的定义。我们的“泥炭地”概念包括所有的“泥炭地”,泥炭地是泥炭形成的地方。该地图是在保持原始输入数据的比例尺的基础上,在GIS中合并国家数据集构建的。这种“自下而上”的方法表明,欧洲泥炭地的总面积为593,727平方公里。泥炭地覆盖面积超过32万平方公里(约占泥炭地总面积的54%)。如果将俄罗斯欧洲部分的浅泥炭地(< 30厘米泥炭地)也计算在内,欧洲的泥炭地总面积超过1,000,000平方公里,几乎占总表面积的10%。这里为欧洲提出的国家泥炭地资料综合清单可用于查明实地调查的差距和优先领域,并有助于交叉核对和校准基于遥感的制图方法。
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引用次数: 154
Carbon dioxide and methane fluxes in grazed and undisturbed mountain peatlands in the Ecuadorian Andes 厄瓜多尔安第斯山脉放牧和未受干扰的山地泥炭地的二氧化碳和甲烷通量
IF 1.2 4区 环境科学与生态学 Q4 ENVIRONMENTAL SCIENCES Pub Date : 2017-10-31 DOI: 10.19189/MAP.2017.OMB.277
M. Sánchez, R. Chimner, J. Hribljan, E. Lilleskov, E. Suárez
Peatlands are widespread throughout the tropical Andean paramo. Despite the large carbon stocks in these ecosystems, carbon dioxide (CO2) and methane (CH4) flux data are lacking. In addition, cattle grazing is widespread in the paramo and could alter gas fluxes. Therefore, our objectives were to measure CO2 and CH4 fluxes with the static chamber technique in an undisturbed and in an intensively cattle grazed peatland in the mountains of Ecuador. We found that hummocks in the undisturbed site had higher net ecosystem exchange (NEE), gross primary production (GPP), ecosystem respiration (ER), and CH4 fluxes, compared to lawns. In contrast, microtopography at the grazed site did not predict CO2 fluxes, whereas vegetation cover was correlated for all three metrics (NEE, ER, and GPP). At low vegetation cover, NEE was positive (losing carbon). CH4 emissions in the undisturbed site were low (8.1 mg CH4 m-2 d-1). In contrast, CH4 emissions at the grazed site were much greater (132.3 mg CH4 m-2 d-1). This is probably attributable to trampling and nutrient inputs from cattle. In summary, the two peatlands differed greatly in CO2 and CH4 exchange rates, which could be due to the variation in climate and hydrology, or alternatively to intensive grazing by cattle.
泥炭地分布在整个安第斯热带地区。尽管这些生态系统中有大量的碳储量,但缺乏二氧化碳(CO2)和甲烷(CH4)通量数据。此外,放牧在帕拉莫地区很普遍,可能会改变气体流量。因此,我们的目标是在厄瓜多尔山区未受干扰和密集放牧的泥炭地中,使用静态室技术测量CO2和CH4通量。我们发现,与草坪相比,未扰动场地的鹰嘴豆泥具有更高的净生态系统交换(NEE)、初级生产总值(GPP)、生态系统呼吸(ER)和CH4通量。相反,放牧地的微观地形不能预测CO2通量,而植被覆盖率与所有三个指标(NEE、ER和GPP)相关。在植被覆盖率较低的情况下,NEE为正(损失碳)。未扰动场地的CH4排放量较低(8.1 mg CH4 m-2 d-1)。相比之下,放牧地点的CH4排放量要大得多(132.3 mg CH4 m-2 d-1)。这可能是由于牛的践踏和营养投入造成的。总之,这两个泥炭地的二氧化碳和甲烷交换率差异很大,这可能是由于气候和水文的变化,也可能是由于牛的密集放牧。
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引用次数: 19
Drivers of peat accumulation rate in a raised bog: impact of drainage, climate, and local vegetation composition 抬高沼泽泥炭积累速率的驱动因素:排水、气候和当地植被组成的影响
IF 1.2 4区 环境科学与生态学 Q4 ENVIRONMENTAL SCIENCES Pub Date : 2017-03-21 DOI: 10.19189/MAP.2016.OMB.262
N. Stivrins, I. Ozoloa, M. Gałka, Eliza Kuske, T. Alliksaar, T. J. Andersen, M. Lamentowicz, S. Wulf, T. Reitalu
1Department of Geosciences and Geography, University of Helsinki, Helsinki, Finland 2Institute of Geology, Tallinn University of Technology, Tallinn, Estonia 3Institute of Soil and Plant Sciences, Faculty of Agriculture, Latvia University of Agriculture, Jelgava, Latvia 4Lake and Peatland Research Centre, Alojas District, Puikule, Latvia 5Department of Biogeography and Palaeoecology, Adam Mickiewicz University, Poznań, Poland 6Faculty of Geography and Earth Sciences, University of Latvia, Riga, Latvia 7Department of Geosciences and Natural Resource Management, University of Copenhagen, Copenhagen, Denmark 8Laboratory of Wetlands Ecology and Monitoring, Adam Mickiewicz University, Poznań, Poland 9Senckenberg Research Institute & Natural History Museum, BIK-F, TSP6 Evolution and Climate, Frankfurt, Germany 10Climate Dynamics and Landscape Evolution, GFZ German Research Centre for Geosciences, Potsdam, Germany 11Institute of Earth Sciences, Heidelberg University, Heidelberg, Germany _______________________________________________________________________________________
1芬兰赫尔辛基赫尔辛基大学地球科学与地理系2爱沙尼亚塔林塔林科技大学地质学院3拉脱维亚杰尔加瓦拉脱维亚农业大学农业学院土壤与植物科学学院4拉脱维亚普伊库勒阿洛哈斯区拉克和泥炭地研究中心5生物地理和古生态学系,波兰波兹南Adam Mickiewicz大学6拉脱维亚里加拉脱维亚大学地理与地球科学学院7丹麦哥本哈根哥本哈根大学地球科学与自然资源管理系8波兰波兹南Adam Mickewicz大学湿地生态与监测实验室9森肯贝格研究所和自然历史博物馆,TSP6进化与气候,德国法兰克福10气候动力学与景观进化,GFZ德国地球科学研究中心,德国波茨坦11海德堡大学地球科学研究所,德国海德堡_______________________________________________________________________________________
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引用次数: 21
Towards ecosystem-based restoration of peatland biodiversity 基于生态系统的泥炭地生物多样性恢复
IF 1.2 4区 环境科学与生态学 Q4 ENVIRONMENTAL SCIENCES Pub Date : 2017-01-18 DOI: 10.19189/MAP.2013.OMB.150
T. Minayeva, O. Bragg, A. Sirin
Natural peatlands support rich biological diversity at the genetic, species, ecosystem and landscape levels. However, because the character of this diversity differs from that of other ecosystem types, the value of peatlands for biodiversity has often been overlooked. Fundamentally, this arises because peatland ecosystems direct part of the energy captured by primary production into long-term storage within a peat layer, and thus establish a structural and functional basis for biodiversity maintenance that is not found elsewhere. This article examines the far-reaching implications for the assessment of peatland biodiversity as well as for the drivers, methods and targets of peatland conservation and restoration initiatives. It becomes clear that a robust framework for the management and restoration of peatland biodiversity must be founded in structuralfunctional ecosystem analysis, and such a framework is developed. The authors draw on a broad base of historical and contemporary literature and experience, including important Russian contributions that have previously had little international exposure.
天然泥炭地在遗传、物种、生态系统和景观层面支持丰富的生物多样性。然而,由于这种多样性的特征不同于其他生态系统类型,泥炭地对生物多样性的价值往往被忽视。从根本上说,这是因为泥炭地生态系统将初级生产所捕获的部分能量直接转化为泥炭层内的长期储存,从而为维持生物多样性建立了其他地方所没有的结构和功能基础。本文探讨了泥炭地生物多样性评估以及泥炭地保护和恢复举措的驱动因素、方法和目标的深远影响。在结构功能生态系统分析中,必须建立一个强有力的泥炭地生物多样性管理和恢复框架,并建立了这样一个框架。作者借鉴了广泛的历史和当代文献和经验,包括以前很少在国际上曝光的重要的俄罗斯贡献。
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引用次数: 75
Holocene elemental, lead isotope and charcoal record from peat in Southern Poland 波兰南部泥炭的全新世元素、铅同位素和木炭记录
IF 1.2 4区 环境科学与生态学 Q4 ENVIRONMENTAL SCIENCES Pub Date : 2017-01-01 DOI: 10.19189/MAP.2016.OMB.257
K. Tudyka, A. Pazdur, F. Vleeschouwer, M. Lityńska-Zając, L. Chróst, N. Fagel
1 Department of Radioisotopes, Institute of Physics, Silesian University of Technology, Gliwice, Poland 2 University of Toulouse (INP, UPS) and CNRS, EcoLab, ENSAT, Castanet Tolosan, France 3 Institute of Archaeology and Ethnology, Polish Academy of Sciences, Kraków, Poland 4 Laboratory for Ecological Research, Measurement and Expertise, Gliwice, Poland 5 UR AGEs, Department of Geology, University of Liège (Sart Tilman), Belgium _______________________________________________________________________________________
1西里西亚理工大学物理研究所放射性同位素系,格列维采,波兰2图卢兹大学(INP, UPS)和CNRS, EcoLab, ENSAT, Castanet Tolosan,法国3波兰科学院考古和民族学研究所,Kraków,波兰4生态研究,测量和专业知识实验室,波兰格列维采,波兰5 urages,格列维采大学地质系(Sart Tilman),波兰比利时 _______________________________________________________________________________________
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引用次数: 8
Quality loss of Swiss bog vegetation - the key importance of the margins 瑞士沼泽植被的质量损失——边缘的关键重要性
IF 1.2 4区 环境科学与生态学 Q4 ENVIRONMENTAL SCIENCES Pub Date : 2017-01-01 DOI: 10.19189/MAP.2016.OMB.237
E. Feldmeyer-Christe, M. Küchler
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引用次数: 2
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Mires and Peat
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