60.泥炭沼泽Vodniza，里拉山脉（保加利亚）

IF 0.9 4区生物学 Q4 PLANT SCIENCES

Grana Pub Date : 2022-05-05 DOI:10.1080/00173134.2022.2052954

S. Tonkov, O. Heiri, A. Lotter

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引用次数: 0

摘要

泥炭沼泽Vodniza(北纬42°08 ' 12.34 "，东经23°25 ' 24.48 ";海拔2113米[a.s.l.])，原湖，位于里拉山脉中部靠近木材线的高山植被带。该植被带以针叶树(云杉、松)为主。场地呈细长形状，长约90米，宽约40米，形成于一个东北坡陡峭的岩石洼地，周围是一群群的mugo Turra, Pinus peuce Griseb。云杉(Picea abies)h .岩溶。、西洋松和西伯利亚刺柏。沼泽表面长满了斑点的Sphagnum spp.， Carex nigra (L.)。Reichard, Carex rostrata Stokes, Deschampsia cespitosa (L.)测定。高山参，桔梗，桔梗。，锦葵，Caltha laeta Schott, Nyman et Kotschy，欧花莲，锦葵。， Geum bulgaricum Pancǐc， * Silene roemeri Friv。白藜芦醇;， Bartsia alpina L, Rumex alpinus L, Bistorta vivipara (L.)德拉布尔，大钟，星期五。龙胆车前草;三胸精(野生)哈耶克等。一条小溪穿过泥炭沼泽，流入沃迪尼扎河(Tonkov et al. 2018)。海拔1000米以上为山地气候，海拔1800 ~ 1900米，1月平均气温- 6℃，8月平均气温11.4℃。年最高降水量在年均1300-2400米达到2000毫米，其中大部分为雪(Velev 2002)。沉积物的描述

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60. Peat bog Vodniza, Rila Mountains (Bulgaria)

Site details The peat bog Vodniza (42° 08′ 12.34′′ N, 23° 25′ 24.48′′ E; 2113 m above sea level [a.s.l.]), a former lake, is located in the upper montane vegetation zone of the central part of the Rila Mountains near the timber-line. This vegetation zone is dominated by conifers (Picea, Pinus). The site has an elongated shape, c. 90 m long and 40 m wide, formed in a depression with a steep and rocky northeast slope, surrounded by groups of Pinus mugo Turra, Pinus peuce Griseb., Picea abies (L.) H. Karst., Pinus sylvestris L. and Juniperus sibirica Burgsd. The bog surface is overgrown by spots of Sphagnum spp., Carex nigra (L.) Reichard, Carex rostrata Stokes, Deschampsia cespitosa (L.) P. Beauv., Phleum alpinum L., Eriophorum angustifolium Honck., Eriophorum latifolium Hoppe, Caltha laeta Schott, Nyman et Kotschy, Trollius europaeus L., Geum coccineum Sm., Geum bulgaricum Pancǐc,́ Silene roemeri Friv., Veratrum lobelianum Bernh., Bartsia alpina L., Rumex alpinus L., Bistorta vivipara (L.) Delarbre, Campanula sparsa Friv., Plantago gentianoides Sm., Senecio nemorensis L., Tripleurospermum caucasicum (Willd.) Hayek, etc. A small brook passes through the peat bog and drains into the Vodniza River (Tonkov et al. 2018). The climate above 1000 m is montane and at an elevation of 1800 to 1900 m a.s.l. the mean January temperature is −6 °C and the mean August temperature 11.4 °C. The highest annual precipitation reaches 2000 mm at 1300–2400 m a.s.l., much of it as snow (Velev 2002). Sediment description

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来源期刊

Grana 生物-植物科学

CiteScore

2.10

自引率

11.10%

发文量

审稿时长

>12 weeks

期刊介绍： Grana is an international journal of palynology and aerobiology. It is published under the auspices of the Scandinavian Palynological Collegium (CPS) in affiliation with the International Association for Aerobiology (IAA). Grana publishes original papers, mainly on ontogony (morphology, and ultrastructure of pollen grains and spores of Eucaryota and their importance for plant taxonomy, ecology, phytogeography, paleobotany, etc.) and aerobiology. All submitted manuscripts are subject to initial appraisal by the Editors, and, if found suitable for further consideration, to peer review by independent, anonymous expert referees. All peer review is single blind and submission is online via ScholarOne Manuscripts.