DOCSLIB.ORG

Natural and Human-Transformed Vegetation and Landscape Reflected by Modern Pollen Data in the Boreonemoral Zone of Northeastern Europe

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Natural and Human-Transformed Vegetation and Landscape Reflected by Modern Pollen Data in the Boreonemoral Zone of Northeastern Europe Article Natural and Human-Transformed Vegetation and Landscape Reflected by Modern Pollen Data in the Boreonemoral Zone of Northeastern Europe Normunds Stivrins 1,2,3,* , Agrita Briede 1, Dace Steinberga 4, Nauris Jasiunas 1, Jurijs Jeskins 4, Laimdota Kalnina 1,3, Alekss Maksims 4, Zigmars Rendenieks 1 and Liva Trasune 1,5 1 Department of Geography, University of Latvia, Jelgavas iela 1, LV-1004 Riga, Latvia; [email protected] (A.B.); [email protected] (N.J.); [email protected] (L.K.); [email protected] (Z.R.); [email protected] (L.T.) 2 Department of Geology, Tallinn University of Technology, Ehitajate tee 5, EE-19086 Tallinn, Estonia 3 Lake and Peatland Research Centre, LV-4063 Aloja, Latvia 4 Department of Geology, University of Latvia, Jelgavas iela 1, LV-1004 Riga, Latvia; [email protected] (D.S.); [email protected] (J.J.); [email protected] (A.M.) 5 Department of Geosciences and Geography, University of Helsinki, P.O. Box 64, FI-00014 Helsinki, Finland * Correspondence: [email protected] Abstract: Modern pollen composition obtained from waterbody surface sediment represents sur- rounding vegetation and landscape features. A lack of detailed information on modern pollen from Latvia potentially limits the strength of various pollen-based reconstructions (vegetation composition, climate, landscape, human impact) for this territory. The aim of this study is to compare how modern pollen from natural and human-made waterbodies reflects the actual vegetation composition and landscape characteristics. Modern pollen analyses from surface sediment samples of 36 waterbodies Citation: Stivrins, N.; Briede, A.; from Latvia alongside oceanic-continental, lowland-upland, urban-rural and forested-agricultural Steinberga, D.; Jasiunas, N.; Jeskins, J.; Kalnina, L.; Maksims, A.; Rendenieks, gradients have been studied. In addition, we considered the dominant Quaternary sediment, soil Z.; Trasune, L. Natural and type and land use around the studied waterbodies in buffer zones with widths of one and four km. Human-Transformed Vegetation and The information on climate for the last 30 years from the closest meteorological station for each Landscape Reflected by Modern study site was obtained. Data were analyzed using Pearson correlation and principal component Pollen Data in the Boreonemoral analysis. Results show that relative pollen values from surface sediment of waterbodies reflect Zone of Northeastern Europe. Forests dominant vegetation type and land use. Modern forest biomass had a positive correlation with pollen 2021, 12, 1166. https://doi.org/ accumulation rate, indicating the potential use of pollen-based forest biomass reconstructions for the 10.3390/f12091166 boreonemoral zone after additional research and calibration. Received: 20 July 2021 Keywords: forest; agriculture; natural; urban; lake; pond; Latvia; CORINE Accepted: 25 August 2021 Published: 28 August 2021 Publisher’s Note: MDPI stays neutral 1. Introduction with regard to jurisdictional claims in published maps and institutional affil- Pollen is one of the most abundant microfossils (sub-fossils) preserved in sediment iations. archives, whose sedimentary assemblages are related to regional and local vegetation [1,2]. Whilst fossil pollen can be found in lake sediments extending back for thousands of years, modern pollen surface samples are a component of that fossil record found in the last decades. Modern pollen samples from lake surface sediment reflect differences in vegetation in a similar way to moss pollsters, pollen traps, and might be combined for Copyright: © 2021 by the authors. Licensee MDPI, Basel, Switzerland. vegetation or climate calibration purposes [3]. This article is an open access article In a time when the modeling approach is significantly expanding, the production distributed under the terms and of raw data is less attractive to new and established researchers because it is time- and conditions of the Creative Commons labor-consuming. Nevertheless, modeling of climate, environmental change, forest biomass Attribution (CC BY) license (https:// reconstructions or distribution of biota, vegetation functionality and phylogenetic diversity creativecommons.org/licenses/by/ require input data and validation [4–9]. Although limited in spatial coverage and affected 4.0/). by uncertainties [10], proxy records are used in model-data comparisons and quantitative Forests 2021, 12, 1166. https://doi.org/10.3390/f12091166 https://www.mdpi.com/journal/forests Forests 2021, 12, x FOR PEER REVIEW 2 of 15 Forests 2021, 12, 1166 2 of 15 require input data and validation [4–9]. Although limited in spatial coverage and affected by uncertainties [10], proxy records are used in model-data comparisons and quantitative synthesessyntheses [ 11[11,12].,12]. ForFor example,example, climateclimate modelsmodels areare commonly commonly validatedvalidated againstagainst proxy-proxy- basedbased (e.g., (e.g., pollen) pollen) reconstructions. reconstructions. These These models models should should be ablebe able to reproduce to reproduce past climatepast cli- andmate vegetation and vegetation change change to be useful to be inuseful future in projectionsfuture projections (e.g., [13 (e.g.,]). To [13]). improve To improve our ability our toability reconstruct to reconstruct environments environments and climate, and modernclimate, proxymodern calibration proxy calibration studies along studies climatic along andclimatic ecological and ecological gradients gradients are needed. are Modernneeded. pollenModern surface pollen samplessurface samples currently currently have a lowhave spatial a low resolutionspatial resolution in Latvia, in i.e.,Latvia, 10 samplesi.e., 10 samples [14], therefore [14], therefore lacking lacking the full the potential full po- estimatedtential estimated current, current, past and past possible and possible future natural future andnatural anthropogenic and anthropogenic processes. processes. TheThe aim aim of of this this study study is is to to compare compare how how modern modern pollen pollen from from natural natural and and human- human- mademade waterbodies waterbodies in in Latvia, Latvia, northeastern northeastern Europe Europe reflect reflect actual actual vegetation vegetation composition composition andand landscape landscape characteristics. characteristics. ForFor thethe firstfirst timetime inin Latvia, Latvia, modern modern pollenpollen fromfrom 36 36 water- water- bodybody sediment sediment surfaces surfaces were were analyzed analyzed and and compared compared with with local local vegetation vegetation composition, composition, biomass,biomass, dominant dominant Quaternary Quaternary sediment sediment type type and and climate. climate. 2.2. Materials Materials and and Methods Methods 2.1.2.1. Study Study Sites Sites ◦ ◦ TheThe study study sites sites are are situated situated 55–58 55–58°N N and and 20–28 20–28°E E in in Latvia, Latvia, northeastern northeastern Europe Europe (Figure(Figure1 ;1; Table Table2) in1) in the the hemiboreal hemiboreal forest forest zone, zone, which which is characterizedis characterized by by a mixturea mixture of of coniferousconiferous and and deciduous deciduous tree tree species, species, such such as as the the Norway Norway spruce spruce ( Picea(Picea abies abies),), Scots Scots pine pine (Pinus(Pinus sylvestris sylvestris),), birch birch (Betula (Betulaspp.), spp.), alder alder ( Alnus(Alnus glutinosa glutinosa, Alnus, Alnus incana incana),), wych wych elm elm ( Ulmus(Ulmus glabraglabra),), European European ash ash ( Fraxinus(Fraxinus excelsior excelsior),), small-lived small-lived lime lime ( Tilia(Tilia cordata cordata)) and and pedunculate pedunculate oakoak ( Quercus(Quercus robur robur).). FigureFigure 1. 1.Study Study area area in in Europe Europe ( A(A)) and and the the location location of of waterbodies waterbodies in in Latvia Latvia used used in in current current article article (B): 1—Lake Liepājas, 2—Lake Durbes, 3—Dam Alsungas, 4—Lake Ķikuru, 5—Lake Pinku, 6— (B): 1—Lake Liepajas,¯ 2—Lake Durbes, 3—Dam Alsungas, 4—Lake K, ikuru, 5—Lake Pinku, 6— Pond Cūku, 7—Lake Usmas, 8—Lake Sūnezers, 9—Lake Lielais Pēterezers, 10—Lake Rūmiķis, 11— Pond Cuku,¯ 7—Lake Usmas, 8—Lake Sunezers,¯ 9—Lake Lielais Peterezers,¯ 10—Lake Rumi¯ k, is, Lake Vēžezers, 12—Lake Saldus, 13—Dam Vaides, 14—Lake Talsu, 15—Lake Sasmakas, 16—Lake 11—Lake Vežezers,¯ 12—Lake Saldus, 13—Dam Vaides, 14—Lake Talsu, 15—Lake Sasmakas, 16— Sesavas, 17—Lake Lielais Vipēdes, 18—Lake Vaskaris, 19—Lake Velnezers, 20—Lake Sekšu, 21— Lake Sesavas, 17—Lake Lielais Vipedes,¯ 18—Lake Vaskaris, 19—Lake Velnezers, 20—Lake Sekšu, Lake Mazais Baltezers, 22—Lake Lilastes, 23—Lake Āraišu, 24—Lake Trikātas, 25—Lake Bricu, 26— ¯ 21—LakePond Esplan Mazaisādes, Baltezers, 27—Lake 22—Lake Gubiščes, Lilastes, 28—Lake 23—Lake MazaisAraišu, Stropu, 24—Lake 29—Lake Trik Lielaisatas,¯ Stropu, 25—Lake 30—Lake Bricu, 26—PondGluhoje, 31—Lake Esplanades,¯ Lielais 27—Lake Svētiņ Gubišˇces,28—Lakeu, 32—Lake Čertoks, Mazais 33—Lake Stropu, Puderova 29—Lakes, 34—Lake Lielais Stropu,Zosnas, 30— 35— ˇ LakeLake Gluhoje, Dagdas, 31—Lake36—Pond Lielais Dagdas. Sv etiRoman¯ n, u, 32—Lake numbersCertoks, indicate 33—Lakecontinentality Puderovas, index zones: 34—Lake I—weak, Zosnas, II— 35—Lakemoderate, Dagdas, III—average, 36—Pond IV—strong. Dagdas. Roman numbers indicate continentality index zones: I—weak, II—moderate, III—average, IV—strong. Forests 2021, 12, 1166 3 of 15 Table 1. Study sites and related information. Coordinates,
Load more

Recommended publications
  • Experiences from Lithuania
    EUROPEANEUROPEAN FORESTFOREST TYPESTYPES Technical workshop “Reporting using the new European Forest Types” EXPERIENCESEXPERIENCES FROMFROM LITHUANIALITHUANIA Lithuanian State Forest Service National Forest Inventory Department Gintaras Kulbokas European forest types/Technical workshop © Lithuanian State Forest Service Bordeaux, France| May 19-21, 2010 e‐mail [email protected] FORESTFOREST GROWINGGROWING CONDITIONSCONDITIONS ININ LITHUANIALITHUANIA ¾The surface is covered by quaternary rocks, originated from glacier; ¾Thickness of this layer: in the northern part - 1-5 m, in the south - up to 200-250 m; ¾The climate is comparable mild, ranging from sea to continental; ¾The hilly highlands are mixtured with plain lowlands; ¾Mean height above sea level is 99 m; ¾ Highest point being 294 m; ¾Mean annual temperature +6ºC; ¾Amount of annual precipitation 630 mm. Area of Lithuania – 65.3 km2 European forest types/Technical workshop © Lithuanian State Forest Service Bordeaux, France| May 19-21, 2010 e‐mail [email protected] LITHUANIANLITHUANIAN FORESTFOREST TYPESTYPES (NFI(NFI--2007)2007) Pine forest 34% Forest area 2.1 mln. ha Spruce forest 18% Birch forest 20% Aspen forest 6% Black alder forest 9% Grey alder forest 7% Oak forest 2% Ash forest 2 % 70% of the forests are stands of natural origin. European forest types/Technical workshop © Lithuanian State Forest Service Bordeaux, France| May 19-21, 2010 e‐mail [email protected] LITUANIANLITUANIAN FORESTFOREST SITESITE TYPESTYPES (NFI(NFI--2007)2007) Humidity of soil: Fertility of soil: Slopes (>15º) 2% Very poor 5% Normal water regime 38% Poor 25% Temporarily overmoisture 37% Fertile 40% Overmoisture 7% Very fertile 27% Drained peatland 8% Especially fertile 3% Peatland 8% Totally 56 forest site types European forest types/Technical workshop © Lithuanian State Forest Service Bordeaux, France| May 19-21, 2010 e‐mail [email protected] RELATIONSHIPRELATIONSHIP BETWEENBETWEEN LITHUANIANLITHUANIAN SITESITE TYPESTYPES ANDAND EUROPEANEUROPEAN FORESTFOREST TYPESTYPES Lithuanian forest site types European forest types Soil fer 2.
    [Show full text]
  • The Gasteromycetes of the Aland Islands, SW Finland: an Annotated Checklist
    Karstenia 37:11-18, 1997 0 The Gasteromycetes of the Aland Islands, SW Finland: an annotated checklist CARL-ADAM fuEGGSTROM HJEGGSTROM, C.-A. 1997: The Gasteromycetes of the Aland Islands, SW Finland: an annotated checklist. - Karstenia 37:11-18. Helsinki. ISSN 0453-3402 Both herbarium specimens and published data on the Gasteromycetes s.l. of the Aland Islands are treated. Altogether, 37 species have been reported which is a little more than half of the total species number of Finland. Seven species, namely Bovista nigres­ cens, B. plumbea, Calvatia excipuliformis, C. utriformis, Lycoperdon perlatum, L. pyriforme and Phallus impudicus seem to be common or fairly common in the Aland Islands. Eight species, viz. Geastrum elegans, G. floriforme, G. schmidelii, G. stria­ tum, Langermannia gigantea, Lycoperdon echinatum, Melanogaster ambiguus and Tulostoma brumale are listed as threatened in Aland. Key words: Aland Islands, checklist, Finland, Gasteromycetes Carl-Adam Hceggstrdm, Department of Ecology and Systematics, PO. Box 7, FIN- 00014 University of Helsinki, Finland Introduction trum specimens in the herbarium of Dr. Stellan Sunhede which are treated in detail in his doctor­ The written knowledge of the Gasteromycetes of al thesis (Sunhede 1989). Besides my own col­ the Aland Islands has hitherto been both scat­ lections (included in H), I have obtained speci­ tered and rather insignificant. In his papers on mens from the following herbaria: H, OULU, Basidiomycetes of Finland, P.A. Karsten (1889, TUR, TURA and UPS . No specimens were sent 1893, 1898) enumerates 27 species, some of from GB , KUO, LD and S. Furthermore, I have them dubious, or defined differently than now, of tried to find published information on Gastero­ the Gasteromycetes s.l.
    [Show full text]
  • Determining Reference Conditions of Hemiboreal Lakes in Latvia, NE Europe: a Palaeolimnological Approach
    Ann. Limnol. - Int. J. Lim. 2018, 54, 22 Available online at: © EDP Sciences, 2018 www.limnology-journal.org https://doi.org/10.1051/limn/2018014 RESEARCH ARTICLE Determining reference conditions of hemiboreal lakes in Latvia, NE Europe: a palaeolimnological approach Normunds Stivrins1,2,3,4,*, Ieva Grudzinska3,5,6,7, Kati Elmi4, Atko Heinsalu4 and Siim Veski4 1 Department of Geography, Faculty of Geography and Earth Sciences, University of Latvia, Riga, Jelgavas street 1, 1004, Latvia 2 Department of Geosciences and Geography, University of Helsinki, P.O. Box 64, Helsinki 00014, Finland 3 Lake and Peatland Research Centre, Alojas district, Puikule, Purvisi, Latvia 4 Institute of Geology, Tallinn University of Technology, Ehitajate tee 5, 19086 Tallinn, Estonia 5 Institute of Plant Sciences, University of Bern, Altenbergrain 21, CH-3013 Bern, Switzerland 6 Oeschger Centre for Climate Change Research, University of Bern, Falkenplatz 16, CH-3013 Bern, Switzerland 7 Institute of Biology, University of Latvia, Miera iela 3, Salaspils 2169, Latvia Received: 28 November 2017; Accepted: 7 May 2018 Abstract – The current status of a lake can be evaluated via monitoring, but such data can only provide information about the last few decades to a century at best. In most cases, the natural state of a lake cannot be ascertained. This is even more challenging if the apparent anthropogenic effects on the environment over the last millennia are considered. We used data on fossil algae from five evenly distributed hemiboreal lakes in geographically different regions in Latvia, NE Europe to assess the amount of compositional change or turnover (i.e., the beta-diversity) in the algae datasets for the last 2000 years by using a Detrended Canonical Correspondence Analysis.
    [Show full text]
  • Characteristics of Boreal and Hemiboreal Herb-Rich Forests As Habitats for Polypore Fungi
    Silva Fennica vol. 52 no. 5 article id 10001 Category: research article https://doi.org/10.14214/sf.10001 SILVA FENNICA http://www.silvafennica.fi Licenced CC BY-SA 4.0 ISSN-L 0037-5330 | ISSN 2242-4075 (Online) The Finnish Society of Forest Science Karoliina Hämäläinen1, Teemu Tahvanainen 2 and Kaisa Junninen3 Characteristics of boreal and hemiboreal herb-rich forests as habitats for polypore fungi Hämäläinen K., Tahvanainen T., Junninen K. (2018). Characteristics of boreal and hemiboreal herb-rich forests as habitats for polypore fungi. Silva Fennica vol. 52 no. 5 article id 10001. 16 p. https://doi.org/10.14214/sf.10001 Highlights • Polypore species richness and diversity were affected positively by dead-wood diversity, and negatively by increasing latitude. • Red-listed species responded only to the abundance of large-diameter dead wood. • Main factor determining composition of polypore assemblages was host-tree species. • High proportion of deciduous dead-wood in herb-rich forests provides complementary effect on polypore assemblages in boreal forest landscapes. Abstract Herb-rich forests are often considered biodiversity hotspots in the boreal zone but their fungal assemblages, particularly those of wood-decaying fungi, remain poorly known. We studied herb-rich forests as habitats for polypores, a distinct group of wood-decaying fungi, and assessed the importance of tree- and stand-scale variables for polypore species richness, abundance, and diversity, including red-listed species. The data include 71 herb-rich forest stands in Finland and 4797 dead wood items, on which we made 2832 observations of 101 polypore species. Dead-wood diversity was the most important variable explaining polypore species richness and diversity, whereas increasing latitude had a negative effect.
    [Show full text]
  • Stand Type Affects Fluxes of Volatile Organic Compounds from the Forest Floor in Hemiboreal and Boreal Climates
    Plant Soil (2019) 441:363–381 https://doi.org/10.1007/s11104-019-04129-3 REGULAR ARTICLE Stand type affects fluxes of volatile organic compounds from the forest floor in hemiboreal and boreal climates Mari Mäki & D. Krasnov & H. Hellén & S. M. Noe & J. Bäck Received: 10 January 2019 /Accepted: 3 May 2019 /Published online: 24 May 2019 # The Author(s) 2019 Abstract by Scots pine with small coverage of Norway spruce Aims The forest floor is a significant contributor to the and birches (Betula pendula and Betula pubescens). stand-scale fluxes of biogenic volatile organic com- Results The total monoterpenoid fluxes were higher pounds. In this study, the effect of tree species (Scots from the Scots pine forest floor (boreal 23 μgm−2 h−1) pine vs. Norway spruce) on forest floor fluxes of volatile and from the mixed forest floor (hemiboreal organic compounds (VOC) was compared in boreal and 32 μgm−2 h−1) compared to the Norway spruce forest hemiboreal climates. floor in both boreal (12 μgm−2 h−1) and hemiboreal Methods Monoterpenoid and sesquiterpene flux rates (9 μgm−2 h−1) climates. Due to higher litterfall produc- were determined during 2017–2018 using dynamic tion, the forest floor seems to be a greater source of (steady-state flow-through) chambers placed on perma- monoterpenoids and sesquiterpenes in the hemiboreal nent soil collars on boreal and hemiboreal forest floors, mixed stand dominated by Scots pine compared to the where the canopy was formed by Scots pine (Pinus boreal Scots pine stand, although the difference was not sylvestris), Norway spruce (Picea abies)ordominated statistically significant.
    [Show full text]
  • Carbon Pools in a Hemiboreal Over-Mature Norway Spruce Stands
    Article Carbon Pools in a Hemiboreal Over-Mature Norway Spruce Stands 1, 1,2 ID 1 ID 1 Laura K, enin¯ , a *, Didzis Elferts , Endijs Baders¯ and Aris¯ Jansons 1 Latvian State Forest Research Institute Silava, R¯ıgas street 111, LV–2169 Salaspils, Latvia; [email protected] (D.E.); [email protected] (E.B.); [email protected] (A.J.)¯ 2 Faculty of Biology, University of Latvia, Jelgavas street 1, LV–1004 R¯ıga, Latvia * Correspondence: [email protected]; Tel.: +371-26-172-965 Received: 21 June 2018; Accepted: 19 July 2018; Published: 20 July 2018 Abstract: Old unmanaged forests are commonly assumed to be carbon neutral; however, there is still a lack of reference studies available to increase the recognition of carbon stock changes in these forests. Studies of old forest carbon storage from hemiboreal regions are very rare compared to temperate and boreal forests in Europe; therefore, the aim of this study was to quantify the carbon stock in hemiboreal over-mature (167–213 years) Norway spruce (Picea abies (L.) Karst.) stands. To explore the total ecosystem carbon pool, the carbon stock of tree biomass, deadwood, and soil in unmanaged (for at least the last 40 years) spruce stands was calculated and compared between different forest site types on dry, wet, and drained mineral soils. Total carbon stock of hemiboreal over-mature spruce stands ranged from 164.8 Mg C ha−1 to 386.7 Mg C ha−1, and 238.5 Mg C ha−1 on average, with no significant differences (p > 0.05) between the forest site types.
    [Show full text]
  • LATVIA: COUNTRY REPORT to the FAO INTERNATIONAL TECHNICAL CONFERENCE on PLANT GENETIC RESOURCES (Leipzig,1996)
    LATVIA: COUNTRY REPORT TO THE FAO INTERNATIONAL TECHNICAL CONFERENCE ON PLANT GENETIC RESOURCES (Leipzig,1996) Prepared by: Ministry of Agriculture Riga, July 1995 LATVIA country report 2 Note by FAO This Country Report has been prepared by the national authorities in the context of the preparatory process for the FAO International Technical Conference on Plant Genetic Resources, Leipzig, Germany, 17-23 June 1996. The Report is being made available by FAO as requested by the International Technical Conference. However, the report is solely the responsibility of the national authorities. The information in this report has not been verified by FAO, and the opinions expressed do not necessarily represent the views or policy of FAO. The designations employed and the presentation of the material and maps in this document do not imply the expression of any option whatsoever on the part of the Food and Agriculture Organization of the United Nations concerning the legal status of any country, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. LATVIA country report 3 Table of Contents CHAPTER 1 INTRODUCTION TO LATVIA AND ITS AGRICULTURAL SECTOR 5 1.1 GEOGRAPHY AND CLIMATE 5 1.2 THE LAND USE 6 1.3 FACTS ABOUT AGRICULTURE 6 1.3.1 Sown areas of different crops 7 CHAPTER 2 INDIGENOUS PLANT GENETIC RESOURCES 9 2.1 WILD SPECIES AND WILD RELATIVES 9 2.2 LANDRACES AND OLD CULTIVARS 9 2.3 PROTECTION 10 CHAPTER 3 NATIONAL CONSERVATION ACTIVITIES 11 3.1 IN SITU CONSERVATION ACTIVITIES 11 3.2 EX SITU COLLECTIONS
    [Show full text]
  • Glossary of Landscape and Vegetation Ecology for Alaska
    U. S. Department of the Interior BLM-Alaska Technical Report to Bureau of Land Management BLM/AK/TR-84/1 O December' 1984 reprinted October.·2001 Alaska State Office 222 West 7th Avenue, #13 Anchorage, Alaska 99513 Glossary of Landscape and Vegetation Ecology for Alaska Herman W. Gabriel and Stephen S. Talbot The Authors HERMAN w. GABRIEL is an ecologist with the USDI Bureau of Land Management, Alaska State Office in Anchorage, Alaskao He holds a B.S. degree from Virginia Polytechnic Institute and a Ph.D from the University of Montanao From 1956 to 1961 he was a forest inventory specialist with the USDA Forest Service, Intermountain Regiono In 1966-67 he served as an inventory expert with UN-FAO in Ecuador. Dra Gabriel moved to Alaska in 1971 where his interest in the description and classification of vegetation has continued. STEPHEN Sa TALBOT was, when work began on this glossary, an ecologist with the USDI Bureau of Land Management, Alaska State Office. He holds a B.A. degree from Bates College, an M.Ao from the University of Massachusetts, and a Ph.D from the University of Alberta. His experience with northern vegetation includes three years as a research scientist with the Canadian Forestry Service in the Northwest Territories before moving to Alaska in 1978 as a botanist with the U.S. Army Corps of Engineers. or. Talbot is now a general biologist with the USDI Fish and Wildlife Service, Refuge Division, Anchorage, where he is conducting baseline studies of the vegetation of national wildlife refuges. ' . Glossary of Landscape and Vegetation Ecology for Alaska Herman W.
    [Show full text]
  • Height-Growth Dynamics of Scots Pine (Pinus Sylvestris L.) in Burned and Clearcut Areas in Hemiboreal Forests, Latvia
    PROCEEDINGS OF THE SECOND INTERNATIONAL CONGRESS OF SILVICULTURE Florence, November 26th - 29th 2014 HEIGHT-GROWTH DYNAMICS OF SCOTS PINE (PINUS SYLVESTRIS L.) IN BURNED AND CLEARCUT AREAS IN HEMIBOREAL FORESTS, LATVIA Mara Zadina1, Liga Purina1, Agris Pobiarzens1, Juris Katrevics1 Janis Jansons2, Aris Jansons1 1Latvian State Forest Research Institute “Silava”, Rigas 111, Salaspils, Latvia; [email protected] 2Forest Competence Centre, Dzerbenes str. 27, Riga, Latvia The aim of this study was to compare medium-term growth dynamics of Scots pine (Pinus sylvestris L.) in areas after forest fire and clearcut in different forest types to improve the understanding of post-fire growth of trees in hemiboreal forest zone. The data were collected at four Scots pine dominated forest stands located in northern and central parts of Latvia (56°45´ - 57°40´N; 22°32´- 24°98´E) burned or clearcut in 1992, 2004 and 2006; forest types Vacciniosa, Vacciniosa mel and Myrtillosa mel. In each study site 100m2 and 25 m2 circular plots were placed systematically and height increment of Scots pine were measured. The average height of Scots pine at the age of 8 years was 167±54.2 cm Vacciniosa and 230±90.3 cm Myrtillosa mel. At the age of 10 years 184+71.1 cm Vacciniosa mel, and at the age of 22 years 360±214.1 cm Vacciniosa. Our results demonstrated that 8 years after the forest fire mean height of Scots pine was significantly lower in burned areas in comparison to clearcut, but there were no significant differences in mean height of trees 10 and 19 years after forest fire.
    [Show full text]
  • A New Record of Arctic Bramble, Rubus Arcticus, in the Åland Islands, SW Finland
    Memoranda Soc. Fauna Flora Fennica 86:54–58. 2010 A new record of Arctic Bramble, Rubus arcticus, in the Åland Islands, SW Finland Torsten Stjernberg, Ralf Carlsson, Carl-Adam Hæggström, Eeva Hæggström & Kajsa Sundberg Torsten Stjernberg, Finnish Museum of Natural History, Zoological Museum, P.O. Box 17, FI-00014 University of Helsinki, Finland. E-mail: [email protected] Carlsson, R., Högbackagatan 10, AX-22100 Mariehamn, Åland, Finland. E-mail: [email protected] Hæggström, C.-A., Finnish Museum of Natural History, Botanical Museum, P.O. Box 7, FI-00014 University of Helsinki, Finland. E-mail: [email protected] Hæggström, E., Tornfalksvägen 2/26, FI-02620 Esbo, Finland. E-mail: eeva. [email protected] Sundberg, K., Södravägen 491, AX-22340 Geta, Åland, Finland. E-mail: kajsa. [email protected] The Arctic Bramble, Rubus arcticus L., was found in Gottby in the municipality of Jomala, the Åland Islands, SW Finland, in June 2009. It was both flowering and fruiting, although rather sparingly. This boreal species has not been observed in the Åland Islands since 1950. The total distribution of the species is outlined. An account is given of the pre- vious six observations of R. arcticus in Åland. The dispersal of the seeds (endocarps with seeds) of R. arcticus is treated. Introduction concentration in the central part of the country (Saastamoinen 1931, Hultén 1971, Lampinen & The arctic bramble, Rubus arcticus L. is a northern Lahti 2009). Rubus arcticus is, however, a very species. Its area comprises most of the Eurasian rare plant in the southwestern archipelago area of taiga, from Scandinavia to the Far East (Hultén & Finland including the Ålands Islands (Palmgren & Fries 1986).
    [Show full text]
  • Undrained Peatland Areas Disturbed by Surrounding Drainage: a Large Scale GIS Analysis in Finland with a Special Focus on Aapa Mires
    Undrained peatland areas disturbed by surrounding drainage: a large scale GIS analysis in Finland with a special focus on aapa mires A. Sallinen1,3,4, S. Tuominen2, T. Kumpula3 and T. Tahvanainen4 1Biodiversity Centre, Finnish Environment Institute SYKE, Kuhmo, Finland 2Biodiversity Centre, Finnish Environment Institute SYKE, Helsinki, Finland 3Department of Geographical and Historical Studies, University of Eastern Finland, Joensuu, Finland 4Department of Environmental and Biological Sciences, University of Eastern Finland, Joensuu, Finland _______________________________________________________________________________________ SUMMARY Half of the Finnish peatland area is drained for forestry. The remaining undrained peatlands are not all pristine, because surrounding drainage may disturb their hydrology. This concerns especially aapa mires, which are dependent on hydrological connections to their upper catchments. We investigated the amount and sizes of Finnish undrained peatlands, the drainage state of their margins, and the naturalness of aapa mires in large (> 50 ha) undrained peatland areas, using a GIS analysis based on digital map data, aerial images and an elevation model. The results show that a majority (66.7 % of count, 84.7 % of area) of undrained peatland areas have at least partly drained margins. Drainage activities commonly disturb minerotrophic water discharge to aapa mires. In the middle boreal zone, on average 41.6 % (median 42.8 %) of the catchment area of aapa mires is such that hydrological connection with the mire is disturbed by intervening drainage. In the southern boreal zone, the figure is 25.1 % (median 16.1 %), and in the southern part of the northern boreal zone 24.2 % (median 9.9 %). Possible implications of the disturbances include tree encroachment, hummock formation and fen–bog transition, which is likely to cause a loss of biodiversity but could potentially increase peat growth and carbon sequestration.
    [Show full text]
  • Ground-Living Spider Communities (Araneae) on Boreal and Hemiboreal Peatbogs
    Ground-living spider communities (Araneae) on boreal and hemiboreal peatbogs Seppo Koponen Zoological Museum, Centre for Biodiversity University of Turku, FIN-20014 Turku Finland; e-mail: [email protected] Introduction Peatbogs are typical biotopes in the northern coniferous forest zone. Approximately a third of the land area of Finland was covered by peatlands, of which about a half has been drained for forestry, farming and peat harvesting (Wahlström et al. 1996). So peat- land ecosystems (mires, bogs, fens) are endangered even in northern Europe, and many organisms living in peatland habitats are nowadays considered as threatened. This is true also for spiders (e.g. Koponen 1985). For example, in the recent Finnish Red Data Book (Rassi et al. 2000) six of the total 34 listed spider species are inhabitants of mires. Some general information is here given on typical peatbogs spiders, both abundant and rare ones, and on their distributional trends, along a transect from the southern- most parts of the hemiboreal vegetation zone to northern borders of the northern boreal zone. Material Spiders were collected along a transect from southern Lithuania (54°N) to Lapland (northern Finland, 69°30’N). Peatbogs studied included both open treeless and pine growing Sphagnum bogs in the hemiboreal and boreal vegetation zones. Ground-li- ving, epigeic spiders were collected using pitfall traps. For details of study sites and collecting methods, see Koponen et al. (2001). Additional data used here is based on studies by Asta Vilbaste on Estonian peatbogs (e.g. Vilbaste 1980-81) and on the pre- sent author’s published (Koponen 1968, 1979a, 1979b, 1985, Lehtinen et al.
    [Show full text]