Late-quaternary vegetation in eastern Blekinge, south-eastern Sweden a pollen-analytical study by BjoМ€rn E. Berglund

Cover of: Late-quaternary vegetation in eastern Blekinge, south-eastern Sweden | BjoМ€rn E. Berglund

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  • Sweden,
  • Blekinge.


  • Pollen, Fossil -- Sweden -- Blekinge.,
  • Paleobotany -- Quaternary.,
  • Paleobotany -- Sweden -- Blekinge.

Edition Notes

Part of illustrative matter in pocket.

Book details

Statementby Björn E. Berglund.
SeriesOpera botanica,, v. 12:1-2, Publications from the Institute of Mineralogy, Paleontology, and Quaternary Geology, University of Lund, Sweden,, no. 134, Publications from the Institutes of Mineralogy, Paleontology, and Quaternary Geology, University of Lund, Sweden ;, no. 134.
LC ClassificationsQE1 .L952 no. 134
The Physical Object
Pagination2 v.
ID Numbers
Open LibraryOL5689109M
LC Control Number70005759

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Get this from a library. Late-quaternary vegetation in eastern Blekinge, south-eastern Sweden; a pollen-analytical study. [Björn E Berglund]. This volume presents a review and evaluation of the palynological examination of Near and Eastern sediment cores covering the l years, eith the aim of reconstructing the Late Quaternary vegetational history.

The pollen evidence is supplemented by archaeobotanical the vegetation of earlier times cannot be understood without Cited by: Late Quaternary Vegetation in Eastern Blekinge, South-Eastern Sweden by Björn Berglund (p. Berglund, BE (b) Late-Quaternary Vegetation in Eastern Blekinge, South-Eastern Sweden: A Pollen-Analytical Study – II.

Post-Glacial Time (Opera Botanica 12). Post-Glacial Time (Opera Botanica 12).Cited by: The number of pollen taxa (terrestrial plants) recorded in the eastern Blekinge data set (pollen diagrams from 14 sites; Berglund, a, Berglund, b) have been compiled and plotted in a cumulative diagram (cf.

Berglund, b, Fig. 60).The synthesis Late-quaternary vegetation in eastern Blekinge in Fig. 5 presents percentages for each chronozone in relation to the records for Late Holocene (last years).Cited by: To order a copy of articles of the books, please contact us via email:: [email protected] LATE-QUATERNARY VEGETATION IN EASTERN BLEKINGE, SOUTH-EASTERN SWEDENvol.

1 BERGLUND-B.E. LATE-QUATERNARY VEGETATION IN EASTERN BLEKINGE, SOUTH-EASTERN SWEDENvol. 2 Keywords: paleontologia, altro: LINNERMARK-N. PODSOL OCH. Late Quaternary vegetation history and climatic change in the eastern Orange Free State, South Africa L.

Scott, Department of Botany, University of the Orange Free State, P.O. BoxBloemfontein, Republic of South Africa Department Late-quaternary vegetation in eastern Blekinge Botany, University of the Orange Free State P.O. Box Bloemfontein Republic of South Africa Sixty-nine pollen spectra from three sites with Cited by: Late-Devensian deposits REFERENCES BERGLUND, B.

Late-Quaternary vegetation in Eastern Blekinge, South-Eastern Sweden. Late-Glacial by: 8. A late Quaternary pollen dataset from eastern continental Asia for vegetation and climate reconstructions: Set up and evaluation April Review of Palaeobotany and Palynology –   Boethius, A.

Signals of sedentism: Faunal exploitation as evidence of a delayed-return economy at Norje Sunnansund, an Early Mesolithic site in south-eastern Sweden. Data on environmental change at the Younger Dryas-Preboreal transition and during the early Holocene are reviewed with Berglund, B.E.

Late Quaternary vegetation in eastern Blekinge, southeastern Sweden Symposium on Lateglacial and Holocene environmental changes, Vistula BasinExcursion Guide book, Cracow, Cited by: The Pedunculate oak is Sweden’s oldest and largest known tree and referred to as Kvilleken.

It is speculated that it is over a years old. As old oak trees have a hollow trunk, it is impossible to determine its age by counting the tree rings (tree rings within the trunk indicate the age of a tree).

Late-Devensian deposits I71 REFERENCES BERGLUND, B. (i). Late-Quaternary vegetation in Eastern Blekinge, South-Eastern Sweden. Late-Glacial Time. We review the history of Quaternary pollen analysis from to the present-day, with particular emphasis on methodological and conceptual developments and on the early pioneers of the subject.

The history is divided into three phases—the pioneer phase –, the building phase –, and the mature phase –present-day. We also south-eastern Sweden book relevant studies prior to Cited by: Margaret Adebisi Sowunmi (née Jadesimi) (Septem -) is a Nigerian botanist and environmental archaeologist.

She was Professor of Palynology and Environmental Archaeology at the University of pioneered the study of environmental archaeology and palaeoethnobotany in Nigeria and is the founder and president of the Palynological Association of mater: University College Ibadan.

The Littorina transgression in southeastern Sweden and its relation to mid-Holocene climate variability By Shi-Yong Yu This thesis is based on the work carried out while I was a Ph. student at the Department of Geol-ogy, GeoBiosphere Science Centre, Lund Univer-sity, between September and November   Berglund BE (b) Late-Quaternary vegetation in eastern Blekinge, south-eastern by: The Quaternary cover in eastern Skåne and on the Listerlandet Peninsula is dominated by glaciofluvial and glaciolacustrine deposits from the Late Weichselian deglaciation and wave-washed sand deposited primarily during the early Holocene [ 68, 69 ].Cited by: 1.

Per Björn-Erik Berglund, föddär en svensk geolog. Berglund blev filosofie doktor vid Lunds universitet på avhandlingen Late-Quaternary Vegetation in Eastern Blekinge, South-Eastern Sweden: a Pollen-Analytical var professor i kvartärgeologi vid nämnda universitet (som efterträdare till Tage Nilsson).Han blev ledamot av Vetenskapsakademien.

LATE QUATERNARY VEGETATION HISTORY IN THE HORTOBÁGY STEPPE AND MIDDLE TISZA FLOODPLAIN, NE HUNGARY E. MAGYARI HAS-NHMUS Research Group for Palaeontology, H– Budapest, Pf.Hungary; [email protected] Palaeoecological records of the last glacial period and the Holocene in NE Hungary are.

Vegetation zones and their sections in northwestern Europe IND Habitat preferences of red-listed fungi and bryophytes in woodland key habitats in southern Sweden--analyses of data from a national survey.

Late-Quaternary vegetation in eastern Blekinge, south-eastern Sweden. Berglund. Opera Botanica Landscape-ecological aspects of Cited by: Kluwer Academic Publishers, Dordrecht. Berglund, B.

Late-Quaternary vegetation in eastern Blekinge, south-eastern Sweden. A pollen-analytical study. Late-Glacial time. The Baltic sea-level oscillations in the Atlantic and Subboreal periods are known from sedimentary records on slightly uplifting coasts in Denmark and southern Sweden (e.g., Berglund, ; Digerfeldt, ).The periodicity of those oscillations is in close correlation with recent data on climatic cycles with a periodicity of, and yr (e.g., Stuiver et al., ; Chapman and.

There have been few Late Quaternary vegetation records from the acidic lithologies of south east England. This study reports on investigations from three new valley mire sites (Bagshot, Conford and Hurston Warren), using pollen and charcoal analyses with chronologies provided by radiocarbon dating.

The Bagshot sequence begins at c. cal. BP with high Betula and Pinus sylvestris pollen. markedly changed the original vegetation. Only a few small natural grassland areas remain in S and SE Brazil.

Methods and available pollen records Pollen analysis of Late Quaternary peat, lake or other organic deposits is one important tool to reconstruct the history of grasslands.

Grass and sedge pollen in conjunction with pollen from oth. Try the new Google Books. Check out the new look and enjoy easier access to your favorite features East African vegetation catena Celtis clay climate coastal Combretum common Compositeae cover Cyperaceae Dendrosenecio distribution dominant drier East Africa eastern Ecol ecological elephant epiphytic Euphorbiaceae excelsa Fergus Wilson.

Scania, Swedish: Skåne (Swedish: [ˈskôːnɛ] ()), is the southernmost province (landskap) of Scania, there are 33 municipalities that are autonomous within the Scania Regional 's largest city is Malmö, which is also the third largest in Sweden, as well as the fifth largest in Scandinavia.

To the north, Scania borders the provinces of Halland and Småland, to Country: Sweden. In this book, Bleda Düring offers an archaeological analysis of Asia Minor, the area equated with much of modern-day Turkey, f to 2, BC.

During this period human societies moved from small-scale hunter-gatherer groups to complex and hierarchical communities with economies based on agriculture and by: Lake Vättern is the second-largest lake ( km 2) in Sweden; it is km long and has a maximum width of 31 lake occupies a graben that trends SSW-NNE and follows the Sveconorwegian front ().The front marks the eastern boundary of the – Ga Sveconorwegian province (Bingen et al., ).This province is juxtaposed against older Svecokarelian by: Southern Mongolia is a part of the arid to semiarid region of Central Asia and represents a transitional zone between the circulation systems of westerlies and associated North Atlantic Oscillation (NAO), the Asian summer monsoon and the Mongolian High Pressure System (MHPS).

The sedimentary records from this geographically important region are a central key to understand past vegetation and Cited by: 5. Terrestrial, algal, and siliceous indicators.

Developments in paleoenvironmental research, vol 3. Kluwer, Dordrecht, pp 5–33 Berglund BE () Vegetation på ön Senoren I. Bot Not – Berglund BE () Late-Quaternary vegetation in eastern Blekinge, south-eastern Sweden. A pollen analytical study I: late-glacial time.

The stratigraphy and chronology of Late Quaternary raised coastal deposits in Renfrewshire and Ayrshire, western Scotland. Littorina transgressions in Blekinge, South Sweden. A preliminary survey.

Sedimentary environments of the Weald Clay of south-eastern : William E. Boyd. Late Quaternary vegetation, This problem is particularly acute in the extra-Andean ranges of eastern Brazil, the so-called ‘Mata Atlantica biodiversity hotspot’, where rigorous palaeoecological work has only begun during the last few years.

Discussion and conclusions for conservation and by: Abstract: The Southern Forests study area covers an area of about six million hectares of south-eastern New South Wales, south of Oberon and Kiama and east of Albury and Boorowa (latitude 33° 02’–37 ° 06’ S; longitude ° 56’ – ° 06’ E).

The total area of existing vegetation mapped was three million hectares (3 Berglund, B.E. Late-Quaternary vegetation in eastern Blekinge, south-eastern Sweden.

Opera Botanica, 12, Berglund, B.E., Malmer, N., Persson, T. () Landscape-ecological aspects of long-term changes in the Ystad area. The Cultural Landscape During years in Southern Sweden — the Ystad Project.

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Postdrifting mesozoic. Africa, the "Odd man out". Floristic relationships between tropical Africa and tropical America.

Angiosperm evolution and the relationship of the floras of Africa and America. Palms in the tropical forest ecosystems of Africa and South America. Problems related to the transoceanic transport of insects, especially between the Amazon and Congo Areas. Detailed description of plants, one plant per page.

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In eastern Blekinge, Ringberg placed the level at about 65 m a.s.l., slightly higher than in the western part. Nilsson's () shoreline displacement record, partly based on a sediment sequence from central Blekinge described by De Geer (), shows several drainage events during the Cited by: 2.

The climate fluctuated; new land became available due to melting ice and isostatic land uplift. The vegetation changed rapidly. During a single lifetime great changes could be observed. From the Late Glacial / Holocene transition to the middle of the Preboreal, great changes occurred in the climate, vegetation and fauna both on land and in the sea.Issuu is a digital publishing platform that makes it simple to publish magazines, catalogs, newspapers, books, and more online.

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