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Journal articles on the topic 'Holocène – Europe'

Author: Grafiati

Published: 4 June 2021

Last updated: 17 February 2022

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1

Auffray, Jean-Christophe, Jacques Cassaing, and Serge Legendre. "Anthropisation et biosphère : impact de l'homme sur la guilde des souris et les communautés de mammifères en Europe au Pléistocène et Holocène." Bulletin de la Société préhistorique française 88, no. 4 (1991): 122–28. http://dx.doi.org/10.3406/bspf.1991.9468.

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2

Buczkó, Krisztina, and Enikő Magyari. "The Holocene diatom flora of Lake Saint Anna (Eastern Carpathians, Europe)." Algological Studies 124 (July 1, 2007): 1–28. http://dx.doi.org/10.1127/1864-1318/2007/0124-0001.

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3

Castel, Ilona, Eduard Koster, and Rudolf Slotboom. "Morphogenetic aspects and age of Late Holocene eolian drift sands in Northwest Europe." Zeitschrift für Geomorphologie 33, no. 1 (1989): 1–26. http://dx.doi.org/10.1127/zfg/33/1989/1.

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4

Allen, Judy R. M., Antony J. Long, Chris J. Ottley, D. Graham Pearson, and Brian Huntley. "Holocene climate variability in northernmost Europe." Quaternary Science Reviews 26, no. 9-10 (2007): 1432–53. http://dx.doi.org/10.1016/j.quascirev.2007.02.009.

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5

Forestier, Hubert, Michel Grenet, Antony Borel, and Vincenzo Celiberti. "Les productions lithiques de l’Archipel indonésien." Journal of Lithic Studies 4, no. 2 (2017): 231–303. http://dx.doi.org/10.2218/jls.v4i2.2544.

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Proposer une synthèse sur la préhistoire d’un archipel et de ses assemblages lithiques n’est pas chose facile, d’une part à cause de l’immensité de l’espace concerné mesurant 2 millions de km2, d’autre part du fait que la notion de Paléolithique y est difficilement applicable et notamment celles de « Paléolithique supérieur » ou d’Epipaléolithique-Mésolithique établies en Eurasie occidentale. L’Indonésie et ses myriades d’îles et îlots (environ 18000) s’inscrivent dans un rectangle 5000 km sur 2000 km de part et d’autre de l’équateur ce qui en fait le plus grand archipel du monde. Cette aire g

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6

Goudie, A. S., H. A. Viles, and A. Pentecost. "The late-Holocene tufa decline in Europe." Holocene 3, no. 2 (1993): 181–86. http://dx.doi.org/10.1177/095968369300300211.

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7

Robson, Harry K. "The early settlement of Northern Europe." Antiquity 93, no. 367 (2019): 260–63. http://dx.doi.org/10.15184/aqy.2018.264.

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This three-volume publication presents an up-to-date overview on the human colonisation of Northern Europe across the Pleistocene–Holocene transition in Scandinavia, the Eastern Baltic and Great Britain. Volume 1, Ecology of early settlement in Northern Europe, is a collection of 17 articles focusing on subsistence strategies and technologies, ecology and resource availability and demography in relation to different ecological niches. It is structured according to three geographic regions, the Skagerrak-Kattegat, the Baltic Region and the North Sea/Norwegian Sea, while its temporal focus is La

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8

Kern, Zoltán, Attila Demény, Aurel Perşoiu, and István Gábor Hatvani. "Speleothem Records from the Eastern Part of Europe and Turkey—Discussion on Stable Oxygen and Carbon Isotopes." Quaternary 2, no. 3 (2019): 31. http://dx.doi.org/10.3390/quat2030031.

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The region comprising of East Central Europe, South East Europe and Turkey contributed to the SISAL (Speleothem Isotopes Synthesis and AnaLysis) global database with stable carbon and oxygen isotope time-series from 18 speleothems from 14 caves. The currently available oldest record from the studied region is the ABA-2 flowstone record (Abaliget Cave; Hungary) reaching back to MIS 6. The temporal distribution of the compiled 18 records from the region points out a ~20 kyr-long period, centering around 100 ka BP, lacking speleothem stable isotope data. The regional subset of SISAL_v1 records di

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9

Affolter, Stéphane, Anamaria Häuselmann, Dominik Fleitmann, R. Lawrence Edwards, Hai Cheng, and Markus Leuenberger. "Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years." Science Advances 5, no. 6 (2019): eaav3809. http://dx.doi.org/10.1126/sciadv.aav3809.

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The reasons for the early Holocene temperature discrepancy between northern hemispheric model simulations and paleoclimate reconstructions—known as the Holocene temperature conundrum—remain unclear. Using hydrogen isotopes of fluid inclusion water extracted from stalagmites from the Milandre Cave in Switzerland, we established a mid-latitude European mean annual temperature reconstruction for the past 14,000 years. Our Milandre Cave fluid inclusion temperature record (MC-FIT) resembles Greenland and Mediterranean sea surface temperature trends but differs from recent reconstructions obtained f

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10

Ponomarev, D. V., Kolfschoten van, and der van. "Late Glacial and Holocene micromammals of northeastern Europe." Russian Journal of Theriology 11, no. 2 (2012): 121–30. http://dx.doi.org/10.15298/rusjtheriol.11.2.02.

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11

Zimmermann, Andreas. "Cultural cycles in Central Europe during the Holocene." Quaternary International 274 (October 2012): 251–58. http://dx.doi.org/10.1016/j.quaint.2012.05.014.

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12

HYVARINEN, HANNU. "Holocene vegetation dynamics in Europe at continental scale." Boreas 13, no. 4 (2008): 376. http://dx.doi.org/10.1111/j.1502-3885.1984.tb00952.x.

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13

Long, D., A. G. Dawson, and D. E. Smith. "Tsunami risk in northwestern Europe: a Holocene example." Terra Nova 1, no. 6 (1989): 532–37. http://dx.doi.org/10.1111/j.1365-3121.1989.tb00429.x.

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14

Seppä, H., A. E. Bjune, R. J. Telford, H. J. B. Birks, and S. Veski. "Last nine-thousand years of temperature variability in Northern Europe." Climate of the Past 5, no. 3 (2009): 523–35. http://dx.doi.org/10.5194/cp-5-523-2009.

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Abstract. The threat of future global warming has generated a major interest in quantifying past climate variability on centennial and millennial time-scales. However, palaeoclimatological records are often noisy and arguments about past variability are only possible if they are based on reproducible features in several reliably dated datasets. Here we focus on the last 9000 years, explore the results of 36 Holocene pollen-based July mean and annual mean temperature reconstructions from Northern Europe by stacking them to create summary curves, and compare them with a high-resolution, summary

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15

Seppä, H., A. E. Bjune, R. J. Telford, H. J. B. Birks, and S. Veski. "Last nine-thousand years of temperature variability in Northern Europe." Climate of the Past Discussions 5, no. 3 (2009): 1521–52. http://dx.doi.org/10.5194/cpd-5-1521-2009.

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Abstract. The threat of future global warming has generated a major interest in quantifying past climate variability on centennial and millennial time-scales. However, palaeoclimatological records are often noisy and arguments about past variability are only possible if they are based on reproducible features in several reliably dated datasets. Here we focus on the last 9000 years, explore the results of 35 Holocene pollen-based July mean and annual mean temperature reconstructions from Northern Europe by stacking them to create summary curves, and compare them with a high-resolution, summary

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16

Clemmensen, Lars B., Aslaug C. Glad, Kristian W. T. Hansen, and Andrew S. Murray. "Episodes of aeolian sand movement on a large spit system (Skagen Odde, Denmark) and North Atlantic storminess during the Little Ice Age." Bulletin of the Geological Society of Denmark 63 (April 24, 2015): 17–28. http://dx.doi.org/10.37570/bgsd-2015-63-03.

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Late Holocene coastal dune successions in north-western Europe contain evidence of episodic aeolian sand movement in the recent past. If previous periods of increased sand movement can be dated sufficiently precisely and placed in a correct cultural and geomorphological context, they may add to our understanding of storminess variation and climate change in the North Atlantic during the later part of the Holocene.

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17

Souto, Castro, García-Rodeja, and Pontevedra-Pombal. "The Use of Plant Macrofossils for Paleoenvironmental Reconstructions in Southern European Peatlands." Quaternary 2, no. 4 (2019): 34. http://dx.doi.org/10.3390/quat2040034.

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The analysis of plant macrofossils in peatland ecosystems has been widely used for the climatic and ecological reconstruction of the Holocene in the high latitudes of the northern hemisphere. By contrast, perhaps associated with rarity of these ecosystems, this proxy has barely been explored for southern Europe. In this work, a compilation and review of existing knowledge on the study of plant macrofossils of peatlands in southern Europe has been carried out, both from a paleoenvironmental perspective and in terms of biodiversity dynamics. Although small in surface area, the peatlands of south

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18

Feurdean, Angelica, Boris Vannière, Walter Finsinger, et al. "Fire hazard modulation by long-term dynamics in land cover and dominant forest type in eastern and central Europe." Biogeosciences 17, no. 5 (2020): 1213–30. http://dx.doi.org/10.5194/bg-17-1213-2020.

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Abstract. Wildfire occurrence is influenced by climate, vegetation and human activities. A key challenge for understanding the risk of fires is quantifying the mediating effect of vegetation on fire regimes. Here, we explore the relative importance of Holocene land cover, land use, dominant functional forest type, and climate dynamics on biomass burning in temperate and boreo-nemoral regions of central and eastern Europe over the past 12 kyr. We used an extensive data set of Holocene pollen and sedimentary charcoal records, in combination with climate simulations and statistical modelling. Bio

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19

Hercman, Helena, Michał Gąsiorowski, Jacek Pawlak, et al. "Atmospheric circulation and the differentiation of precipitation sources during the Holocene inferred from five stalagmite records from Demänová Cave System (Central Europe)." Holocene 30, no. 6 (2020): 834–46. http://dx.doi.org/10.1177/0959683620902224.

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Five stalagmites from the Demänová Cave System (DCS, Western Carpathians, Slovakia), spanning the period from 13,000 to 500 a BP, were analyzed for their oxygen and carbon stable isotopic composition of the calcite. The isotopic data obtained from several stalagmites located in one cave system allow us to separate the changes of regional/global importance from the local changes. Oxygen isotope ratios point to dynamic changes in the environment at the onset of the Holocene. Despite the local differences, carbon isotope data express the gradual and steady development of vegetation on the surface

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20

Magny, Michel, Urs Leuzinger, Sigmar Bortenschlager, and Jean Nicolas Haas. "Tripartite climate reversal in Central Europe 5600–5300 years ago." Quaternary Research 65, no. 1 (2006): 3–19. http://dx.doi.org/10.1016/j.yqres.2005.06.009.

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AbstractThe history of variations in water level of Lake Constance, as reconstructed from sediment and pollen analysis of a sediment sequence from the archaeological site of Arbon-Bleiche 3, shows an abrupt rise in lake level dendrochronologically dated to 5375 yr ago (5320 yr relative to AD 1950). This event, paralleled by the destruction of the Neolithic village by fire, provoked the abandonment of this prehistoric lake-shore location established in the former shallow bay of Arbon-Bleiche, and was the last of a series of three episodes of successively higher lake level, the first occurring a

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21

Kaplan, Jed O. "Integrated modeling of Holocene land cover change in Europe." Quaternary International 279-280 (November 2012): 235–36. http://dx.doi.org/10.1016/j.quaint.2012.08.530.

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22

Magri, Donatella. "Some questions on the late-Holocene vegetation of Europe." Holocene 5, no. 3 (1995): 354–60. http://dx.doi.org/10.1177/095968369500500312.

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23

Waller, Richard. "Holocene book review: Iceland (Classic Geology in Europe 3)." Holocene 25, no. 4 (2015): 727–28. http://dx.doi.org/10.1177/0959683615569111.

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24

Roman, Dídac, Célia Fat Cheung, and Mathieu Langlais. "Cultures of the Pleistocene-Holocene transition in Western Europe." Quaternary International 564 (October 2020): 1–2. http://dx.doi.org/10.1016/j.quaint.2020.06.039.

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25

Clark, Geoffrey A. "A Mesolithic Tapestry—Holocene Europe Prior to the Neolithic." Journal of Island and Coastal Archaeology 4, no. 2 (2009): 249–55. http://dx.doi.org/10.1080/15564890903083541.

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26

Emeis, Kay-Christian, and Alastair G. Dawson. "Holocene palaeoclimate records over Europe and the North Atlantic." Holocene 13, no. 3 (2003): 305–9. http://dx.doi.org/10.1191/0959683603hl622ed.

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27

Harrison, Sandy P., I. Colin Prentice, and Joël Guiot. "Climatic controls on Holocene lake-level changes in Europe." Climate Dynamics 8, no. 4 (1993): 189–200. http://dx.doi.org/10.1007/bf00207965.

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28

Dubatolov, Vladimir, and Oleg Kosterin. "Nemoral species of Lepidoptera (Insecta) in Siberia: a novel view on their history and the timing of their range disjunctions." Entomologica Fennica 11, no. 3 (2000): 141–66. http://dx.doi.org/10.33338/ef.84061.

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Distributions in Siberia of nemorallepidopteran species, trophically or cenotically tied to broad-leaved (nemoral) forests or their phytocenotic derivates, display seven main types of range: Amphipalaearctic; Europe – West-Siberia – Far-East disjunctive; East-Europe – Altai – Far-East disjunctive; Altai – Far-East disjunctive; South-Siberia – Far-East; Transbaikalia – Far-East; Europe- Transuralia. An eastern origin can be traced for most of these species, with the exception of the last-mentioned type. According to palynological data, a continuous belt of broad-leaved forests was re-establishe

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29

Andersson, C., F. S. R. Pausata, E. Jansen, B. Risebrobakken, and R. J. Telford. "Holocene trends in the foraminifer record from the Norwegian Sea and the North Atlantic Ocean." Climate of the Past Discussions 5, no. 4 (2009): 2081–113. http://dx.doi.org/10.5194/cpd-5-2081-2009.

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Abstract. The early to mid-Holocene thermal optimum is a well-known feature in a wide variety of paleoclimate archives from the Northern Hemisphere. Reconstructed summer temperature anomalies from across northern Europe show a clear maximum around 6 ka. For the marine realm, Holocene trends in sea-surface temperature reconstructions for the North Atlantic and Norwegian Sea do not exhibit a consistent pattern of early to mid-Holocene warmth. Sea-surface temperature records based on alkenones and diatoms generally show the existence of a warm early to mid-Holocene optimum. In contrast, several f

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30

Andersson, C., F. S. R. Pausata, E. Jansen, B. Risebrobakken, and R. J. Telford. "Holocene trends in the foraminifer record from the Norwegian Sea and the North Atlantic Ocean." Climate of the Past 6, no. 2 (2010): 179–93. http://dx.doi.org/10.5194/cp-6-179-2010.

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Abstract. The early to mid-Holocene thermal optimum is a well-known feature in a wide variety of paleoclimate archives from the Northern Hemisphere. Reconstructed summer temperature anomalies from across northern Europe show a clear maximum around 6000 years before present (6 ka). For the marine realm, Holocene trends in sea-surface temperature reconstructions for the North Atlantic and Norwegian Sea do not exhibit a consistent pattern of early to mid-Holocene warmth. Sea-surface temperature records based on alkenones and diatoms generally show the existence of a warm early to mid-Holocene opt

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31

Pandolfi, Luca, Carmelo Petronio, and Leonardo Salari. "Bos primigenius Bojanus, 1827 from the Early Late Pleistocene Deposit of Avetrana (Southern Italy) and the Variation in Size of the Species in Southern Europe: Preliminary Report." Journal of Geological Research 2011 (June 22, 2011): 1–11. http://dx.doi.org/10.1155/2011/245408.

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Very abundant remains of Bos primigenius have been recovered in the early Late Pleistocene site of Avetrana (southern Italy). The site is characterized by a karst filling originated from a series of almost coeval depositional events. This discovery represents a rare record in the early Late Pleistocene of southern Europe. Biometrical analysis of the metapodial bones of aurochs from Avetrana gave the cue to examine the evolutive trend of the species in southern Europe, from the Middle Pleistocene to Holocene. This trend is characterized by an increase in size of the metapodial bones from Middle

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32

Fischer, N., and J. Jungclaus. "Effects of orbital forcing on atmosphere and ocean heat transports in Holocene and Eemian climate simulations with a comprehensive Earth system model." Climate of the Past Discussions 5, no. 5 (2009): 2311–41. http://dx.doi.org/10.5194/cpd-5-2311-2009.

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Abstract. Orbital forcing does not only exert direct insolation effects but also alters climate indirectly through feedback mechanisms that modify atmosphere and ocean dynamics and meridional heat and moisture transfers. We investigate the regional effects of these changes by detailed analysis of atmosphere and ocean circulation and heat transports in a coupled atmosphere-ocean-sea ice-biosphere general circulation model (ECHAM5/JSBACH/MPI-OM). We perform long term quasi equilibrium simulations under pre-industrial, mid-Holocene (6000 years before present – yBP), and Eemian (125 000 yBP) orbit

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33

Deininger, Michael, Martin Werner, and Frank McDermott. "North Atlantic Oscillation controls on oxygen and hydrogen isotope gradients in winter precipitation across Europe; implications for palaeoclimate studies." Climate of the Past 12, no. 11 (2016): 2127–43. http://dx.doi.org/10.5194/cp-12-2127-2016.

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Abstract. Winter (October to March) precipitation δ18OP and δDP values in central Europe correlate with the winter North Atlantic Oscillation index (wNAOi), but the causal mechanisms remain poorly understood. Here we analyse the relationships between precipitation-weighted δ18OP and δDP datasets (δ18Opw and δDpw) from European GNIP and ANIP stations and the wNAOi, with a focus on isotope gradients. We demonstrate that longitudinal δ18Opw and δDpw gradients across Europe (“continental effect”) depend on the wNAOi state, with steeper gradients associated with more negative wNAOi states. Changing

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34

Fischer, N., and J. H. Jungclaus. "Effects of orbital forcing on atmosphere and ocean heat transports in Holocene and Eemian climate simulations with a comprehensive Earth system model." Climate of the Past 6, no. 2 (2010): 155–68. http://dx.doi.org/10.5194/cp-6-155-2010.

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Abstract. Orbital forcing does not only exert direct insolation effects, but also alters climate indirectly through feedback mechanisms that modify atmosphere and ocean dynamics and meridional heat and moisture transfers. We investigate the regional effects of these changes by detailed analysis of atmosphere and ocean circulation and heat transports in a coupled atmosphere-ocean-sea ice-biosphere general circulation model (ECHAM5/JSBACH/MPI-OM). We perform long term quasi equilibrium simulations under pre-industrial, mid-Holocene (6000 years before present – yBP), and Eemian (125 000 yBP) orbi

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35

Pató, Zsuzsanna Anna, Tibor Standovár, Mariusz Gałka, et al. "Exposure matters: Forest dynamics reveal an early Holocene conifer refugium on a north facing slope in Central Europe." Holocene 30, no. 12 (2020): 1833–48. http://dx.doi.org/10.1177/0959683620950452.

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Although several studies provide a broad overview of vegetation changes in the Carpathian Basin during the Holocene, stand-scale vegetation changes are lesser known because of the rarity of suitable sampling sites. In this study we investigated the sediment of a small closed-canopy site (Nagy-forrás forest hollow, 685 m a.s.l., 0.1 ha), located in the Mátra Mountains, on the north facing slope of Kékes (1014 m a.s.l.). We carried out detailed pollen, conifer stomata and plant macrofossil analyses, as well as radiocarbon dating to examine Late Glacial and Holocene dynamics of vegetation develop

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36

Edwards, Kevin J., and Glen M. MacDonald. "Holocene palynology: II human influence and vegetation change." Progress in Physical Geography: Earth and Environment 15, no. 4 (1991): 364–91. http://dx.doi.org/10.1177/030913339101500402.

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Much palynological research has focused upon the role of humans in influencing the development of vegetation. This continues to be the case in Europe and anthropogenic studies in pollen analysis now extend to most parts of the world. An attempt is made to present some of the major research published between 1985 and mid-1991. The material selected represents a broad range of palynological applications and geographical areas. Methodological aspects include fine resolution, spatial and absolute pollen studies. Area studies concentrate upon Europe (with particular emphasis on the Corylus maximum,

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37

Linseele, Veerle. "SIZE AND SIZE CHANGE OF THE AFRICAN AUROCHS DURING THE PLEISTOCENE AND HOLOCENE." Journal of African Archaeology 2, no. 2 (2004): 165–85. http://dx.doi.org/10.3213/1612-1651-10026.

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Several assumptions on the size of the African aurochs have been tested primarily using measurements assembled from the literature. During the Holocene, the African aurochs was indeed smaller than its European and Near Eastern cousins and it appears also to have been more gracile. The available African aurochs measurements of this period probably derive mostly from male animals, since many females may have been misidentified as domestic cattle. Therefore, the degree of sexual dimorphism remains unknown, although iconographic evidence suggests that it may have been marked. Male Holocene aurochs

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38

Huntley, Brian. "Dissimilarity Mapping Between Fossil and Contemporary Pollen Spectra in Europe for the Past 13,000 Years." Quaternary Research 33, no. 3 (1990): 360–76. http://dx.doi.org/10.1016/0033-5894(90)90062-p.

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AbstractThe degree of analogy between fossil and contemporary pollen spectra in Europe has been investigated using the chord-distance dissimilarity measure. No-analog pollen spectra represent vegetation without a modern analog and hence, by inference, represent macroclimatic conditions different from any occurring in the region today. Such spectra have minimum chord distances that exceed a threshold value assessed using contemporary samples from the same and different vegetation u units. Contoured maps of minimum chord distance portray the changing patterns of analogous and no-analog pollen sp

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39

Aldhouse-Green, Stephen, Paul Pettitt, and Christopher Stringer. "Holocene humans at Pontnewydd and Cae Gronw caves." Antiquity 70, no. 268 (1996): 444–47. http://dx.doi.org/10.1017/s0003598x00083423.

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Pontnewydd, in north Wales, is known as a rare Middle Pleistocene site in northern Europe with human remains. Radiocarbon AMS dates identify human specimens, deriving from later use of the cave at Pontnewydd and its neighbour Cae Gronw, that have no part in its earlier story.

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40

Bartosiewicz, László, and Janez Dirjec. "Camels in antiquity: Roman Period finds from Slovenia." Antiquity 75, no. 288 (2001): 279–85. http://dx.doi.org/10.1017/s0003598x00060919.

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Camels were not native to Europe during the Holocene and were evidently imported by conquering peoples. The discovery of camel bones at two sites in Slovenia is an important contribution to understanding the distribution and function of these animals during the Roman Imperial Period.

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41

Cullen, Tracey. "Mesolithic mortuary ritual at Franchthi Cave, Greece." Antiquity 69, no. 263 (1995): 270–89. http://dx.doi.org/10.1017/s0003598x00064681.

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Mesolithic sites are rare in the Aegean, and Mesolithic burials are uncommon throughout Europe. The Mesolithic human remains from Franchthi Cave, that remarkable, deeply stratified site in southern Greece, offer a rare glimpse into the burial practices of early Holocene hunter-gatherers of the Mediterranean.

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42

Rushby, Greg T., Geoff T. Richards, W. Roland Gehrels, William P. Anderson, Mark D. Bateman, and William H. Blake. "Testing the mid-Holocene relative sea-level highstand hypothesis in North Wales, UK." Holocene 29, no. 9 (2019): 1491–502. http://dx.doi.org/10.1177/0959683619854513.

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Accurate Holocene relative sea-level curves are vital for modelling future sea-level changes, particularly in regions where relative sea-level changes are dominated by isostatically induced vertical land movements. In North Wales, various glacial isostatic adjustment (GIA) models predict a mid-Holocene relative sea-level highstand between 4 and 6 ka, which is unsubstantiated by any geological sea-level data but affects the ability of geophysical models to model accurately past and future sea levels. Here, we use a newly developed foraminifera-based sea-level transfer function to produce a 3300

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43

Mikkelsen, Naja, Antoon Kuijpers, and Jette Arneborg. "The Norse in Greenland and late Holocene sea-level change." Polar Record 44, no. 1 (2008): 45–50. http://dx.doi.org/10.1017/s0032247407006948.

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ABSTRACTNorse immigrants from Europe settled in southern Greenland in around AD 985 and managed to create a farming community during the Medieval Warm Period. The Norse vanished after approximately 500 years of existence in Greenland leaving no documentary evidence concerning why their culture foundered. The flooding of fertile grassland caused by late Holocene sea-level changes may be one of the factors that affected the Norse community. Holocene sea-level changes in Greenland are closely connected with the isostatic response of the Earth's crust to the behaviour of the Greenlandic ice sheet.

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44

Brewer, S., J. Guiot, and F. Torre. "Mid-Holocene climate change in Europe: a data-model comparison." Climate of the Past Discussions 2, no. 6 (2006): 1155–86. http://dx.doi.org/10.5194/cpd-2-1155-2006.

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Abstract. We present here a comparison between the outputs of a set of 25 climate models run for the mid-Holocene period (6 ka BP) with a set of palaeo-climate reconstructions from over 400 fossil pollen sequences distributed across the European continent. Three climate parameters were available (moisture availability, temperature of the coldest month and growing degree days), which were then grouped together using cluster analysis to provide regions of homogenous climate change. Each model was then investigated to see if it reproduced 1) the same directions of change and 2) the correct locati

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45

Chambers, Frank M., and JRG Daniell. "Peatland archives of late-Holocene climate change in northern Europe." PAGES news 18, no. 1 (2010): 4–6. http://dx.doi.org/10.22498/pages.18.1.4.

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Satkūnas, Jonas, and Miglė Stančikaitė. "Pleistocene and Holocene palaeoenvironments and recent processes across NE Europe." Quaternary International 207, no. 1-2 (2009): 1–3. http://dx.doi.org/10.1016/j.quaint.2009.07.003.

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Vannière, Boris. "Quantitative and regional reconstructions of Holocene fire history in Europe." Quaternary International 279-280 (November 2012): 516. http://dx.doi.org/10.1016/j.quaint.2012.08.1783.

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PUZACHENKO, Andrei Yurievich, and Anastasia Konstantinovna MARKOVA. "Mammal diversity during the Pleistocene-Holocene transition in Eastern Europe." Integrative Zoology 9, no. 4 (2014): 461–70. http://dx.doi.org/10.1111/1749-4877.12059.

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García-Artola, Ane, Pierre Stéphan, Alejandro Cearreta, Robert E. Kopp, Nicole S. Khan, and Benjamin P. Horton. "Holocene sea-level database from the Atlantic coast of Europe." Quaternary Science Reviews 196 (September 2018): 177–92. http://dx.doi.org/10.1016/j.quascirev.2018.07.031.

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Dabkowski, Julie. "The late-Holocene tufa decline in Europe: Myth or reality?" Quaternary Science Reviews 230 (February 2020): 106141. http://dx.doi.org/10.1016/j.quascirev.2019.106141.

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