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 development. The site dates back to ca. 15,500 cal yr BP, when open boreal forests and wet tundra-like habitats occurred around the hollow. Closed forest cover developed around 14,600 cal yr BP, when a boreal European larch-Swiss stone pine (Larix decidua-Pinus cembra) forest surrounded the hollow. This vegetation type remained stable up to 7700 cal yr BP. We observed a hiatus between 7700 and 2710 cal yr BP, followed by a beech (Fagus sylvatica) dominated mixed temperate deciduous forest. Our results confirmed that the area was covered by a primary forest, as human influence was visible only from 175 cal yr BP. The relatively long lasting persistence of Pinus cembra in the Holocene at relatively low altitude was documented, which has never been found in Holocene sediments in the Pre-Carpathians before. We hypothesize that the north facing slope acted as a cold-stage refugium in the Early Holocene and could play the same role for the present-day beech forest that is threatened by recent climate change.
AugspurgerCK (2013) Reconstructing patterns of temperature, phenology, and frost damage over 124 years: Spring damage risk is increasing. Ecology94(1): 41–50.
BennettKDWillisKJ (2001) Pollen. In: SmolJPBirksHJBLastWM, et al. (eds) Tracking Environmental Change Using Lake Sediments: Terrestrial, Algal, and Siliceous Indicators. Dordrecht: Springer Netherlands, pp. 5–32.
4.
BerggrenG (1981) Atlas of Seeds. Part 3. Salicaceae-Cruciferae. Stockholm: Swedish Museum of Natural History.
5.
BeugH-J (2004) Leitfaden der Pollenbestimmung für Mitteleuropa und angrenzende Gebiete. München: Verlag Dr. Friedrich Pfeil.
6.
BirksHH (2001) 4. Plant macrofossils. In: SmolJPBirksHJBLastWM (eds) Tracking Environmental Change Using Lake Sedinments. Volume 3: Terrestial, Algal, and Siliceous Indicators. Dordrecht: Kluwer Academic Publishers, pp. 49–74.
7.
BirksHH (2003) The importance of plant macrofossils in the reconstruction of Lateglacial vegetation and climate: Examples from Scotland, western Norway, and Minnesota, USA. Quaternary Science Reviews22(5–7): 453–473.
8.
BirksHH (2007) Plant Macrofossil Introduction. In: Encyclopedia of Quaternary Science3. Elsevier, pp. 2266–2288.
9.
BirksHHBirksHJB (2006) Multi-proxy studies in palaeolimnology. Vegetation History and Archaeobotany15(4): 235–251.
10.
BirksHJB (1996) Contributions of Quaternary palaeoecology to nature conservations. Journal of Vegetation Science7: 89–98.
11.
BirksHJBBirksH (2000) Future uses of pollen analysis must include plant macrofossils. Journal of Biogeography27(1): 31–35.
12.
BirksHJBWillisKJ (2008) Alpines, trees, and refugia in Europe. Plant Ecology & Diversity1(2): 147–160.
13.
BíróK (1984) Őskori leletek a Mátra hegységből. AGRIA20: 5–11.
14.
BiszakEKulovitsHBiszakS, et al. (2014) Cartographic heritage of the Habsburg Empire on the web: the MAPIRE initiative.:6.
15.
BjörkmanLFeurdeanAWohlfarthB (2003) Late-glacial and Holocene forest dynamics at Steregoiu in the Gutaiului Mountains, Northwest Romania. Review of Palaeobotany and Palynology124(1–2): 79–111.
16.
BlaauwMChristenJA (2011) Flexible paleoclimate age-depth models using an autoregressive gamma process. Bayesian Analysis6(3): 457–474.
17.
BodnariucABouchetteADedoubatJJ, et al. (2002) Holocene vegetational history of the Apuseni mountains, central Romania. Quaternary Science Reviews21(12–13): 1465–1488.
18.
BojnanskýVFargašováA (2007) Atlas of Seeds and Fruits of Central and East-European Flora. The Carpathian Mountains Region. Dordrecht: Springer Netherlands.
19.
BradshawR (2007) Stand-Scale Palynology. Elsevier, pp. 2535–2543.
20.
BradshawRHW (1988) Spatially-precise studies of forest dynamics. In: HuntleyBWebbT (eds) Vegetation History. Dordrecht: Springer Netherlands, pp. 725–751.
21.
BradshawRHWKitoNGieseckeT (2010) Factors influencing the Holocene history of Fagus. Forest Ecology and Management259(11): 2204–2212.
22.
BuczkóKMagyariEKBitušíkP, et al. (2009) Review of dated Late Quaternary palaeolimnological records in the Carpathian Region, east-central Europe. Hydrobiologia631(1): 3–28.
23.
CalcoteR (1995) Pollen source area and pollen productivity: Evidence from forest hollows. The Journal of Ecology83(4): 591.
24.
CappersRTBekkerRMJansJE (2012) Digital Seed Atlas of the Netherlands. 1st ed. Groningen Archaeological Studies 4. Barkhuis.
25.
CasalegnoSAmatulliGCamiaA, et al. (2010) Vulnerability of Pinus cembra L. in the Alps and the Carpathian mountains under present and future climates. Forest Ecology and Management259(4): 750–761.
26.
CaudulloGde RigoD (2016) Pinus cembra in Europe: Distribution, habitat, usage and threats. In: San-Miguel-AyanzJde RigoDCaudulloG, et al. (eds) European Atlas of Forest Tree Species. Luxembourg: Publications Office of the European Union.
27.
ClearJLSeppäHKuosmanenN, et al. (2015) Holocene stand-scale vegetation dynamics and fire history of an old-growth spruce forest in southern Finland. Vegetation History and Archaeobotany24(6): 731–741.
28.
CzájlikP (2009) Kékes-Észak erdőrezervátum és térségének története: az őserdő fragmentum fennmaradása. In: Az erdőrezervátum kutatás eredményei (Results of Forest Reserve Research in Hungary). ER 3. Vácrátót: MTA Ökológiai és Botanikai Kutatóintézet, pp. 7–82.
29.
CzerwińskiSMargielewskiWłodzimierzGałkaMariusz, et al. (2019) Late Holocene transformations of lower montane forest in the Beskid Wyspowy Mountains (Western Carpathians, Central Europe): a case study from Mount Mogielica. Paly-nology44(2): 355–368.
30.
CzúczBGálhidyLMátyásC (2013) A bükk és a kocsánytalan tölgy elterjedésének szárazsági határa. Erdészettudományi Közlemények3(1): 39–53.
31.
DávidL (1992) A Mátra északi lejtőinek csuszamlásos felszínfejlődése. Folia historico-naturalia Musei Matraensis17: 9–26.
32.
DénesJNovákiG (2010) A Mátra őskori és középkori várai. In: BarázC (ed.) A Mátrai Tájvédelmi Körzet. Heves és Nógrád határán. A Bükki Nemzeti Park Igazgatóság Monográfiái 4. Eger: Bükki Nemzeti Park Ig., pp. 239–250.
33.
DobrowskiSZ (2011) A climatic basis for microrefugia: the influence of terrain on climate: A Climatic basis of microrefugia. Global Change Biology17(2): 1022–1035.
34.
DomboróczkiLBudekADaróczi-SzabóL, et al. (2016) Excavation along the easternmost frontier of the LBK in NE-Hungary at Apc-Berekalja I (2008–2009). Archaeologiai Értesítő141(1): 1–27.
35.
EliasSA (2007) Encyclopedia of Quaternary Science. Elsevier Science.
36.
FangJLechowiczMJ (2006) Climatic limits for the present distribution of beech (Fagus L.) species in the world. Journal of Biogeography33(10): 1804–1819.
37.
FărcaşSTanţăuIMîndrescuM, et al. (2013) Holocene vegetation history in the Maramureş Mountains (Northern Romanian Carpathians). Quaternary International293: 92–104.
38.
FeketeGMolnárZsMagyariE, et al. (2014) A new framework for understanding Pannonian vegetation patterns: regularities, deviations and uniqueness. Community Ecology15(1): 12–26.
39.
FeurdeanA (2005) Holocene forest dynamics in northwestern Romnania. The Holocene15(3): 435–446.
40.
FeurdeanA (2010) Forest conservation In a changing world: natural or cultural? Example from the Western Carpathians forests, Romania. Studia Universitatis Babes-Bolyai, Geologia55(1): 45–48.
41.
FeurdeanATanţăuIFărcaşS (2011) Holocene variability in the range distribution and abundance of Pinus, Picea abies, and Quercus in Romania; implications for their current status. Quaternary Science Reviews30(21–22): 3060–3075.
42.
FeurdeanALiakkaJVannièreB, et al. (2013) 12,000-Years of fire regime drivers in the lowlands of Transylvania (Central-Eastern Europe): a data-model approach. Quaternary Science Reviews81: 48–61.
43.
FeurdeanAGałkaMTanţăuI, et al. (2016) Tree and timberline shifts in the northern Romanian Carpathians during the Holocene and the responses to environmental changes. Quaternary Science Reviews134: 100–113.
44.
FeurdeanAPerşoiuATanţăuI, et al. (2014) Climate variability and associated vegetation response throughout Central and Eastern Europe (CEE) between 60 and 8 ka. Quaternary Science Reviews106: 1–19.
45.
FodorL (2010) A Mátravidék régészeti lelőhelyei, leletei. In: BarázC (ed.) A Mátrai Tájvédelmi Körzet. Heves és Nógrád határán. A Bükki Nemzeti Park Igazgatóság Monográfiái 4. Eger: Bükki Nemzeti Park Ig., pp. 229–238.
46.
GałkaMTanţăuIFeurdeanA (2017) Plant succession in a peatland in the Eastern Carpathian Mts. (CE Europe) during the last 10,200 years: Implications for peatland development and palaeoclimatic research. Review of Palaeobotany and Palynology244: 203–216.
47.
GałkaMFeurdeanAHutchinsonS, et al. (2018) Response of a spring-fed fen ecosystem in Central Eastern Europe (NW Romania) to climate changes during the last 4000 years: A high resolution multi-proxy reconstruction. Palaeogeography, Palaeoclimatology, Palaeoecology504: 170–185.
48.
GaramszegiBKernZ (2014) Climate influence on radial growth of Fagus sylvatica growing near the edge of its distribution in Bükk Mts., Hungary. Dendrobiology72: 93–102.
49.
GardnerAR (2002) Neolithic to Copper Age woodland impacts in northeast Hungary? Evidence from the pollen and sediment chemistry records. The Holocene12(5): 541–553.
50.
GavinDGFitzpatrickMCGuggerPF, et al. (2014) Climate refugia: joint inference from fossil records, species distribution models and phylogeography. New Phytologist204(1): 37–54.
51.
GeigerRBouyoucosGJ (1951) The climate near the ground. American Journal of Physics19: 192–192.
52.
GieseckeTHicklerTKunkelT, et al. (2006) Towards an understanding of the Holocene distribution of Fagus sylvatica L. Journal of Biogeography34(1): 118–131. DOI:
53.
GregussP (1940) Kritikai megjegyzések a magyarországi prehisztorikus faszenek meghatározásaira. Botanikai Közlemények37(3–4.): 189–195.
GrindeanRTanţăuIFărcaşS, et al. (2014) Middle to Late Holocene vegetation shifts in the NW Transylvanian lowlands (Romania). Studia Universitatis Babes-Bolyai, Geologia59(1–2): 29–37.
56.
GrindeanRFeurdeanAHurduB, et al. (2015) Lateglacial/Holocene transition to mid-Holocene: Vegetation responses to climate changes in the Apuseni Mountains (NW Romania). Quaternary International388: 76–86.
57.
GrindeanRTanţăuIFeurdeanA (2019) Linking vegetation dynamics and stability in the old-growth forests of Central Eastern Europe: Implications for forest conservation and management. Biological Conservation229: 160–169.
58.
GutayM (2016) Előzetes jelentés az Apc-Somlyó 5-6. és 9. sz. felső paleolitikus lelőhelyek tervásatásairól. AGRIAXLIX.: 17–28.
59.
HájkováPPetrLHorsákM, et al. (2015) Interstadial inland dune slacks in south-west Slovakia: a multi-proxy vegetation and landscape reconstruction. Quaternary International357: 314–328.
60.
HeiriOLotterAFLemckeG (2001) Loss on ignition as a method for estimating organic and carbonate content in sediments: reproducibility and comparability of results. Journal of Paleolimnology (25): 101–110.
61.
HermannMJánossyDStieberJ, et al. (1956) Ausgrabungen in der Petényi- und Peskő-Höhle. Folia Archeologica8: 3–22.
62.
HofstetterSTinnerWValsecchiV, et al. (2006) Lateglacial and Holocene vegetation history in the Insubrian Southern Alps—New indications from a small-scale site. Vegetation History and Archaeobotany15(2): 87–98.
63.
HöhnMGugerliFAbranP, et al. (2009) Variation in the chloroplast DNA of Swiss stone pine (Pinus cembra L.) reflects contrasting post-glacial history of populations from the Carpathians and the Alps. Journal of Biogeography36(9): 1798–1806.
64.
HuntleyB (1990) European vegetation history: Palaeovegetation maps from pollen data - 13 000 yr BP to present. Journal of Quaternary Science5(2): 103–122.
65.
JacksonSTHobbsRJ (2009) Ecological restoration in the light of ecological history. Science325(5940): 567–569.
66.
JacksonSTSaxDF (2010) Balancing biodiversity in a changing environment: extinction debt, immigration credit and species turnover. Trends in Ecology & Evolution25(3): 153–160.
67.
JakabGSümegiP (2004) A lágyszárú növények tõzegben található maradványainak határozója mikroszkópikus bélyegek alapján. KitaibeliaIX.(1): 93–129.
68.
JakabGSümegiP (2005) A nagybárkányi Nádas-tó kialakulása a makrofosszília vizsgálatok alapján (Cserhát, Észak-Magyarország). KitaibeliaX(1): 104–114.
69.
JakabGSümegiP (2010) Preliminary data on the bog surface wetness from the Sirok Nyírjes-tó peat bog, Mátra Mts, Hungary. Central European Geology53(1): 43–65.
JamrichováESzabóPHédlR, et al. (2013) Continuity and change in the vegetation of a Central European oakwood. The Holocene23(1): 46–56.
72.
JamrichováEHédlRKolářJ, et al. (2017) Human impact on open temperate woodlands during the middle Holocene in Central Europe. Review of Palaeobotany and Palynology245: 55–68.
73.
JankovskáV (1984) Late Glacial Finds of Pinus cembra L. in the Lubovnianská kotlina Basin. Folia Geobotanica et Phytotaxonomica19(3): 323–325.
74.
JankovskáV (1988) A reconstruction of the Late-Glacial and Early-Holocene evolution of forest vegetation in the Poprad Basin, Czechoslovakia. Folia Geobotanica & Phytotaxonomica23(3): 303–319.
75.
JánossyD (1961) Vorläufige ergebnisse der Ausgrabunge in der felnische Rejtek 1. (Bükk Gebirge, Gem. Répáshuta). Karszt- és Barlangkutatás3: 49–58.
76.
JasinskiKAngelstamP (2002) Long-term differences in the dynamics within a natural forest landscapeÐconsequences for management. Forest Ecology and Management161(1–3): 1–11.
JuhászI (2007) Comparison and correlation of four pollen sequences from the Little Balaton region (Alsópáhok, Fönyed, Keszthely, Zalavár). In: ZatykóCJuhászISümegiP (eds) Environmental Archaeology in Transdanubia. Budapest, Hungary: Archaeological Institute of the Hungarian Academy of Sciences, pp. 36–51.
79.
KatzNKatzSKipianiM (1965) Atlas and Keys of Fruits and Seeds Occurring in the Quaternary Deposits of the USSR. Moskow: Publishing House Nauka.
80.
KołaczekPMargielewskiWGałkaM, et al. (2017) Five centuries of the Early Holocene forest development and its interactions with palaeoecosystem of small landslide lake in the Beskid Makowski Mountains (Western Carpathians, Poland) — High resolution multi-proxy study. Review of Palaeobotany and Palynology244: 113–127.
81.
KörnerC (2003) Alpine Plant Life: Functional Plant Ecology of High Mountain Ecosystems. 2nd ed.Berlin ; New York: Springer.
82.
KrapiecMMargielewskiW (2003) Reconstruction of paleoclimatic changes registered in Kaletowa landslide (Beskid Makowski Mts. Outer Carpathians, South Poland) on basis on the basis of sedimentological and dendrochronological records. Folia Quaternalia74: 17–33.
83.
KrąpiecMMargielewskiWKorzeńK, et al. (2016) Late Holocene palaeoclimate variability: The significance of bog pine dendrochronology related to peat stratigraphy. The Puścizna Wielka raised bog case study (Orawa – Nowy Targ Basin, Polish Inner Carpathians). Quaternary Science Reviews148: 192–208.
84.
KunešPAbrahamV (2017) History of Czech Vegetation Since the Late Pleistocene. In: ChytrýMDanihelkaJKaplanZ, et al. (eds) Flora and Vegetation of the Czech Republic. Cham: Springer International Publishing, pp. 193–227.
85.
KunešPPelánkováBChytrýM, et al. (2008) Interpretation of the last-glacial vegetation of eastern-central Europe using modern analogues from southern Siberia. Journal of Biogeography35(12): 2223–2236.
86.
LángVFuchsMWaltnerI, et al. (2013) Soil taxonomic distance, a tool for correlation: As exemplified by the Hungarian Brown Forest Soils and related WRB Reference Soil Groups. Geoderma192: 269–276.
87.
LatałowaMvan der KnaapWO (2006) Late Quaternary expansion of Norway spruce Picea abies (L.) Karst. in Europe according to pollen data. Quaternary Science Reviews25(21–22): 2780–2805.
88.
LenoirJHattabTPierreG (2017) Climatic microrefugia under anthropogenic climate change: implications for species redistribution. Ecography40(2): 253–266.
89.
LeuschnerCEllenbergH (2017) Ecology of Central European Forests: Vegetation Ecology of Central Europe, Volume I. Cham: Springer International Publishing.
90.
LindbladhMBrunetJHannonG, et al. (2007) Forest history as a basis for ecosystem restoration?A multidisciplinary case study in a south Swedish temperate landscape. Restoration Ecology15(2): 284–295.
91.
MacleanIMDHopkinsJJBennieJ, et al. (2015) Microclimates buffer the responses of plant communities to climate change: Community responses to climate change. Global Ecology and Biogeography24(11): 1340–1350.
92.
MagriD (2008) Patterns of post-glacial spread and the extent of glacial refugia of European beech (Fagus sylvatica). Journal of Biogeography35(3): 450–463.
93.
MagriDVendraminGGCompsB, et al. (2006) A new scenario for the Quaternary history of European beech populations: Palaeobotanical evidence and genetic consequences. New Phytologist171(1): 199–221.
94.
MagyariEVinczeIOrbánI, et al. (2018) Timing of major forest compositional changes and tree expansions in the Retezat Mts during the last 16,000 years. Quaternary International477: 40–58.
95.
MagyariEK (2002) Holocene biogeography of Fagus sylvatica L. and Carpinus betulus L. in the Carpathian-Alpine Region. Folia historico-naturalia Musei Matraensis (26): 15–35.
96.
MagyariEK (2015) A Kárpát-medence és DK-Európa késő pleniglaciális és holocén vegetációfejlődése különös tekintettel a gyors felmelegedési és lehűlési hullámokra mutatott vegetációs válaszokra. Doctor of the Hungarian Academy of Science. Thesis. MTA-MTM-ELTE, Budapest. Available at: http://real-d.mtak.hu/800/.
97.
MagyariEKChapmanJCPassmoreDG, et al. (2010) Holocene persistence of wooded steppe in the Great Hungarian Plain. Journal of Biogeography37(5): 915–935.
98.
MagyariEKJakabGBálintM, et al. (2012) Rapid vegetation response to Lateglacial and early Holocene climatic fluctuation in the South Carpathian Mountains (Romania). Quaternary Science Reviews35: 116–130.
99.
MagyariEKJakabGRudnerZE, et al. (1999) Palynological and plant macrofossil data on Late Pleistocene short-term climatic oscillations in North-Eastern Hungary. Acta Palaeobotanica2(Suppl.): 491–502.
100.
MagyariEKJakabGSümegiP, et al. (2008) Holocene vegetation dynamics in the Bereg Plain, NE Hungary - the Báb-tava pollen and plant macrofossil record. ACTA GGM DEBRECINA3(Geology, Geomorphology, Physical Geography Series): 33–50.
101.
MagyariEKSümegiPBraunM, et al. (2001) Retarded wetland succession: Anthropogenic and climatic signals in a Holocene peat bog profile from north-east Hungary. Journal of Ecology (89): 1019–1032.
102.
MagyariEKVeresDWennrichV, et al. (2014) Vegetation and environmental responses to climate forcing during the Last Glacial Maximum and deglaciation in the East Carpathians: attenuated response to maximum cooling and increased biomass burning. Quaternary Science Reviews106: 278–298.
103.
MargielewskiWMichczyńskiAObidowiczA (2010) Records of the middle - and late Holocene palaeoenvironmental changes in the Pcim-Sucha landslide peat bogs (Beskid Makowski Mts., Polish Outer Carpathians). Geochronometria35: 11–23.
104.
MargielewskiWObidowiczAPelcS (2003) Late Glacial-Holocene peat bog on Koton Mt. and its significance for reconstruction of paleaoenvironment in Western Outer Carpathians (Beskid Makowski Range, south Poland). Folia Quaternalia74: 35–56.
105.
MátyásCBerkiICzúczB, et al. (2010) Future of beech in southeast Europe from the perspective of evolutionary ecology. Acta Silvatica et Lignaria Hungarica6: 91–110.
106.
Metzner-NebelsickC (2012) Social transition and spatial organisation: The problem of the early iron age occupation of the strongholds in northeast Hungary. In: AnreiterPBánffyEBartosiewiczL, et al. (eds) Archaeological, Cultural and Linguistic Heritage. Archaeolingua 25. Budapest: Archaeolingua Alapítvány, pp. 425–448.
Moskal-del HoyoMLityńska-ZającMRaczkyP, et al. (2018) The character of the Atlantic oak woods of the Great Hungarian Plain. Quaternary International463: 337–351.
109.
NovákJAbrahamVŠídaP, et al. (2019) Holocene forest transformations in sandstone landscapes of the Czech Republic: Stand-scale comparison of charcoal and pollen records. The Holocene: 095968361985451.
110.
ÓdorP (2000) Description of the bryoflora and bryophyte vegetation of Kékes North Forest Reserve in Mátra mountains (N-Hungary). Kitaibelia5: 115–123.
111.
OrbánIBirksHHVinczeI, et al. (2018) Treeline and timberline dynamics on the northern and southern slopes of the Retezat Mountains (Romania) during the late glacial and the Holocene. Quaternary International477: 59–78.
112.
Overballe-PetersenMVBradshawRHW (2011) The selection of small forest hollows for pollen analysis in boreal and temperate forest regions. Palynology35(1): 146–153.
113.
Overballe-PetersenMVNielsenABHannonGE, et al. (2013) Long-term forest dynamics at Gribskov, eastern Denmark with early-Holocene evidence for thermophilous broadleaved tree species. The Holocene23(2): 243–254.
114.
Overballe-PetersenMVRaulund-RasmussenKButtenschønRM, et al. (2014) The forest Gribskov, Denmark: lessons from the past qualify contemporary conservation, restoration and forest management. Biodiversity and Conservation23(1): 23–37.
115.
PackhamJRThomasPAAtkinsonMD, et al. (2012) Biological Flora of the British Isles: Fagus sylvatica. Journal of Ecology100(6): 1557–1608.
116.
ParshallT (1999) Documenting forest stand invasion: fossil stomata and pollen in forest hollows. Canadian Journal of Botany77(10): 1529–1538.
117.
ParshallTCalcoteR (2001) Effect of pollen from regional vegetation on stand-scale forest reconstruction. The Holocene11(1): 81–87.
118.
PetitRJHuFSDickCW (2008) Forests of the past: A window to future changes. Science320(5882): 1450–1452.
119.
PokornýPNovákJŠídaP, et al. (2017) I. Vývoj vegetace severočeských pískovcových území od pozdního glaciálu po střední holocén [Vegetation development of northern-Bohemian sandstone areas since the Late Glacial to the Middle Holocene]. In: SvobodaJ (ed.) Mezolit Severních Čech 2 [Mesolithic of Northern Bohemia 2]. Brno: Archeologický ústav AV, pp. 11–37.
120.
ProvanJBennettK (2008) Phylogeographic insights into cryptic glacial refugia. Trends in Ecology & Evolution23(10): 564–571.
121.
RamseyBC (2009) Bayesian Analysis of Radiocarbon Dates. Radiocarbon51(1): 337–360.
122.
ReimerPJBardEBaylissA, et al. (2013) IntCal13 and Marine13 radiocarbon age calibration curves 0 - 50000 years cal BP. Radiocarbon55(4): 1869–1887.
123.
RigbyJRPorporatoA (2008) Spring frost risk in a changing climate. Geophysical Research Letters35(12): 1–5.
124.
RudnerZESümegiP (2001) Recurring Taiga forest-steppe habitats in the Carpathian Basin in the Upper Weichselian. Quaternary International76–77: 177–189.
125.
SabatiniFMBurrascanoSKeetonWS, et al. (2018) Where are Europe’s last primary forests?EsslF (ed.) Diversity and Distributions24(10): 1426–1439.
126.
Salamon-AlbertÉLőrinczPPaulerG, et al. (2016) Drought stress distribution responses of continental beech forests at their xeric edge in central Europe. Forests7(12): 298.
127.
SaltréFSaint-AmantRGrittiES, et al. (2013) Climate or migration: What limited European beech post-glacial colonization? European beech post-glacial migration. Global Ecology and Biogeography22(11): 1217–1227.
128.
SárkányS (1937) A magyarországi ősemberkutatás a növénytan tükrében. orsz. Ev. Tanáregy. Évk1937–1938: 1–9.
129.
StandovárTHorváthSAszalósR (2017) Temporal changes in vegetation of a virgin beech woodland remnant: stand-scale stability with intensive fine-scale dynamics governed by stand dynamic events. Nature Conservation17: 35–56.
130.
StewartJRListerAMBarnesI, et al. (2010) Refugia revisited: Individualistic responses of species in space and time. Proceedings of the Royal Society B: Biological Sciences277(1682): 661–671.
131.
StieberJ (1967) A magyarországi felsöpleisztocén vegetáció-története az anthrakotómiai eredmények (1957-IG) Tükrében. Földtani Közlöny97(3): 308-317.
132.
StieberJ (1969) A hazai későglaciális vegetációtörténet antrakotómiai vizsgálatok alapján. Földtani Közlöny99(2): 188–193.
133.
SuggittAJGillinghamPKHillJK, et al. (2011) Habitat microclimates drive fine-scale variation in extreme temperatures. Oikos120(1): 1–8.
134.
SuggittAJWilsonRJIsaacNJB, et al. (2018) Extinction risk from climate change is reduced by microclimatic buffering. Nature Climate Change8(8): 713–717.
135.
SümegiPNáfrádiK (2015) A radiocarbon-dated cave sequence and the Pleistocene/Holocene transition in Hungary. Open Geosciences7(1): 783–798.
136.
SümegiPPersaitsGGulyásS (2012) Woodland-grassland ecotonal shifts in environmental mosaics: Lessons learnt from the environmental history of the Carpathian Basin (Central Europe) during the Holocene and the last ice age based on investigation of paleobotanical and mollusk remains. In: MysterRW (ed.) Ecotones between Forest and Grassland. New York, NY: Springer, pp. 17–57.
137.
SvenningJ-CNormandSKageyamaM (2008) Glacial refugia of temperate trees in Europe: insights from species distribution modelling. Journal of Ecology96(6): 1117–1127.
138.
SweeneyCA (2004) A key for the identification of stomata of the native conifers of Scandinavia. Review of Palaeobotany and Palynology128(3–4): 281–290.
139.
SykesMTPrenticeICCramerW (1996) A bioclimatic model for the potential distributions of north European tree species under present and future climates. Journal of Biogeography23(2): 203–233.
140.
SzabóJ (1992) Landslide processes and fonns in the Hungarian Moutains of volcanic origin. In: New Perspectives in Hungarian Geography. Studies in Geography in Hungary 27. Budapest, pp. 63–75.
141.
SzabóJ (1993) Vergleichende Untersuchung der Rutschungsprozesse in Ungarn. Berliner Geographische Arbeiten, Heft79(79): 133–161.
142.
SzabóJFélegyháziE (1997) Problems of landslide chronology in the Mátra mountains in Hungary. Eiszeitalter und Gegenwart120–128.
143.
TanţăuIGeantăAFeurdeanA, et al. (2014) Pollen nalysis from high altitude site in Rodna Mountains (Romania). Carpathian Journal of Earth and Environmental Sciences9(2): 23–30.
144.
TanţăuIFeurdeanADe BeaulieuJ-L, et al. (2014) Vegetation sensitivity to climate changes and human impact in the Harghita Mountains (Eastern Romanian Carpathians) over the past 15 000 years: vegetation changes in Hargitha Mountains. Journal of Quaternary Science29(2): 141–152.
145.
TímárGBiszakSSzékelyB, et al. (2010) Digitized maps of the Habsburg military surveys – overview of the project of ARCANUM Ltd. (Hungary). In: JobstM (ed.) Preservation in Digital Cartography. Berlin, Heidelberg: Springer Berlin Heidelberg, pp. 273–283.
146.
TóthEGyBede-FazekasÁVendraminGG, et al. (2019) Mid-Pleistocene and Holocene demographic fluctuation of Scots pine (Pinus sylvestris L.) in the Carpathian Mountains and the Pannonian Basin: Signs of historical expansions and contractions. Quaternary International504: 202–213.
147.
TóthMMagyariEKBuczkóK, et al. (2015) Chironomid-inferred Holocene temperature changes in the South Carpathians (Romania). The Holocene25(4): 569–582.
148.
Troels-SmithJ (1955) Karakterisering af lose jordarter. Characterization of unconsolidated sediments. Danmarks Geologiske Undersogelse (3): 39–73.
149.
VälirantaMKaakinenAKuhryP, et al. (2011) Scattered late-glacial and early Holocene tree populations as dispersal nuclei for forest development in north-eastern European Russia: Holocene forest development in north-eastern European Russia. Journal of Biogeography38(5): 922–932.
150.
Van GeelB (2006) Quaternary non-pollen palynomorphs. Review of Palaeobotany and Palynology141(vii–viii): 1–230.
151.
Van GeelBBohnckeSJPDeeH (1980) A palaeoecological study of an upper late glacial and holocene sequence from “de borchert”, The Netherlands. Review of Palaeobotany and Palynology31: 367–448.
152.
Van GeelBHallewasDPPalsJP (1983) A late holocene deposit under the Westfriese Zeedijk near Enkhuizen (Prov. of Noord-Holland, The Netherlands): Palaeoecological and archaeological aspects. Review of Palaeobotany and Palynology38(3–4): 269–335.
153.
VinczeIOrbánIBirksHH, et al. (2017) Holocene treeline and timberline changes in the South Carpathians (Romania): Climatic and anthropogenic drivers on the southern slopes of the Retezat Mountains. The Holocene27(11): 1613–1630.
154.
VojtkóASramkóGMagosG, et al. (2010) Növényvilág. In: BarázC (ed.) A Mátrai Tájvédelmi Körzet. Nógrád és Heves határán. A Bükki Nemzeti Park Igazgatóság Monográfiái 4. Eger: Bükki Nemzeti Park Ig., pp. 149–174.
155.
WagnerSLittTSánchez-GoñiM-F, et al. (2015) History of Larix decidua Mill. (European larch) since 130 ka. Quaternary Science Reviews124: 224–247.
156.
WiezikMJamrichováEHájkováP, et al. (2019) The last glacial and Holocene history of mountain woodlands in the southern part of the Western Carpathians, with emphasis on the spread ofFagus sylvatica. Palynology1–14.
157.
WillisKvan AndelT (2004) Trees or no trees? The environments of central and eastern Europe during the Last Glaciation. Quaternary Science Reviews23(23–24): 2369–2387.
158.
WillisKJAraújoMBBennettKD, et al. (2007) How can a knowledge of the past help to conserve the future? Biodiversity conservation and the relevance of long-term ecological studies. Philosophical Transactions of the Royal Society B: Biological Sciences362(1478): 175–187.
159.
WillisKJBennettKDBhagwatSA, et al. (2010) 4°C and beyond: What did this mean for biodiversity in the past?Systematics and Biodiversity8(1): 3–9.
160.
WillisKJBraunMSümegiP (1997) Does soil change cause vegetation change or vice versa? A temporal perspective from Hungary. Ecology78(3): 740–750.
161.
WillisKJSümegiPBraunM, et al. (1995) The late Quaternary environmental history of Bátorliget, NE Hungary. Paleogeography, Paleoclimatology, Paleoecology (118): 25–47.
162.
WillisKJSümegiPBraunM, et al. (1998) Prehistoric land degradation in Hungary: who, how and why?Antiquity72(275): 101–113.
163.
WillisKJRudnerESümegiP (2000) The full-glacial forests of central and southeastern Europe. Quaternary Research53(2): 203–213.
164.
ZhangKZhaoYGuoXL (2011) Conifer stomata analysis in paleoecological studies on the Loess Plateau: An example from Tianchi Lake, Liupan Mountains. Journal of Arid Environments75(11): 1209–1213.
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