<p>The objectives of this thesis are to establish a chronological framework for environmental changes during the last 15,000 years in northwest Romania, to reconstruct the vegetation development, and to evaluate the underlying processes for forest dynamics. Furthermore, an overview of earlier and ongoing pollenstratigraphic work in Romania is provided. </p><p>Sediments from two former crater lakes, Preluca Tiganului and Steregoiu, situated in the Gutaiului Mountains, on the western extremity of the Eastern Carpathians at 730 m and 790 m a.s.l., respectively were obtained and analysed for high-resolution pollen, macrofossils, charcoal, mineral magnetic parameters and organic matter. The chronostratigraphic framework was provided by dense AMS ¹⁴C measurements. </p><p>Cold and dry climatic conditions are indicated by the occurrence of open vegetation with shrubs and herbs, and cold lake water prior to 14,700 cal. yr BP. The climatic improvement at the beginning of the Lateglacial interstadial (around 14,700 cal. yr BP) is seen by the development of open forests. These were dominated by <i>Pinus</i> and <i>Betula</i>, but contained also new arriving tree taxa, such as <i>Populus</i>, <i>Alnus</i> and <i>Prunus</i>. The gradual establishment of forests may have led to a stabilization of the soils in the catchment. Between ca. 14,100 and 13,800 cal. yr BP the forest density became reduced to stands of <i>Pinus</i>, <i>Betula</i>, <i>Alnus</i>, <i>Larix</i> and <i>Populus</i> trees and grassland expanded, suggesting colder climatic conditions. <i>Picea</i> arrived as a new taxon at around 13,800 cal. yr BP, and between 13,800 and 12,900 cal. yr BP, the surroundings of the sites were predominantly covered by <i>Picea </i>forest. This forest included <i>Betula</i>, <i>Pinus</i>, <i>Alnus</i>, <i>Larix</i> and <i>Populus</i> and, from 13,200 cal. yr BP onwards also <i>Ulmus</i>. At ca. 12,900 cal. yr BP, the forest became significantly reduced and at 12,600 cal. yr BP, a recurrence of open vegetation with stands of <i>Larix</i>, <i>Pinus</i>, <i>Betula</i>, <i>Salix</i> and <i>Alnus</i> is documented, lasting until 11,500 cal. yr BP. This distinct change in vegetation may by taken as a strong decline in temperature and moisture availability.</p><p>At the transition to the Holocene, at ca. 11,500 cal. yr BP, <i>Pinus</i>, <i>Betula</i> and <i>Larix</i> quickly expanded (from small local stands) and formed open forests, probably as a response to warmer and more humid climatic conditions. At 11,250 cal. yr BP<i> Ulmus</i> and <i>Picea</i> expanded and the landscape became completely forested. The rapid increase of <i>Ulmus</i> and <i>Picea</i> after 11,500 cal. yr BP may suggest the existence of small residual populations close to the study sites during the preceding cold interval. <i>Ulmus</i> was the first and most prominent deciduous taxa in the early Holocene in the Gutaiului Mountains. From ca. 10,750 cal. yr BP onwards <i>Quercus,</i> <i>Tilia</i>, <i>Fraxinus </i>and <i>Acer</i> expanded and <i>Corylus</i> arrived. A highly diverse, predominantly deciduous forest with <i>Ulmus</i>, <i>Quercus</i>, <i>Tilia</i>,<i> Fraxinus</i>, <i>Acer</i>, <i>Corylus</i> and <i>Picea</i> developed between 10,700 and 8200 cal. yr BP, which possibly signifies more continental climatic conditions. The development of a <i>Picea-Corylus</i> dominated forest between 8200 and 5700 cal. yr BP is likely connected to a more humid and cooler climate. The establishment of <i>Carpinus</i> and <i>Fagus</i> was dated to 5750 cal. yr BP and 5200 cal. yr BP, respectively. The dominance of <i>Fagus</i> during the late Holocene, from 4000 cal. yr BP onwards, may have been related to cooler and more humid climatic conditions. First signs of human activities are recorded around 2300 cal. yr BP, but only during the last 300 years did local human impact become significant. </p><p>The vegetation development recorded in the Gutaiului Mountains during the Lateglacial is very similar to reconstructions based on lowland sites, whereas higher elevation sites seem not to have always experienced visible vegetation changes. The time of tree arrival and expansion during the past 11,500 cal. yr BP seems to have occurred almost synchronously across Romania. The composition of the forests during the Holocene in the Gutaiului Mountains is consistent with that reconstructed at mid-elevation sites, but differs from the forest composition at higher elevations. Important differences between the Gutaiului Mountains and other studied sites in Romania are a low representation of <i>Carpinus </i>and a late and weak human impact. </p><p>The available data sets for Romania give evidence for the presence of coniferous and cold-tolerant deciduous trees before 14,700 cal. yr BP. Glacial refugia for <i>Ulmus</i> may have occurred in different parts of Romania, whereas the existence of <i>Quercu</i>s, <i>Tilia</i>, <i>Corylus</i> and <i>Fraxinus</i> has not been corroborated. </p>

The objectives of this thesis are to establish a chronological framework for environmental changes during the last 15,000 years in northwest Romania, to reconstruct the vegetation development, and to evaluate the underlying processes for forest dynamics. Furthermore, an overview of earlier and ongoing pollenstratigraphic work in Romania is provided. Sediments from two former crater lakes, Preluca Tiganului and Steregoiu, situated in the Gutaiului Mountains, on the western extremity of the Eastern Carpathians at 730 m and 790 m a.s.l., respectively were obtained and analysed for high-resolution pollen, macrofossils, charcoal, mineral magnetic parameters and organic matter. The chronostratigraphic framework was provided by dense AMS 14C measurements. Cold and dry climatic conditions are indicated by the occurrence of open vegetation with shrubs and herbs, and cold lake water prior to 14,700 cal. yr BP. The climatic improvement at the beginning of the Lateglacial interstadial (around 14,700 cal. yr BP) is seen by the development of open forests. These were dominated by Pinus and Betula, but contained also new arriving tree taxa, such as Populus, Alnus and Prunus. The gradual establishment of forests may have led to a stabilization of the soils in the catchment. Between ca. 14,100 and 13,800 cal. yr BP the forest density became reduced to stands of Pinus, Betula, Alnus, Larix and Populus trees and grassland expanded, suggesting colder climatic conditions. Picea arrived as a new taxon at around 13,800 cal. yr BP, and between 13,800 and 12,900 cal. yr BP, the surroundings of the sites were predominantly covered by Picea forest. This forest included Betula, Pinus, Alnus, Larix and Populus and, from 13,200 cal. yr BP onwards also Ulmus. At ca. 12,900 cal. yr BP, the forest became significantly reduced and at 12,600 cal. yr BP, a recurrence of open vegetation with stands of Larix, Pinus, Betula, Salix and Alnus is documented, lasting until 11,500 cal. yr BP. This distinct change in vegetation may by taken as a strong decline in temperature and moisture availability. At the transition to the Holocene, at ca. 11,500 cal. yr BP, Pinus, Betula and Larix quickly expanded (from small local stands) and formed open forests, probably as a response to warmer and more humid climatic conditions. At 11,250 cal. yr BP Ulmus and Picea expanded and the landscape became completely forested. The rapid increase of Ulmus and Picea after 11,500 cal. yr BP may suggest the existence of small residual populations close to the study sites during the preceding cold interval. Ulmus was the first and most prominent deciduous taxa in the early Holocene in the Gutaiului Mountains. From ca. 10,750 cal. yr BP onwards Quercus, Tilia, Fraxinus and Acer expanded and Corylus arrived. A highly diverse, predominantly deciduous forest with Ulmus, Quercus, Tilia, Fraxinus, Acer, Corylus and Picea developed between 10,700 and 8200 cal. yr BP, which possibly signifies more continental climatic conditions. The development of a Picea-Corylus dominated forest between 8200 and 5700 cal. yr BP is likely connected to a more humid and cooler climate. The establishment of Carpinus and Fagus was dated to 5750 cal. yr BP and 5200 cal. yr BP, respectively. The dominance of Fagus during the late Holocene, from 4000 cal. yr BP onwards, may have been related to cooler and more humid climatic conditions. First signs of human activities are recorded around 2300 cal. yr BP, but only during the last 300 years did local human impact become significant. The vegetation development recorded in the Gutaiului Mountains during the Lateglacial is very similar to reconstructions based on lowland sites, whereas higher elevation sites seem not to have always experienced visible vegetation changes. The time of tree arrival and expansion during the past 11,500 cal. yr BP seems to have occurred almost synchronously across Romania. The composition of the forests during the Holocene in the Gutaiului Mountains is consistent with that reconstructed at mid-elevation sites, but differs from the forest composition at higher elevations. Important differences between the Gutaiului Mountains and other studied sites in Romania are a low representation of Carpinus and a late and weak human impact. The available data sets for Romania give evidence for the presence of coniferous and cold-tolerant deciduous trees before 14,700 cal. yr BP. Glacial refugia for Ulmus may have occurred in different parts of Romania, whereas the existence of Quercus, Tilia, Corylus and Fraxinus has not been corroborated.

As the world faces the effects of rapid climate change it is essential that we understand how the Earth’s climate has evolved in recent geological history. The island of Jersey harbours loess deposits which hold clues to recent climate change which have not been extensively studied. In this study, grain size analysis was employed on loess from the site of La Motte in order to shed light on climate change in the region during the last glacial. Several metrics such as the ratio of coarse to fine silt, the rate of deposition and the formation of ancient soils was used to assess the climate conditions during the time of deposition. The results show that the loess of La Motte is coarse compared to typical European loess but similar in grain size distribution to other sites along the English Channel, with relatively high amounts of sand and low amounts of clay. The relative coarseness of the deposits suggests a cold and dry depositional environment as well as proximity to the source of sediment and high wind intensities during the time of deposition. The fraction of coarse silt to fine silt, along with the rate of deposition and the occurrence of soil formation across the stratigraphy indicates that the climate slowly cooled from around 55 000 to 24 000 years ago when a sudden cooling event took place, then warmed until about 16 800 years ago where the climate suddenly cooled again. The timing of these rapid climatic shifts appears to correspond with Heinrich events 1 and 2 when large masses of ice were discharged from continental ice sheets. / Medan världen står inför effekterna av snabba klimatförändringar är det väsentligt att vi förstår hur jordens klimat har utvecklats under den senaste geologiska tiden. Ön Jersey hyser lössavlagringar som håller ledtrådar om den senaste tidens klimatförändringar och som inte studerats har studerats omfattande. I denna studie användes kornstorleksanalys på löss från lokaliteten La Motte med avsikt att utöka kunskapen om klimatförändringar i regionen under den senaste nedisningen. Ett flertal mått så som förhållandet mellan grov och fin silt, depositionshastigheten och bildningen av gamla jordar användes för att bedöma klimatförhållandena under avsättningstiden. Resultatet visar att La Mottes löss är grov jämfört med europeiska lössjordar, men i kornstorleksdistribution lik med andra lokaliteter längs med Engelska kanalen med relativt höga mängder sand och låga mängder lera. Avlagringarnas relativa grovhet tyder på en kall och torr avsättningsmiljö såväl som närhet till sedimentkällan och höga vindstyrkor under avsättningstiden. Förhållandet mellan grov och fin silt, tillsammans med depositionshastigheten och förekomsten av jordbildning genom stratigrafin tyder på att klimatet långsamt kyldes ner från omkring 55 000 år sedan till 24 000 år sedan då en plötslig nedkylning skedde. Klimatet värmdes sedan upp fram till omkring 16 800 år sedan då klimatet plötsligt kyldes ner igen. Tidpunkterna då dessa snabba avkylningar skedde verkar korrespondera med Heinrich-händelserna 1 och 2 då stora ismassor lossades från kontinentala istäcken ut i Nordatlanten.

Aeolian dust that gets deposited builds up loess sequences that cover 10% of the Earth's continents. Such sequences can be several metres thick with material deposited over thousands of years, and therefore act like archives of past climates. The glacial and interglacial cycles during the late Quaternary affects the loess deposition and the dust in the atmosphere, which has an impact on the global climate. Loess material is deposited during colder and drier periods. Paleosols have often been developed in the loess sequences, reflecting a warmer and wetter climate with decreased dust deposition. By sampling loess from different depths of the sequence and analysing different properties of the material, a reconstruction of past environment and climate can be done. Two commonly used methods are magnetic susceptibility analysis and grain size analysis and differences in the result can show differences in the climate and environment at the time the material was deposited. The late Quaternary climate was influenced by changes in the North Atlantic, and loess in the area is important to study to get a better understanding of the climate at the time it was deposited. In this project, loess material from a 10 metres thick sequence at the Romont site, Belgium has been analysed with grain size and magnetic susceptibility measurements to reconstruct past climate. The results show differences in the magnetic enhancement and the grain size as a gradual decrease in the magnetic enhancement, indicating a colder climate as confirmed by an increase in the U-ratio. This is followed by the abrupt onset of the warm Holocene period, matching the marine isotope record at the approximate same time period. The magnetic susceptibility data identifies the Rocourt tephra layer and also shows evidence of erosion of material between the Kincamp soil and the Nagelbeek Tongue Horizon. / Fint sandmaterial som transporteras med vinden kallas för stoft, när det sedan avsätts på marken bygger det upp så kallade för löss-sekvenser. En löss-sekvens kan vara flera meter tjock och uppbyggd under tusentals år, vilket innebär att materialet på olika djup reflekterar hur klimatet var då det avsattes. Klimatet under senkvartär tid reflekterar istider och mellanistider, vilket påverkar mängden stoft i atmosfären och avsättningen av materialet. Materialet har främst avsatts under kalla och torra perioder. Avsättningen minskade under varma och blöta perioder, vilket var optimalt för så kallade  paleosoler att bildas genom vittring. Genom att ta prover från olika djup i en löss-sekvens och analysera dem är det möjligt att tolka tidigare förändringar i klimatet. Två vanliga analysmetoder är att mäta materialets magnetiska mottaglighet och kornstorleken på materialet. Klimatet under senkvartär tid (130 - 12 tusen år sedan) påverkades av norra Atlanten. Det är därför av stor vikt att analysera prover från platser i närheten, för att bättre förstå hur klimatet varierat då materialet avsattes. I det här projektet har material från en 10 meter tjock löss-sekvens i Romont, Belgien analyserats. Resultatet visar variationer i kornstorlek och magnetisk mottaglighet. Ett vulkaniskt lager som kallas Rocourt identifierades, följt av en gradvis minskning av den magnetiska mottagligheten som visar på ett gradvis kallare klimat fram till början på den varma Holocen-perioden som vi befinner oss i nu. Resultatet visar också bevis för erosion mellan två enheter i sekvensen.