Insights into the raw materials and technology used to produce Copper Age ceramics in the Southern Carpathians (Romania)

© 2016, Springer-Verlag Berlin Heidelberg. The Copper Age Coţofeni culture occupied a large territory which covers present day W Romania, NE Serbia, and NW Bulgaria. The Coțofeni people lived in settlements located on hill slopes and river terraces, as well as in caves. Their hand-modeled ceramic pottery is richly ornamented by incisions, incrustations, and “lentil bean” appliqués. Potsherds found in the “Peştera Mare de la Cerişor” (i.e., the “Great Cave of Cerişor”) located in Paleozoic crystalline limestones and dolomites (Southern Carpathians, Romania) were studied in terms of mineralogy and petrography by OM, XRD, and EMPA. The sherds consist of an Fe-rich illitic matrix embedding quartz, K-feldspar, muscovite, plagioclase, biotite, chlorite, various heavy minerals, metamorphic, magmatic and sedimentary lithoclasts, as well as soil concretions and chamotte. Within a temperature interval, spanning between ∼800 and ∼900 °C, three firing groups were roughly separated, based on the optical characteristics of the matrix and the intensity of the illite/muscovite diffraction peaks. Quaternary and Miocene rocks from the area were analyzed by XRD in order to determine the provenance of the raw materials

Insights into the raw materials and technology used to produce Copper Age ceramics in the Southern Carpathians (Romania)

© 2016, Springer-Verlag Berlin Heidelberg. The Copper Age Coţofeni culture occupied a large territory which covers present day W Romania, NE Serbia, and NW Bulgaria. The Coțofeni people lived in settlements located on hill slopes and river terraces, as well as in caves. Their hand-modeled ceramic pottery is richly ornamented by incisions, incrustations, and “lentil bean” appliqués. Potsherds found in the “Peştera Mare de la Cerişor” (i.e., the “Great Cave of Cerişor”) located in Paleozoic crystalline limestones and dolomites (Southern Carpathians, Romania) were studied in terms of mineralogy and petrography by OM, XRD, and EMPA. The sherds consist of an Fe-rich illitic matrix embedding quartz, K-feldspar, muscovite, plagioclase, biotite, chlorite, various heavy minerals, metamorphic, magmatic and sedimentary lithoclasts, as well as soil concretions and chamotte. Within a temperature interval, spanning between ∼800 and ∼900 °C, three firing groups were roughly separated, based on the optical characteristics of the matrix and the intensity of the illite/muscovite diffraction peaks. Quaternary and Miocene rocks from the area were analyzed by XRD in order to determine the provenance of the raw materials

Climate Variability and Associated Vegetation Response throughout Central and Eastern Europe (CEE) between 60 and 8 ka

Records of past climate variability and associated vegetation response exist in various regions throughout Central and Eastern Europe (CEE). To date, there has been no coherent synthesis of the existing palaeo-records. During an INTIMATE meeting (Cluj Napoca, Romania) focused on identifying CEE paleo-records, it was decided to address this gap by presenting the palaeo-community with a compilation of high-quality climatic and vegetation records for the past 60–8 ka. The compilation should also serve as a reference point for the use in the modelling community working towards the INTIMATE project goals, and in data-model inter-comparison studies. This paper is therefore a compilation of up to date, best available quantitative and semi-quantitative records of past climate and biotic response from CEE covering this period. It first presents the proxy and archive used. Speleothems and loess mainly provide the evidences available for the 60–20 ka interval, whereas pollen records provide the main source of information for the Lateglacial and Holocene. It then examines the temporal and spatial patterns of climate variability inferred from different proxies, the temporal and spatial magnitude of the vegetation responses inferred from pollen records and highlights differences and similarities between proxies and sub-regions and the possible mechanisms behind this variability. Finally, it identifies weakness in the proxies and archives and their geographical distribution. This exercise also provides an opportunity to reflect on the status of research in the area and to identify future critical areas and subjects of research

Climate variability and associated vegetation response throughout Central and Eastern Europe (CEE) between 60 and 8 ka

Abstract Records of past climate variability and associated vegetation response exist in various regions throughout Central and Eastern Europe (CEE). To date, there has been no coherent synthesis of the existing palaeo-records. During an INTIMATE meeting (Cluj Napoca, Romania) focused on identifying CEE paleo-records, it was decided to address this gap by presenting the palaeo-community with a compilation of high-quality climatic and vegetation records for the past 60–8 ka. The compilation should also serve as a reference point for the use in the modelling community working towards the INTIMATE project goals, and in data-model inter-comparison studies. This paper is therefore a compilation of up to date, best available quantitative and semi-quantitative records of past climate and biotic response from CEE covering this period. It first presents the proxy and archive used. Speleothems and loess mainly provide the evidences available for the 60–20 ka interval, whereas pollen records provide the main source of information for the Lateglacial and Holocene. It then examines the temporal and spatial patterns of climate variability inferred from different proxies, the temporal and spatial magnitude of the vegetation responses inferred from pollen records and highlights differences and similarities between proxies and sub-regions and the possible mechanisms behind this variability. Finally, it identifies weakness in the proxies and archives and their geographical distribution. This exercise also provides an opportunity to reflect on the status of research in the area and to identify future critical areas and subjects of research