Pub Date : 2016-01-01DOI: 10.4316/GEOREVIEW.2016.0.0.293
M. Braun
This work focuses on building a high-resolution age-depth model for quantitative paleoclimate study from the Mohos peat bog, East Carpathians. Peats are important archives for Quaternary science, because they preserve environmental changes. To study the chronology of peat profiles the key is in the precise coring and reliable dating. However, many studies dealing with coring and radiocarbon dating of peat deposits they often shown problems with the proper methods and material
{"title":"Coring and chronology of Mohoș peat bog, East Carpathians","authors":"M. Braun","doi":"10.4316/GEOREVIEW.2016.0.0.293","DOIUrl":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.293","url":null,"abstract":"This work focuses on building a high-resolution age-depth model for quantitative paleoclimate study from the Mohos peat bog, East Carpathians. Peats are important archives for Quaternary science, because they preserve environmental changes. To study the chronology of peat profiles the key is in the precise coring and reliable dating. However, many studies dealing with coring and radiocarbon dating of peat deposits they often shown problems with the proper methods and material","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"8"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70435982","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2016-01-01DOI: 10.4316/GEOREVIEW.2016.0.0.297
M. Danu
Archaeobotanical, archaeozoological and archaeological studies carried out in Chalcolithic sites to the East of Carpathians (i.g. Poduri- Dealul Ghindaru , and Hoisești), contributed to reconstruct the environmental context of the settlements, and to evidence diverse human activities in the area
{"title":"Interactions between humans and environment in Middle Holocene: comparative study of two Chalcolithic sites to the East of Carpathians","authors":"M. Danu","doi":"10.4316/GEOREVIEW.2016.0.0.297","DOIUrl":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.297","url":null,"abstract":"Archaeobotanical, archaeozoological and archaeological studies carried out in Chalcolithic sites to the East of Carpathians (i.g. Poduri- Dealul Ghindaru , and Hoisești), contributed to reconstruct the environmental context of the settlements, and to evidence diverse human activities in the area","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"12"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70436067","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2016-01-01DOI: 10.4316/GEOREVIEW.2016.0.0.300
M. Evans
The goals of the PAGES 2k project include placing recent global change within the context of the past 2000 years (the 2k interval), and identifying the processes most likely to explain those observations. The 2k project is organized into 9 regional working groups and several transregional initiatives. We encourage an inclusive, international, community-driven, interdisciplinary and open source approach driven by workshops, searchable public metadatabases, virtual collaborations and peer reviewed publications. In this contribution, I will review products from Phase 1 (2006-2015) and progress in Phase 2 (2015-2016), including development of temperature, stable isotope and hydroclimate-relevant observational metadatabases; continental-scale surface temperature and regional and global scale sea surface temperature reconstructions and syntheses; comparison of observed and simulated temperatures; and assessment of the timing of the onset of industrial warming. More information is at: http://www.pages-igbp.org/ini/wg/2k-network/intro .
{"title":"PAGES 2k - Overview of recent products and progress","authors":"M. Evans","doi":"10.4316/GEOREVIEW.2016.0.0.300","DOIUrl":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.300","url":null,"abstract":"The goals of the PAGES 2k project include placing recent global change within the context of the past 2000 years (the 2k interval), and identifying the processes most likely to explain those observations. The 2k project is organized into 9 regional working groups and several transregional initiatives. We encourage an inclusive, international, community-driven, interdisciplinary and open source approach driven by workshops, searchable public metadatabases, virtual collaborations and peer reviewed publications. In this contribution, I will review products from Phase 1 (2006-2015) and progress in Phase 2 (2015-2016), including development of temperature, stable isotope and hydroclimate-relevant observational metadatabases; continental-scale surface temperature and regional and global scale sea surface temperature reconstructions and syntheses; comparison of observed and simulated temperatures; and assessment of the timing of the onset of industrial warming. More information is at: http://www.pages-igbp.org/ini/wg/2k-network/intro .","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"15"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70436137","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2016-01-01DOI: 10.4316/GEOREVIEW.2016.0.0.305
G. Florescu, A. Feurdean
Sedimentary microscopic charcoal (particles smaller than 150 microns) has been used to describe multi-decadal to millennial scale biomass burning at regional scales, whereas macroscopic charcoal (particles larger than 150 microns) analysis is increasingly used to investigate past biomass burning at a local scale
{"title":"Fire as a driver of ecosystem dynamics in Central and Eastern Europe throughout the Lateglacial and Holocene","authors":"G. Florescu, A. Feurdean","doi":"10.4316/GEOREVIEW.2016.0.0.305","DOIUrl":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.305","url":null,"abstract":"Sedimentary microscopic charcoal (particles smaller than 150 microns) has been used to describe multi-decadal to millennial scale biomass burning at regional scales, whereas macroscopic charcoal (particles larger than 150 microns) analysis is increasingly used to investigate past biomass burning at a local scale","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"21-22"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70436243","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2016-01-01DOI: 10.4316/GEOREVIEW.2016.0.0.321
U. Hambach
Late Pleistocene palaeoclimatic records for south-eastern Europe rely largely on loess-palaeosol sequences (LPSS). The general spatial scarcity and often limited temporal range of other sedimentary archives assign the LPSS of the region a key role even in millennial scale temporal reconstructions of the Late Pleistocene terrestrial environmental dynamics. In Eurasia, aeolian dust sediments (loess) are widespread in continental mid-latitudes. The Eurasian loess-belt has its western end in the Middle Danube (Carpathian) and the Lower Danube Basin. Similar to the Chinese Loess Plateau (CLP) and to the steppe areas of Central Asia one can find true loess plateaus in this area dating back more than one million years and comprising a semi-continuous record of the Quaternary palaeoclimate (Markovic et al. 2011, 2015).
东南欧晚更新世古气候记录主要依赖于黄土-古土壤序列(LPSS)。其他沉积档案的普遍空间稀缺性和通常有限的时间范围使该地区的LPSS甚至在晚更新世陆地环境动力学的千年尺度时间重建中发挥关键作用。在欧亚大陆，风沙沉积物(黄土)广泛分布于大陆中纬度地区。欧亚黄土带的西端在多瑙河中部(喀尔巴阡山脉)和多瑙河下游盆地。与中国黄土高原(CLP)和中亚草原地区类似，在该地区可以找到真正的黄土高原，其历史可以追溯到100多万年，构成了第四纪古气候的半连续记录(Markovic et al. 2011, 2015)。
{"title":"Towards multi-proxy based millennial time scales in Late Pleistocene Danubian Loess-Palaeosol Sequences","authors":"U. Hambach","doi":"10.4316/GEOREVIEW.2016.0.0.321","DOIUrl":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.321","url":null,"abstract":"Late Pleistocene palaeoclimatic records for south-eastern Europe rely largely on loess-palaeosol sequences (LPSS). The general spatial scarcity and often limited temporal range of other sedimentary archives assign the LPSS of the region a key role even in millennial scale temporal reconstructions of the Late Pleistocene terrestrial environmental dynamics. In Eurasia, aeolian dust sediments (loess) are widespread in continental mid-latitudes. The Eurasian loess-belt has its western end in the Middle Danube (Carpathian) and the Lower Danube Basin. Similar to the Chinese Loess Plateau (CLP) and to the steppe areas of Central Asia one can find true loess plateaus in this area dating back more than one million years and comprising a semi-continuous record of the Quaternary palaeoclimate (Markovic et al. 2011, 2015).","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"35-37"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70436333","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2016-01-01DOI: 10.4316/GEOREVIEW.2016.0.0.332
Jack Longman, D. Veres
In Europe the characteristics, distribution and effects of recent pollution are well known, with monitoring observations existing at a continental scale. However, estimates of long-term pollution are restricted to central-western Europe, the British Isles and Scandinavia. In Eastern Europe in particular, the lack of such estimates has led to incomplete understanding of regional differences. When coupled to the insufficient knowledge of past emission sources and isotopic signatures of various ores, it is clear there are gaps in our knowledge of the history of pollution in this area. As a result, the causal relationships between humans and the environment are insufficiently explored, particularly within the Carpathian region - one with significant mineral wealth and a long history of human presence
{"title":"Base metal pollution as a result of historical ore smelting in the Romanian Carpathians throughout the Holocene","authors":"Jack Longman, D. Veres","doi":"10.4316/GEOREVIEW.2016.0.0.332","DOIUrl":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.332","url":null,"abstract":"In Europe the characteristics, distribution and effects of recent pollution are well known, with monitoring observations existing at a continental scale. However, estimates of long-term pollution are restricted to central-western Europe, the British Isles and Scandinavia. In Eastern Europe in particular, the lack of such estimates has led to incomplete understanding of regional differences. When coupled to the insufficient knowledge of past emission sources and isotopic signatures of various ores, it is clear there are gaps in our knowledge of the history of pollution in this area. As a result, the causal relationships between humans and the environment are insufficiently explored, particularly within the Carpathian region - one with significant mineral wealth and a long history of human presence","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"53"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70436355","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2016-01-01DOI: 10.4316/GEOREVIEW.2016.0.0.337
D. Michczyńska
The central part of Europe during the last cold stage was occupied by permafrost and twice invaded by the Scandinavian ice sheet, but about 70% of time was taken by transitional phases of continuous fluctuations of permafrost, which are reflected especially in type and thickness of slope, fluvial and aeolian deposits
{"title":"Reflection of climatic changes during Interpleniglacial in geoecosystems of Southern Poland","authors":"D. Michczyńska","doi":"10.4316/GEOREVIEW.2016.0.0.337","DOIUrl":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.337","url":null,"abstract":"The central part of Europe during the last cold stage was occupied by permafrost and twice invaded by the Scandinavian ice sheet, but about 70% of time was taken by transitional phases of continuous fluctuations of permafrost, which are reflected especially in type and thickness of slope, fluvial and aeolian deposits","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"233 1","pages":"60"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70436463","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2016-01-01DOI: 10.4316/GEOREVIEW.2016.0.0.338
D. Michczyńska, W. Margielewski
The Grel raised peat bog is located in the Ludźmierz village vicinity in the Orawa-Nowy Targ Basin. This raised bog, has heavily degraded peat dome covered with numerous post excavation pits which are the results of peat extraction for local purposes. Peat bog is overgrown with birch and pine forests and typical vegetation for raised bog. First palynological study of the peat depositional sequence was performed by Koperowa (1962). The beginning of the peat bog formation was then attributed to the Oldest Dryas. Consequently the Grel is the oldest peat bog in the peatland of the Orawa-Nowy Targ Basin
{"title":"Palaeoenvironmental changes of Orawa-Nowy Targ Basin in the Late Glacial and Holocene recorded in sediments of Grel raised bog","authors":"D. Michczyńska, W. Margielewski","doi":"10.4316/GEOREVIEW.2016.0.0.338","DOIUrl":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.338","url":null,"abstract":"The Grel raised peat bog is located in the Ludźmierz village vicinity in the Orawa-Nowy Targ Basin. This raised bog, has heavily degraded peat dome covered with numerous post excavation pits which are the results of peat extraction for local purposes. Peat bog is overgrown with birch and pine forests and typical vegetation for raised bog. First palynological study of the peat depositional sequence was performed by Koperowa (1962). The beginning of the peat bog formation was then attributed to the Oldest Dryas. Consequently the Grel is the oldest peat bog in the peatland of the Orawa-Nowy Targ Basin","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"61-62"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70436518","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2016-01-01DOI: 10.4316/GEOREVIEW.2016.0.0.351
Ceran Şekeryapan
We present the freshwater ostracod stratigraphy of former lake, in Saglik plain, South Central Anatolia, Turkey, since the Last Late Glacial until the mid-Holocene. Podocopoid (non-marine) ostracods were identified in Saglik II (SAĞ II) core whose the lowermost part goes back to 15500 years ago. Both smooth and noded forms of Cyprideis torosa ( Jones, 1850 ), Candona sp . ( Baird, 1845 ), Ilyocypris sp. ( Brady & Norman, 1889 ) , Darwinula stevensoni ( Brady & Robertson, 1870 ), Plesiocypridopsis newtoni ( Brady & Robertson, 1870 ), and Prionocypris zenkeri ( Chyzer&Toth, 1858 ) were the observed species
{"title":"Non-marine Ostracoda in Sağlık plain, Kahramanmaraş, Turkey, since the Late Glacial to mid-Holocene","authors":"Ceran Şekeryapan","doi":"10.4316/GEOREVIEW.2016.0.0.351","DOIUrl":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.351","url":null,"abstract":"We present the freshwater ostracod stratigraphy of former lake, in Saglik plain, South Central Anatolia, Turkey, since the Last Late Glacial until the mid-Holocene. Podocopoid (non-marine) ostracods were identified in Saglik II (SAĞ II) core whose the lowermost part goes back to 15500 years ago. Both smooth and noded forms of Cyprideis torosa ( Jones, 1850 ), Candona sp . ( Baird, 1845 ), Ilyocypris sp. ( Brady & Norman, 1889 ) , Darwinula stevensoni ( Brady & Robertson, 1870 ), Plesiocypridopsis newtoni ( Brady & Robertson, 1870 ), and Prionocypris zenkeri ( Chyzer&Toth, 1858 ) were the observed species","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"85"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70436738","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2016-01-01DOI: 10.4316/GEOREVIEW.2016.0.0.289
M. Bormann
We present a new record of vegetation and climate history derived from a multiproxy investigation of sediments recovered from the in-filled Mohos crater (46°05' N; 25°55' E) located within the Ciomadul volcano complex (Romania). To date, the 30-m long sediment core, covering MIS 3 to present provides one of the longest lacustrine records from the Carpathian region
{"title":"Vegetation and climate history in the Carpathians during MIS 3-2 – a multi-proxy study of a sediment sequence from Mohoş crater, Romania","authors":"M. Bormann","doi":"10.4316/GEOREVIEW.2016.0.0.289","DOIUrl":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.289","url":null,"abstract":"We present a new record of vegetation and climate history derived from a multiproxy investigation of sediments recovered from the in-filled Mohos crater (46°05' N; 25°55' E) located within the Ciomadul volcano complex (Romania). To date, the 30-m long sediment core, covering MIS 3 to present provides one of the longest lacustrine records from the Carpathian region","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"26 1","pages":"2-3"},"PeriodicalIF":0.0,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70435900","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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