Mirosława Kupryjanowicz
Dados Biográficos
| ID | 3424474 |
|---|---|
| NOME | Mirosława Kupryjanowicz |
| PRENOMES | Mirosława |
| SOBRENOME | Kupryjanowicz |
| ASSINATURA | KUPRYJANOWICZ M |
| AFILIAÇÕES | University of Białystok |
| ORCID | 0000-0003-0629-6247 |
| VERIFICADO | Sim |
| TOTAL DE OBRAS | 22 |
| TOTAL DE CITAÇÕES | 33 |
| TOTAL COMO AUTOR | 22 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 2014 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2025 |
| ÍNDICE H | 3 |
Norway Spruce dynamics in NE Poland at the Middle-Late-Holocene transition
Norway spruce is one of Europe’s most significant trees, with a millennia-long role crucial for maintaining values of forests. Yet its migration, especially at its current range limits, is not fully understood. The paper presents the results of palynological research on the temporal spread of spruce in NE Poland between ca. 5500–2300 cal BP. The significance of our study lies in the fact that we used pollen records to reconstruct the vegetation u…
Late Saalian climatic oscillations – revision of pollen record in Poland compared to other evidences
Late glacial and Holocene vegetation history and climate oscillations – Preliminary pollen data from lake Boczne, NE Poland
Bog pine dendrochronology related to peat stratigraphy
A palaeoenvironmental record of MIS 3 climate change in NE Poland—Sedimentary and geochemical evidence
Tracking fire activity and post-fire limnological responses using the varved sedimentary sequence of Lake Jaczno, Poland
Long-term paleofire perspectives provide key information on natural and human-derived land cover changes. The last few millennia are crucial to understanding the future of wildfire threats, since the increasing global temperatures are expected to have an impact on regions previously assumed to not be endangered. In this study we investigate the interplay between changing climatic conditions, land cover transformation, fires, and human activity ba…
Eemian and early Weichselian environmental changes at the Jałówka site, NE Poland, and their correlation with marine and ice records
Vegetation changes were documented across the last interglacial period (MIS 5e, Eemian) and continuing through the older part of the last glacial period (MIS 5d–a, early Weichselian). This study was based on pollen data collected at the Jałówka site, NE Poland. Two cold oscillations appeared within warm periods during this stage of the upper Pleistocene. The older oscillation was the temporary intra–interglacial cooling at the end of the Eemian. …
Compositional turnover and variation in Eemian pollen sequences in Europe
Occurrence of slender naiad (Najas flexilis (Willd.) Rostk. & W. L. E. Schmidt) during the Eemian Interglacial – An example of a palaeolake from the Hieronimowo site, NE Poland
Vegetation and climate of the Eemian Interglacial and Early Weichselian (Vistulian) in Poland – from the local to regional scale. In memory of Professor Kazimiera Mamakowa
Response of terrestrial and lake environments in NE Poland to Preboreal cold oscillations (PBO)
Was there an abrupt cold climatic event in the middle Eemian? Pollen record from a palaeolake at the Hieronimowo site, NE Poland
The east-west migration of trees during the Eemian Interglacial registered on isopollen maps of Poland
New finds of Eemian Tilia tomentosa Moench macroremais in NE Poland, and the reconstructed European range of this species during the last interglacial
Environmental changes related to the 8.2-ka event and other climate fluctuations during the middle Holocene
Multi-proxy palaeoecological data (pollen, diatom, Cladocera) about the environment during the middle-Holocene from Suchar II and Suchar Wielki, dystrophic lakes, in NE Poland are presented. Fluctuations in the pollen concentration, indicative of changes in pollen productivity and shifts in woodland composition, document the considerable instability of the climate in NE Poland between 9200 and 5750 cal. yr BP. The recognised colder events were da…
Was it ‘ terra desolata ’? Conquering and colonizing the medieval Prussian wilderness in the context of climate change
Pollen, non-pollen palynomorphs, charcoal and geochemical analyses of sediments from Lakes Salęt and Ruskowiejskie (NE Poland) were used to reconstruct vegetation changes in the former Galindia territory (Old Prussia) related to human activity and the climatic instability of the medieval period. Among archaeologists and historians, there is a widespread opinion that the permanent transformations of the environment in Prussia (south-eastern Baltic…
Anthropogenic Transformation of the Vegetation in the Immediate Vicinity of the Settlement Complex at Poganowo (Mrągowo Lakeland, Ne Poland)
The results of pollen, non-pollen palynomorph and microcharcoal particle analyses of deposits from a small pond in north eastern Poland are presented. The study focused on human-induced vegetation changes that occurred in a close vicinity of the settlement complex at Poganowo during the Middle Ages (ca 10 th -16 th centuries). We distinguished three phases of human impact. First and third phases correspond to intensified settlement activity. The …
Evolution of a small Eemian lake in a unique location on a kame hill
Reaction of lake environment on the climatic cooling – Transition from the Eemian Interglacial to Early Vistulian on the basis of Solniki palaeolake sediments (NE Poland)
Postglacial shifts in lake trophic status based on a multiproxy study of a humic lake
The long-term development of a humic lake ecosystem in Poland was investigated via palaeoecological analyses of age-dated sediment cores. Peat and lacustrine deposit records spanning approximately 12,000 years of lake history were analysed with regard to palynomorphs, plant macrofossils, degree of peat decomposition, Cladocera and geochemistry. Our study demonstrated the difficulty of classifying sediments deposited in humic lakes. We considered …
The environmental and cultural contexts of the late Iron Age and medieval settlement in the Mazurian Lake District, NE Poland
Pollen analysis of sediments from three lakes and analysis of plant macroremains including charcoal from archaeological sites in the Mazurian Lake District provide new data for the reconstruction of vegetation changes related to human activity between the 1st and 13th century AD. At that time settlements of the Bogaczewo culture (from the turn of the 1st century AD to the first part of the 5th century AD), the Olsztyn Group (second part of the 5t…
The Iron Age in the Mrągowo Lake District, Masuria, NE Poland
Pollen, non-pollen palynomorphs, charcoal and geochemical analyses of sediments from Lake Salęt (NE Poland) were used to reconstruct vegetation changes related to the activity of the West Balt tribes during the Iron Age, in the period between the second half of the 7th century bc and the beginning of the 10th century ad. We distinguished five phases of human impact on environment. Woodland clearing around the studied lake started at the end of th…
The environmental and cultural contexts of the late Iron Age and medieval settlement in the Mazurian Lake District, NE Poland
Pollen analysis of sediments from three lakes and analysis of plant macroremains including charcoal from archaeological sites in the Mazurian Lake District provide new data for the reconstruction of vegetation changes related to human activity between the 1st and 13th century AD. At that time settlements of the Bogaczewo culture (from the turn of the 1st century AD to the first part of the 5th century AD), the Olsztyn Group (second part of the 5t…
The Iron Age in the Mrągowo Lake District, Masuria, NE Poland
Pollen, non-pollen palynomorphs, charcoal and geochemical analyses of sediments from Lake Salęt (NE Poland) were used to reconstruct vegetation changes related to the activity of the West Balt tribes during the Iron Age, in the period between the second half of the 7th century bc and the beginning of the 10th century ad. We distinguished five phases of human impact on environment. Woodland clearing around the studied lake started at the end of th…
Tracking fire activity and post-fire limnological responses using the varved sedimentary sequence of Lake Jaczno, Poland
Long-term paleofire perspectives provide key information on natural and human-derived land cover changes. The last few millennia are crucial to understanding the future of wildfire threats, since the increasing global temperatures are expected to have an impact on regions previously assumed to not be endangered. In this study we investigate the interplay between changing climatic conditions, land cover transformation, fires, and human activity ba…
Compositional turnover and variation in Eemian pollen sequences in Europe
Late glacial and Holocene vegetation history and climate oscillations – Preliminary pollen data from lake Boczne, NE Poland
Was it ‘ terra desolata ’? Conquering and colonizing the medieval Prussian wilderness in the context of climate change
Pollen, non-pollen palynomorphs, charcoal and geochemical analyses of sediments from Lakes Salęt and Ruskowiejskie (NE Poland) were used to reconstruct vegetation changes in the former Galindia territory (Old Prussia) related to human activity and the climatic instability of the medieval period. Among archaeologists and historians, there is a widespread opinion that the permanent transformations of the environment in Prussia (south-eastern Baltic…
Postglacial shifts in lake trophic status based on a multiproxy study of a humic lake
The long-term development of a humic lake ecosystem in Poland was investigated via palaeoecological analyses of age-dated sediment cores. Peat and lacustrine deposit records spanning approximately 12,000 years of lake history were analysed with regard to palynomorphs, plant macrofossils, degree of peat decomposition, Cladocera and geochemistry. Our study demonstrated the difficulty of classifying sediments deposited in humic lakes. We considered …
Postglacial shifts in lake trophic status based on a multiproxy study of a humic lake
The long-term development of a humic lake ecosystem in Poland was investigated via palaeoecological analyses of age-dated sediment cores. Peat and lacustrine deposit records spanning approximately 12,000 years of lake history were analysed with regard to palynomorphs, plant macrofossils, degree of peat decomposition, Cladocera and geochemistry. Our study demonstrated the difficulty of classifying sediments deposited in humic lakes. We considered …
The environmental and cultural contexts of the late Iron Age and medieval settlement in the Mazurian Lake District, NE Poland
Pollen analysis of sediments from three lakes and analysis of plant macroremains including charcoal from archaeological sites in the Mazurian Lake District provide new data for the reconstruction of vegetation changes related to human activity between the 1st and 13th century AD. At that time settlements of the Bogaczewo culture (from the turn of the 1st century AD to the first part of the 5th century AD), the Olsztyn Group (second part of the 5t…
The Iron Age in the Mrągowo Lake District, Masuria, NE Poland
Pollen, non-pollen palynomorphs, charcoal and geochemical analyses of sediments from Lake Salęt (NE Poland) were used to reconstruct vegetation changes related to the activity of the West Balt tribes during the Iron Age, in the period between the second half of the 7th century bc and the beginning of the 10th century ad. We distinguished five phases of human impact on environment. Woodland clearing around the studied lake started at the end of th…
Anthropogenic Transformation of the Vegetation in the Immediate Vicinity of the Settlement Complex at Poganowo (Mrągowo Lakeland, Ne Poland)
The results of pollen, non-pollen palynomorph and microcharcoal particle analyses of deposits from a small pond in north eastern Poland are presented. The study focused on human-induced vegetation changes that occurred in a close vicinity of the settlement complex at Poganowo during the Middle Ages (ca 10 th -16 th centuries). We distinguished three phases of human impact. First and third phases correspond to intensified settlement activity. The …
Evolution of a small Eemian lake in a unique location on a kame hill
Reaction of lake environment on the climatic cooling – Transition from the Eemian Interglacial to Early Vistulian on the basis of Solniki palaeolake sediments (NE Poland)
Was it ‘ terra desolata ’? Conquering and colonizing the medieval Prussian wilderness in the context of climate change
Pollen, non-pollen palynomorphs, charcoal and geochemical analyses of sediments from Lakes Salęt and Ruskowiejskie (NE Poland) were used to reconstruct vegetation changes in the former Galindia territory (Old Prussia) related to human activity and the climatic instability of the medieval period. Among archaeologists and historians, there is a widespread opinion that the permanent transformations of the environment in Prussia (south-eastern Baltic…
Environmental changes related to the 8.2-ka event and other climate fluctuations during the middle Holocene
Multi-proxy palaeoecological data (pollen, diatom, Cladocera) about the environment during the middle-Holocene from Suchar II and Suchar Wielki, dystrophic lakes, in NE Poland are presented. Fluctuations in the pollen concentration, indicative of changes in pollen productivity and shifts in woodland composition, document the considerable instability of the climate in NE Poland between 9200 and 5750 cal. yr BP. The recognised colder events were da…
Occurrence of slender naiad (Najas flexilis (Willd.) Rostk. & W. L. E. Schmidt) during the Eemian Interglacial – An example of a palaeolake from the Hieronimowo site, NE Poland
Vegetation and climate of the Eemian Interglacial and Early Weichselian (Vistulian) in Poland – from the local to regional scale. In memory of Professor Kazimiera Mamakowa
Response of terrestrial and lake environments in NE Poland to Preboreal cold oscillations (PBO)
Was there an abrupt cold climatic event in the middle Eemian? Pollen record from a palaeolake at the Hieronimowo site, NE Poland
The east-west migration of trees during the Eemian Interglacial registered on isopollen maps of Poland
New finds of Eemian Tilia tomentosa Moench macroremais in NE Poland, and the reconstructed European range of this species during the last interglacial
Compositional turnover and variation in Eemian pollen sequences in Europe
Eemian and early Weichselian environmental changes at the Jałówka site, NE Poland, and their correlation with marine and ice records
Vegetation changes were documented across the last interglacial period (MIS 5e, Eemian) and continuing through the older part of the last glacial period (MIS 5d–a, early Weichselian). This study was based on pollen data collected at the Jałówka site, NE Poland. Two cold oscillations appeared within warm periods during this stage of the upper Pleistocene. The older oscillation was the temporary intra–interglacial cooling at the end of the Eemian. …
Bog pine dendrochronology related to peat stratigraphy
A palaeoenvironmental record of MIS 3 climate change in NE Poland—Sedimentary and geochemical evidence
Tracking fire activity and post-fire limnological responses using the varved sedimentary sequence of Lake Jaczno, Poland
Long-term paleofire perspectives provide key information on natural and human-derived land cover changes. The last few millennia are crucial to understanding the future of wildfire threats, since the increasing global temperatures are expected to have an impact on regions previously assumed to not be endangered. In this study we investigate the interplay between changing climatic conditions, land cover transformation, fires, and human activity ba…
Norway Spruce dynamics in NE Poland at the Middle-Late-Holocene transition
Norway spruce is one of Europe’s most significant trees, with a millennia-long role crucial for maintaining values of forests. Yet its migration, especially at its current range limits, is not fully understood. The paper presents the results of palynological research on the temporal spread of spruce in NE Poland between ca. 5500–2300 cal BP. The significance of our study lies in the fact that we used pollen records to reconstruct the vegetation u…
Late Saalian climatic oscillations – revision of pollen record in Poland compared to other evidences
Late glacial and Holocene vegetation history and climate oscillations – Preliminary pollen data from lake Boczne, NE Poland
Geology and Paleoclimatology Research (20 obras) · Geography (18 obras) · Geology (17 obras) · Physical geography (16 obras) · Ecology (15 obras) · Paleontology (13 obras) · Biology (12 obras) · Pollen (12 obras) · Eemian (10 obras) · Ancient and Medieval Archaeology Studies (9 obras)