Judy R M Allen
Dados Biográficos
| ID | 5666128 |
|---|---|
| NOME | Judy R M Allen |
| PRENOMES | Judy R M |
| SOBRENOME | Allen |
| ASSINATURA | ALLEN J R M |
| AFILIAÇÕES | Durham University |
| ORCID | 0000-0002-0278-2929 |
| VERIFICADO | Sim |
| TOTAL DE OBRAS | 9 |
| TOTAL DE CITAÇÕES | 4 |
| TOTAL COMO AUTOR | 9 |
| TOTAL COMO EDITOR | 0 |
| PRIMEIRO ANO DE PUBLICAÇÃO | 1999 |
| ANO MAIS RECENTE DE PUBLICAÇÃO | 2019 |
| ÍNDICE H | 1 |
Compositional turnover and variation in Eemian pollen sequences in Europe
Diatom response to mid-Holocene climate in three small Arctic lakes in northernmost Finnmark
Palaeoclimatic reconstructions from lake sediment biological records can be challenging, due to variation in non-climatic factors, which alter ecosystem responses. To consider this, it is important to replicate a study regionally, so as to gain information on spatial variability of ecosystem response and the influence of site-specific conditions. Previous pollen-based palaeoclimatic records from three well-dated Arctic lake sites highlight the re…
Millennial-scale variability during the last glacial in vegetation records from Europe
A flexible approach to assessing synchroneity of past events using Bayesian reconstructions of sedimentation history
European vegetation during Marine Oxygen Isotope Stage-3
European vegetation during representative “warm” and “cold” intervals of stage-3 was inferred from pollen analytical data. The inferred vegetation differs in character and spatial pattern from that of both fully glacial and fully interglacial conditions and exhibits contrasts between warm and cold intervals, consistent with other evidence for stage-3 palaeoenvironmental fluctuations. European vegetation thus appears to have been an integral compo…
Comparison of climate model results with European vegetation and permafrost during oxygen isotope stage three
Oxygen isotope stage 3 (OIS3), an interstade between approximately 60,000 and 25,000 yr B.P., presents an ideal opportunity to compare high-resolution climate simulations with the geologic record. To facilitate this comparison, the results of a mesoscale climate model (RegCM2) embedded in the GENESIS GCM are utilized to drive a vegetation model (BIOME 3.5). The BIOME output is then compared with OIS3 compilations derived from pollen. The simulate…
Weichselian palynological records from southern Europe
Weichselian palynostratigraphy, palaeovegetation and palaeoenvironment; the record from Lago Grande di Monticchio, southern Italy
Rapid environmental changes in southern Europe during the last glacial period
Compositional turnover and variation in Eemian pollen sequences in Europe
Diatom response to mid-Holocene climate in three small Arctic lakes in northernmost Finnmark
Palaeoclimatic reconstructions from lake sediment biological records can be challenging, due to variation in non-climatic factors, which alter ecosystem responses. To consider this, it is important to replicate a study regionally, so as to gain information on spatial variability of ecosystem response and the influence of site-specific conditions. Previous pollen-based palaeoclimatic records from three well-dated Arctic lake sites highlight the re…
Rapid environmental changes in southern Europe during the last glacial period
Weichselian palynological records from southern Europe
Weichselian palynostratigraphy, palaeovegetation and palaeoenvironment; the record from Lago Grande di Monticchio, southern Italy
European vegetation during Marine Oxygen Isotope Stage-3
European vegetation during representative “warm” and “cold” intervals of stage-3 was inferred from pollen analytical data. The inferred vegetation differs in character and spatial pattern from that of both fully glacial and fully interglacial conditions and exhibits contrasts between warm and cold intervals, consistent with other evidence for stage-3 palaeoenvironmental fluctuations. European vegetation thus appears to have been an integral compo…
Comparison of climate model results with European vegetation and permafrost during oxygen isotope stage three
Oxygen isotope stage 3 (OIS3), an interstade between approximately 60,000 and 25,000 yr B.P., presents an ideal opportunity to compare high-resolution climate simulations with the geologic record. To facilitate this comparison, the results of a mesoscale climate model (RegCM2) embedded in the GENESIS GCM are utilized to drive a vegetation model (BIOME 3.5). The BIOME output is then compared with OIS3 compilations derived from pollen. The simulate…
A flexible approach to assessing synchroneity of past events using Bayesian reconstructions of sedimentation history
Millennial-scale variability during the last glacial in vegetation records from Europe
Diatom response to mid-Holocene climate in three small Arctic lakes in northernmost Finnmark
Palaeoclimatic reconstructions from lake sediment biological records can be challenging, due to variation in non-climatic factors, which alter ecosystem responses. To consider this, it is important to replicate a study regionally, so as to gain information on spatial variability of ecosystem response and the influence of site-specific conditions. Previous pollen-based palaeoclimatic records from three well-dated Arctic lake sites highlight the re…
Compositional turnover and variation in Eemian pollen sequences in Europe
Geology and Paleoclimatology Research (9 obras) · Geography (8 obras) · Physical geography (8 obras) · Climatology (6 obras) · Holocene (6 obras) · Geology (5 obras) · Glacial period (5 obras) · Paleontology (5 obras) · Ecology (4 obras) · Ecosystem (4 obras)