Herbert E Wright
Biographic Data
| ID | 5649417 |
|---|---|
| NAME | Herbert E Wright |
| GIVEN NAMES | Herbert E |
| FAMILY NAME | Wright |
| SIGNATURE | WRIGHT H E |
| AFFILIATIONS | University of Minnesota |
| VERIFIED | No |
| TOTAL WORKS | 5 |
| TOTAL CITATIONS | 16 |
| WORKS AS AUTHOR | 5 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1972 |
| LATEST PUBLICATION YEAR | 2014 |
| H-INDEX | 2 |
The potential of stomata analysis in conifers to estimate presence of conifer trees
Timing of Atmospheric Precipitation in the Zagros Mountains Inferred from a Multi-Proxy Record from Lake Mirabad, Iran
A sediment core 7.2 m long from Lake Mirabad, Iran, was examined for loss-on-ignition, mineralogy, oxygen-isotopic composition of authigenic calcite, and trace-element composition of ostracodes to complement earlier pollen and ostracode-assemblage studies. Pollen, ostracode-inferred lake level, and high Sr/Ca ratios indicate that the early Holocene (10000 to 6500 cal yr BP) was drier than the late Holocene. Low δ 18 O values during this interval …
Elevational gradients during the Late-Glacial/Holocene vegetational transition in southern Bulgaria
Diatom-based conductivity reconstruction and palaeoclimatic interpretation of a 40-ka record from Lake Zeribar, Iran
Sediment cores from Lake Zeribar in the Zagros Mounitains of western Iran provide a record of changes in the diatom flora since about 40 ka. Conductivity transfer functionis applied to diatom records from the lake indicate generally higher conductivity during the Last Glacial Maximum and Lateglacial, especially between 15.0 and 10.5 ka. This observation is consistent with previous interpretations of relatively arid conditions during this interval…
Interglacial and Postglacial Climates
Pollen studies of the four European interglacial intervals indicate a strong similarity in vegetational sequence: a pretemperate phase (I) marks the late glacial, early temperate (II) and late temperate (III) phases mark the interglacial proper, and a posttemperate phase (IV) represents the beginning of the next cold period. A grossly similar record is now known for the last interglacial (Sangamon) of central and southeastern United States. The H…
The potential of stomata analysis in conifers to estimate presence of conifer trees
Diatom-based conductivity reconstruction and palaeoclimatic interpretation of a 40-ka record from Lake Zeribar, Iran
Sediment cores from Lake Zeribar in the Zagros Mounitains of western Iran provide a record of changes in the diatom flora since about 40 ka. Conductivity transfer functionis applied to diatom records from the lake indicate generally higher conductivity during the Last Glacial Maximum and Lateglacial, especially between 15.0 and 10.5 ka. This observation is consistent with previous interpretations of relatively arid conditions during this interval…
Elevational gradients during the Late-Glacial/Holocene vegetational transition in southern Bulgaria
Interglacial and Postglacial Climates
Pollen studies of the four European interglacial intervals indicate a strong similarity in vegetational sequence: a pretemperate phase (I) marks the late glacial, early temperate (II) and late temperate (III) phases mark the interglacial proper, and a posttemperate phase (IV) represents the beginning of the next cold period. A grossly similar record is now known for the last interglacial (Sangamon) of central and southeastern United States. The H…
Diatom-based conductivity reconstruction and palaeoclimatic interpretation of a 40-ka record from Lake Zeribar, Iran
Sediment cores from Lake Zeribar in the Zagros Mounitains of western Iran provide a record of changes in the diatom flora since about 40 ka. Conductivity transfer functionis applied to diatom records from the lake indicate generally higher conductivity during the Last Glacial Maximum and Lateglacial, especially between 15.0 and 10.5 ka. This observation is consistent with previous interpretations of relatively arid conditions during this interval…
Timing of Atmospheric Precipitation in the Zagros Mountains Inferred from a Multi-Proxy Record from Lake Mirabad, Iran
A sediment core 7.2 m long from Lake Mirabad, Iran, was examined for loss-on-ignition, mineralogy, oxygen-isotopic composition of authigenic calcite, and trace-element composition of ostracodes to complement earlier pollen and ostracode-assemblage studies. Pollen, ostracode-inferred lake level, and high Sr/Ca ratios indicate that the early Holocene (10000 to 6500 cal yr BP) was drier than the late Holocene. Low δ 18 O values during this interval …
Elevational gradients during the Late-Glacial/Holocene vegetational transition in southern Bulgaria
The potential of stomata analysis in conifers to estimate presence of conifer trees
Geology and Paleoclimatology Research (5 works) · Geography (4 works) · Holocene (4 works) · Physical geography (4 works) · Archaeology and ancient environmental studies (3 works) · Climatology (3 works) · Geology (3 works) · Glacial period (3 works) · Pleistocene-Era Hominins and Archaeology (3 works) · Pollen (3 works)