Jerry F McManus
Biographic Data
| ID | 5601160 |
|---|---|
| NAME | Jerry F McManus |
| GIVEN NAMES | Jerry F |
| FAMILY NAME | McManus |
| SIGNATURE | MCMANUS J F |
| AFFILIATIONS | Woods Hole Oceanographic Institution |
| ORCID | 0000-0002-7365-1600 |
| VERIFIED | Yes |
| TOTAL WORKS | 8 |
| TOTAL CITATIONS | 18 |
| WORKS AS AUTHOR | 8 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1971 |
| LATEST PUBLICATION YEAR | 2018 |
| H-INDEX | 1 |
Radiocarbon and Stable Isotope Evidence for Changes in Sediment Mixing in the North Pacific over the Past 30 kyr
Deep-sea sediment mixing by bioturbation is ubiquitous on the seafloor, and it can be an important influence on the fidelity of paleoceanographic records. Bioturbation can be difficult to quantify, especially in the past, but diffusive models based on radioactive tracer profiles have provided a relatively successful approach. However, a singular, constant mixing regime is unlikely to prevail in a region where dynamic oceanographic changes in the …
Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes
Last Interglacial Climates
The last interglacial, commonly understood as an interval with climate as warm or warmer than today, is represented by marine isotope stage (MIS) 5e, which is a proxy record of low global ice volume and high sea level. It is arbitrarily dated to begin at approximately 130,000 yr B.P. and end at 116,000 yr B.P. with the onset of the early glacial unit MIS 5d. The age of the stage is determined by correlation to uranium–thorium dates of raised cora…
Thermohaline Circulation and Prolonged Interglacial Warmth in the North Atlantic
Deep-sea sediment cores provide spatially coherent evidence for the climatic and hydrographic conditions in the subpolar North Atlantic during the last interglaciation. Taken together with similarly high-resolution terrestrial sequences, these records indicate a regional climatic progression, beginning with the extreme and variable climate late in the penultimate glaciation, continuing through a relatively stable climatic optimum during the inter…
Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records
Correlations between climate records from North Atlantic sediments and Greenland ice
Evidence for massive discharges of icebergs into the North Atlantic ocean during the last glacial period
The Early Settlement of Scotland
The Mesolithic settlement at Morton lies some six miles north-north-west of St. Andrews in Fife, Scotland (fig. 1). The area around the site, north-eastern Fife, is surrounded on three sides by water, and projects as a blunt peninsula into the North Sea. The river Eden and the Firth of Tay serve as southern and northern boundaries of this peninsula, which consists today principally of the wind-deposited sands of Tentsmuir. The area of Tentsmuir, …
The Early Settlement of Scotland
The Mesolithic settlement at Morton lies some six miles north-north-west of St. Andrews in Fife, Scotland (fig. 1). The area around the site, north-eastern Fife, is surrounded on three sides by water, and projects as a blunt peninsula into the North Sea. The river Eden and the Firth of Tay serve as southern and northern boundaries of this peninsula, which consists today principally of the wind-deposited sands of Tentsmuir. The area of Tentsmuir, …
Radiocarbon and Stable Isotope Evidence for Changes in Sediment Mixing in the North Pacific over the Past 30 kyr
Deep-sea sediment mixing by bioturbation is ubiquitous on the seafloor, and it can be an important influence on the fidelity of paleoceanographic records. Bioturbation can be difficult to quantify, especially in the past, but diffusive models based on radioactive tracer profiles have provided a relatively successful approach. However, a singular, constant mixing regime is unlikely to prevail in a region where dynamic oceanographic changes in the …
The Early Settlement of Scotland
The Mesolithic settlement at Morton lies some six miles north-north-west of St. Andrews in Fife, Scotland (fig. 1). The area around the site, north-eastern Fife, is surrounded on three sides by water, and projects as a blunt peninsula into the North Sea. The river Eden and the Firth of Tay serve as southern and northern boundaries of this peninsula, which consists today principally of the wind-deposited sands of Tentsmuir. The area of Tentsmuir, …
Evidence for massive discharges of icebergs into the North Atlantic ocean during the last glacial period
Correlations between climate records from North Atlantic sediments and Greenland ice
Last Interglacial Climates
The last interglacial, commonly understood as an interval with climate as warm or warmer than today, is represented by marine isotope stage (MIS) 5e, which is a proxy record of low global ice volume and high sea level. It is arbitrarily dated to begin at approximately 130,000 yr B.P. and end at 116,000 yr B.P. with the onset of the early glacial unit MIS 5d. The age of the stage is determined by correlation to uranium–thorium dates of raised cora…
Thermohaline Circulation and Prolonged Interglacial Warmth in the North Atlantic
Deep-sea sediment cores provide spatially coherent evidence for the climatic and hydrographic conditions in the subpolar North Atlantic during the last interglaciation. Taken together with similarly high-resolution terrestrial sequences, these records indicate a regional climatic progression, beginning with the extreme and variable climate late in the penultimate glaciation, continuing through a relatively stable climatic optimum during the inter…
Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records
Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes
Radiocarbon and Stable Isotope Evidence for Changes in Sediment Mixing in the North Pacific over the Past 30 kyr
Deep-sea sediment mixing by bioturbation is ubiquitous on the seafloor, and it can be an important influence on the fidelity of paleoceanographic records. Bioturbation can be difficult to quantify, especially in the past, but diffusive models based on radioactive tracer profiles have provided a relatively successful approach. However, a singular, constant mixing regime is unlikely to prevail in a region where dynamic oceanographic changes in the …
Geology (7 works) · Geology and Paleoclimatology Research (7 works) · Oceanography (7 works) · Climatology (5 works) · Glacial period (5 works) · Geological formations and processes (4 works) · Methane Hydrates and Related Phenomena (4 works) · North Atlantic Deep Water (4 works) · Paleontology (4 works) · Thermohaline circulation (4 works)