HelioWebBrandon University, Canada
flowchart
I[Brandon University, Canada]
PI["Parent Institutions (0)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (20)"]
CA["Linked Collaborating Authors (0)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
click PI "#parent-institutions"
click CI "#child-institutions"
click AW "#affiliated-works"
click CA "#collaborating-authors"
Parent Institutions [?]
Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- Pollen analysis of Early Eocene laminated sediments from the Okanagan Highlands, British Columbia
- Arctic Climate and Terrestrial Vegetation Responses During the Middle to Late Eocene and Early Oligocene: Colder Winters Preceded Cool-Down.
- Increased sensitivity of Arctic climate to atmospheric CO2 during the Pliocene
- Eocene Precipitation: How Wet and Where? A Model-Proxy Comparison
- Paleobotanical Evidence for Coupling of Temperature and pCO2 during the Early Eocene Climatic Optimum
- Warm Arctic terrestrial surface temperatures during the Pliocene: exploring potential feedback mechanisms
- Eocene precipitation: How wet do greenhouse climates get? (Invited)
- Eocene precipitation: a global monsoon?
- Arctic Climate during Eocene Hyperthermals: Wet Summers on Ellesmere Island?
- Forcing of Global Glacier Fluctuations by Sunspot Activity during the Holocene
- Multi-proxy Paleoclimate and CO<SUB>2</SUB> Reconstruction from the Latest Middle Eocene Sedimentary Fill of a Subarctic Kimberlitic Maar Crater
- Arctic vegetation, temperature, and hydrology during early Eocene transient global warming events.
- Early Eocene climates from mid-latitude upland and high-latitude Arctic environments in Canada: insights from Palaeobotanical proxies
- Palynostratigraphy of the early Paleogene Margaret Formation at Stenkul Fiord, Ellesmere Island, Nunavut, Canada: a comprehensive microfossil record of Arctic hyperthermal (ETM-2) vegetation
- Are sedimentary plant wax n-alkanes derived from conifers? Insights from rarely preserved early Cenozoic conifer-dominated landscapes
- Deciphering Southwest Pacific Eocene temperature proxy mismatches
- Paleobotanical proxy-based reconstructions of early Eocene climates from mid- to high latitudes in Canada.
- Pollen-based reconstruction of Paleocene-Eocene climate in the mid-Atlantic region
- Intensification of the hydrological cycle during Eocene `greenhouse' climates
- Terrestrial Temperatures during the Early Eocene Hyperthermals from the Canadian Arctic (Stenkul Fiord, Ellesmere Island): Evidence from a brGDGT Peat-Specific Temperature Proxy.