Phragging Out

Abstract: Phragmites australis is a fast growing invasive species native to Eurasia. Its faculatively clonal method of replicating allows it to create dense stands that drown out most other species, creating monocultures nearly everywhere they are found. A key aspect to mitigating their spread is knowing where they are, which is largely done by mapping … Read more

Spectral Differences Identified in a P. Australis Monoculture in the Marshlands of the Connecticut River Estuary

Phragmites australis is a fast-growing invasive species native to Eurasia. Its facultatively clonal method of replicating allows it to create dense stands that drown out most other species, creating monocultures nearly everywhere they are found. A key aspect to mitigating their spread is knowing where they are, which is largely done by mapping and remote … Read more

Below Iceberg Alley: Tracking Antarctic ice loss from previous global warm periods

Abstract: The International Ocean Drilling Program (IODP) Site U1537 is located in the Dove Basin off the northeast coast of the Antarctic Peninsula in the Scotia Sea, a region known as “Iceberg Alley.”  After an iceberg breaks off the Antarctic Ice Sheet, it travels northward towards “Iceberg Alley” via the Antarctic Circumpolar Current, and the … Read more

Utilization of Quartz Micro-Textures to Determine Antarctic Ice-Sheet Dynamics

Abstract: Ice-rafted sediment is deposited into the deep sea through abrasive and crushing processes causing the micromorphology of embedded quartz grains to alter. As quartz are high in silica and not easily eroded, their features could be paramount for accurate rebuilding of past ice-cap levels. Paleoclimate reconstructions require a quantitative analysis of ice-rafted debris (IRD)for … Read more

Optimising Sample Preparation for the Investigation of Bottom Current Strengths of the Scotia Sea during the Pliocene

Live Poster Session: Zoom Link Abstract: Seafloor sediment is commonly used to give insight into the climatic history of planet Earth. Seafloor sediment is more suitable for this function than terrestrial sediment because of how dynamic the land on Earth is, and because of natural disasters that periodically affect the Earth’s topographical and geological features. … Read more

Deep-sea Antarctic Ecosystems 1 million years ago: Trace Fossils in the Sediment Record as Analogs for Modern Day Ecosystem Dynamics

Abstract: In the Drake Passage, between Antarctica and South America, bioturbation increases during warmer (open ocean) intervals during Marine Isotope 31. Marine Isotope 31 is a period of time approximately 1 million years ago that is considered an analog to the modern day Antarctic climate because it is the most recent geological warm period and … Read more