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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Admiralty Bay (1)
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Antarctica
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Antarctic ice sheet
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East Antarctic ice sheet (2)
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West Antarctic ice sheet (1)
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Antarctic Peninsula (1)
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Victoria Land
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Arctic region
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Primary terms
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Deep Sea Drilling Project
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Leg 28
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Integrated Ocean Drilling Program
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Expedition 318
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O-18/O-16 (3)
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lava (1)
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barium (1)
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iron (1)
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metamorphic rocks
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meteorology (1)
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Ocean Drilling Program
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Leg 188
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ODP Site 1165 (1)
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orogeny (2)
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oxygen
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soils (3)
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East Antarctic Ice Sheet variability during the middle Miocene Climate Transition captured in drill cores from the Friis Hills, Transantarctic Mountains
Reconciling persistent sub-zero temperatures in the McMurdo Dry Valleys, Antarctica, with Neogene dynamic marine ice-sheet fluctuations
Geochemistry of contrasting stream types, Taylor Valley, Antarctica
Abstract We report on a decade of fieldwork designed to determine the conditions required for erosion of Mars-like gully channels in the McMurdo Dry Valleys (MDV) of Antarctica. We have outlined the major factors in the morphological evolution of gullies in the Inland Mixed Zone of the MDV: (1) the distribution of ice sources; (2) the temporal aspects of ice melting; and (3) the relative significance of melting events in gullies. We show that significant erosion of gully channels can be achieved if geometrical and environmental conditions combine to concentrate ice where it can rapidly melt. In contrast, annual melting of surface ice and snow deposits during late-season discharge events contribute to transport of water, but flux rarely surpasses the infiltration capacity of the active layer. These small discharge events do not erode channels of significant width. Even when the flux is sufficient to carve a c. 10–20 cm deep channel during late summer (January–February) runoff, these small channels seldom persist through multiple seasons, because they are seasonally muted and filled with aeolian deposits. We briefly discuss the application of these results to the study of gully systems on Mars. Supplementary material: Eight videos showing activity and events are available at https://doi.org/10.6084/m9.figshare.c.3935992
Barium and barite dynamics in Antarctic streams
Pioneers in Antarctic research: Lois Jones and her all-woman science team explore the geochemistry of the Dry Valleys
ABSTRACT Today, women make up about one-third of all scientists who go to Antarctica for research. However, it was just under fifty years ago that the first woman principal investigator was funded by the then United States Antarctic Research Program, which today is known as the United States Antarctic Program (USAP). Colin Bull, Director of the Institute for Polar Studies (today called Byrd Polar and Climate Research Center or BPCRC), had advocated for women to be allowed in Antarctica since 1959. At the time, female graduate students worked on Antarctic research, but were not able to conduct their own fieldwork; thus they relied on men to collect samples and gather the data they needed up until the ban was lifted. One such woman was Lois Jones, whose Ph.D. adviser was The Ohio State University geochemist Dr. Gunter Faure. Once she completed her dissertation on the geochemistry of the McMurdo Dry Valleys, she submitted a proposal for fieldwork in Antarctica to be funded by the USAP. Her proposal was approved and she and her field party of three other women went to Antarctica during the austral summer of 1969–1970. In addition to fieldwork in the Dry Valleys, they gained the honor of being four of the first six women to make it to the South Pole. While the women faced many challenges and chauvinism, their field season was successful. This has led to a legacy of women in Antarctica. Faculty, alumna, and staff from The Ohio State University figure prominently in this story, due to the affiliation of the Byrd Polar and Climate Research Center with Ohio State.