Diana Eleanor Northup | |
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Alma mater | University of New Mexico West Virginia University University of Illinois Urbana-Champaign |
Scientific career | |
Institutions | University of New Mexico |
Thesis | Geomicrobiology of caves (2002) |
Diana E. Northup is an American microbiologist, speleologist, ecologist, Visiting Professor of Biology, and Professor Emerita of Library Sciences with the University of New Mexico. Her research focuses on the microbial ecology of caves around the world. Dr. Northup is a Fellow of the National Speleological Society and the Cave Research Foundation. She wrote the Wiley textbook Microbial Ecology. [1] [ page needed ] She was awarded the National Speleological Society Science Prize in 2013. [2]
Northup was an undergraduate student at West Virginia University, where she studied political science. She moved to the University of Illinois Urbana-Champaign for graduate studies, where she earned a Master's of Library Science in 1972. Northup moved to the University of New Mexico, where she earned a Master's degree in biology in 1988. She remained at the University of New Mexico for her doctoral research, where she studied the geomicrobiology of caves. [3] [ page needed ]
Northup is a visiting associate professor at the University of New Mexico where she started the Subsurface Life In Mineral Environments (SLIME) team. [4] In particular, Northup studies the colorful ferromanganese deposits that line the walls of Lechuguilla and Spider Cave in Carlsbad Caverns National Park. [5] Her work on the Lechuguilla Cave was featured in a PBS Nova episode, "The Mysterious Life of Caves." [5] [6] [7] She is also interested in the hydrogen sulfide cave known as'Cueva de las Sardinas' or 'Cueva de Villa Luz' in Tabasco. [8] [7]
Northup was elected Fellow of the National Speleological Society in 1992 [9] , awarded their Science Prize in 2013 [2] , and presented a Luminary talk in 2015 [10] .
In 2011, Northup gave a TEDx talk about how she got started in caving and how that influences her mentoring of students [11] .
Karst is a topography formed from the dissolution of soluble carbonate rocks such as limestone and dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering-resistant rocks such as quartzite given the right conditions.
Speleology is the scientific study of caves and other karst features, as well as their composition, structure, physical properties, history, ecology, and the processes by which they form (speleogenesis) and change over time (speleomorphology). The term speleology is also sometimes applied to the recreational activity of exploring caves, but this is more properly known as caving, potholing, or spelunking. Speleology and caving are often connected, as the physical skills required for in situ study are the same.
A stalagmite is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically composed of calcium carbonate, but may consist of lava, mud, peat, pitch, sand, sinter, and amberat.
At 150.4 miles (242.0 km), Lechuguilla Cave is the eighth-longest explored cave in the world and the second deepest in the continental United States. It is most famous for its unusual geology, rare formations, and pristine condition.
Snottite, also snoticle, is a microbial mat of single-celled extremophilic bacteria which hang from the walls and ceilings of caves and are similar to small stalactites, but have the consistency of nasal mucus. In the Frasassi Caves in Italy, over 70% of cells in Snottite have been identified as Acidithiobacillus thiooxidans, with smaller populations including an archaeon in the uncultivated 'G-plasma' clade of Thermoplasmatales (>15%) and a bacterium in the Acidimicrobiaceae family (>5%).
Sistema Ox Bel Ha is a cave system in Quintana Roo, Mexico. It is the longest explored underwater cave in the world and ranks second including dry caves. As of January 2024 the surveyed length is 496.8 kilometers (308.7 mi) of underwater passages. There are more than 160 cenotes in the system.
Zacatón is a thermal water-filled sinkhole belonging to the Zacatón system - a group of unusual karst features located in Aldama Municipality near the Sierra de Tamaulipas in the northeastern state of Tamaulipas, Mexico. At a total depth of 339 meters (1,112 ft), it is one of the deepest known water-filled sinkholes in the world.
Sistema Sac Actun is an underwater cave system situated along the Caribbean coast of the Yucatán Peninsula with passages to the north and west of the city of Tulum. Discovery of a connection to Sistema Dos Ojos in 2018 made it the longest known underwater cave system. As of January 2023, it is the second longest underwater cave system in the world, only surpassed by Sistema Ox Bel Ha.
Dr. Hazel A. Barton is an English born microbiologist, geologist and cave diving explorer, interested in extremophile microorganisms. She is a Professor and Director of the Integrated Bioscience Program at the University of Akron and has appeared in several documentaries.
Penelope J. Boston is a speleologist and astrobiologist. She was associate director of the National Cave and Karst Research Institute in Carlsbad, New Mexico, along with founding and directing the Cave and Karst Studies Program at New Mexico Institute of Mining and Technology in Socorro. Among her research interests are geomicrobiology of caves and mines, extraterrestrial speleogenesis, and space exploration and astrobiology generally.
The Wittenberg University Speleological Society (WUSS) is a student-run grotto of the National Speleological Society (NSS) created in 1980, dedicated to the advancement of speleology. WUSS has more than 500 members, current and past students, faculty and staff of Wittenberg University, as well as community members dedicated to the scientific study, exploration, and preservation of caves and karst environments. The organization is based out of Wittenberg University in Springfield, Ohio.
The Butler Cave Conservation Society (BCCS) is a 501(c)(3) non-profit Virginia corporation dedicated to the conservation, exploration, survey, preservation, and scientific study of the caves and karst in and around Burnsville Cove, Virginia.
Tears of the Turtle Cave is located in the Bob Marshall Wilderness in western Montana and is currently the deepest known limestone cave in the United States since passing New Mexico's Lechuguilla cave in 2014. As of August 2024, the cave is known to be 2,477 feet (755 m) deep and 1.88 miles (3,030 m) long. The cave consists mostly of narrow fissure passages passing over approximately 50 short rope drops. The cave has a temperature of 37 °F (3 °C), and it is muddy and poorly decorated.
Matthew D. Covington is an American speleologist, most known for his work in hydrogeology and geomorphology, especially in the field of mathematical modeling of karst systems, as well as by his contribution to Cueva Cheve project in Mexico, since 1999.
Nora Noffke is an American geologist who is a professor in the Department of Ocean and Earth Sciences, Old Dominion University in Norfolk, Virginia, USA. Noffke's research focuses on the sedimentology of biofilm forming sedimentary structures in modern aquatic environments, where clastic deposits dominate. Such structures occur in the fossil record as well. Her studies are interdisciplinary combining sedimentology with microbiology, geochemistry, and mineralogy.
Patricia Kambesis is an American caver, cartographer and educator.
Annette Summers Engel is an American earth scientist who is Donald and Florence Jones Professor of Aqueous Geochemistry at the University of Tennessee. Her research considers how microbes interact with rocks and minerals. She was elected Fellow of the American Association for the Advancement of Science in 2019.
Friars Hole Cave System is a cave in West Virginia's Greenbrier and Pocahontas counties. First surveyed in the 1960s, it is one of the longest in the United States and the world.
Kathleen Hoey Lavoie was an American microbiologist and explorer who was Professor of Biological Sciences at the State University of New York at Plattsburgh. Lavoie was a Fellow of the National Speleological Society and the Cave Research Foundation. She was a specialist in biospeleology, and, in particular, the Mammoth Cave National Park in Kentucky.