Anne Grunow
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Anne Grunow is a senior research scientist at
Ohio State University The Ohio State University, commonly called Ohio State or OSU, is a public land-grant research university in Columbus, Ohio. A member of the University System of Ohio, it has been ranked by major institutional rankings among the best publ ...
in the
Byrd Polar Research Center The Byrd Polar and Climate Research Center (BPCRC) is a polar, alpine, and climate research center at Ohio State University, The Ohio State University founded in 1960. History and research The Byrd Polar Research Center (BPRC) at Ohio State Un ...
. She is also the current director of the Polar Rock Repository. Grunow is a geologist specializing in Antarctic tectonics, with her research using methods from geochronology and paleomagnetism.


Early life and education

During her undergraduate years at
Wellesley College Wellesley College is a private women's liberal arts college in Wellesley, Massachusetts, United States. Founded in 1870 by Henry and Pauline Durant as a female seminary, it is a member of the original Seven Sisters Colleges, an unofficial g ...
, Grunow developed a love of geology. Her attachment to the outdoors comes from her childhood when she lived on a farm. This aligned well with the extensive fieldwork that a geology degree required. Grunow graduated from Wellesley College in 1981. She then continued her education at
Columbia University Columbia University (also known as Columbia, and officially as Columbia University in the City of New York) is a private research university in New York City. Established in 1754 as King's College on the grounds of Trinity Church in Manhatt ...
in New York City which marked the beginning of her travels to Antarctica in 1983. Grunow was the first woman to visit many of the remote West Antarctic outcrops in the Ellworth-Whitmore mountains, Thurston Island/Jones Mtns and Pine Island Bay. In 1989 she received her doctorate (PhD) in geology. Grunow worked under advisors Ian W.D. Dalziel and Dennis V. Kent on her dissertation entitled: Aspects of the evolution of the West Antarctic margin of Gondwanaland. Following this, Grunow received a NATO Post Doctoral Fellowship from 1991 to 1993 at the
University of Oxford , mottoeng = The Lord is my light , established = , endowment = £6.1 billion (including colleges) (2019) , budget = £2.145 billion (2019–20) , chancellor ...
. She later worked with Terry Wilson and Richard E. Hanson on the research paper:
Gondwana Gondwana () was a large landmass, often referred to as a supercontinent, that formed during the late Neoproterozoic (about 550 million years ago) and began to break up during the Jurassic period (about 180 million years ago). The final stages ...
assembly: The View from Southern Africa and East
Gondwana Gondwana () was a large landmass, often referred to as a supercontinent, that formed during the late Neoproterozoic (about 550 million years ago) and began to break up during the Jurassic period (about 180 million years ago). The final stages ...
. Their work was published in the ''Journal of Geodynamics'' in 1997.


Career and research

In 1989, she started as a university postdoctoral fellow and then research scientist at
Ohio State University The Ohio State University, commonly called Ohio State or OSU, is a public land-grant research university in Columbus, Ohio. A member of the University System of Ohio, it has been ranked by major institutional rankings among the best publ ...
in the
Byrd Polar Research Center The Byrd Polar and Climate Research Center (BPCRC) is a polar, alpine, and climate research center at Ohio State University, The Ohio State University founded in 1960. History and research The Byrd Polar Research Center (BPRC) at Ohio State Un ...
. Now a senior research scientist at Ohio State, she is also the director of the Polar Rock Repository. Her expertise includes geology and earth science, geochronology, tectonics, paleomagnetism, and polar geology. Her research centers on Antarctic Tectonics and she has led research teams to the Antarctic Peninsula and the Transantartic Mountains. Some of Anne Grunow's most cited and notable work includes her research on Pan-African deformation and the potential links to the lapetus opening. This research centered around data collections dating back to the late
Neoproterozoic The Neoproterozoic Era is the unit of geologic time from 1 billion to 538.8 million years ago. It is the last era of the Precambrian Supereon and the Proterozoic Eon; it is subdivided into the Tonian, Cryogenian, and Ediacaran periods. It is ...
era, and how they demonstrated a temporal correlation between Pan-African deformation and the Iapetus ocean basin closing. Another one of Grunow's most cited research paper was on the changing magmatic and tectonic styles along the paleo‐Pacific margin of
Gondwana Gondwana () was a large landmass, often referred to as a supercontinent, that formed during the late Neoproterozoic (about 550 million years ago) and began to break up during the Jurassic period (about 180 million years ago). The final stages ...
and the onset of early
Paleozoic The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ' ...
magmatism in Antarctica. This research focused on the early
Cambrian The Cambrian Period ( ; sometimes symbolized C with bar, Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million ...
Period tectonics and its association with volcanic arc magmatism . Her research has also been implemented in the ''
Global Change Master Directory {{Notability, date=May 2022 The Global Change Master Directory holds more than 28,000 data set descriptions, known as DIFs (Directory Interchange Format). This format is compatible with the Federal Geographic Data Committee's (FGDC) standard and th ...
'' and published in ''
Journal of Geophysical Research The ''Journal of Geophysical Research'' is a peer-reviewed scientific journal. It is the flagship journal of the American Geophysical Union. It contains original research on the physical, chemical, and biological processes that contribute to the un ...
''. Her work was noted by the
United States Antarctic Program The United States Antarctic Program (or USAP; formerly known as the United States Antarctic Research Program or USARP and the United States Antarctic Service or USAS) is an organization of the United States government which has presence in the A ...
, which commented on the benefit of her work and the Polar Rock Repository's ability to provide samples from Antarctica to a variety of scientific sources for study. Grunow was also active in tectonics research of the Avalon Terrane in New England with Wellesley College mentor, Margaret Thompson. They have published many articles on the Boston Basin and it's evolution in the late Neoproterozoic to early Cambrian. She also conducted research on Neoproterozoic rocks near Corumba, Brazil and Puerto Suarez, Bolivia. Results from this work with colleague Loren Babcock have been published.


Publications

* New paleomagnetic data from the
Antarctic Peninsula The Antarctic Peninsula, known as O'Higgins Land in Chile and Tierra de San Martín in Argentina, and originally as Graham Land in the United Kingdom and the Palmer Peninsula in the United States, is the northernmost part of mainland Antarctic ...
and their tectonic implications * The implications for
Gondwana Gondwana () was a large landmass, often referred to as a supercontinent, that formed during the late Neoproterozoic (about 550 million years ago) and began to break up during the Jurassic period (about 180 million years ago). The final stages ...
of new
Ordovician The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start ...
paleomagnetic data from
igneous rock Igneous rock (derived from the Latin word ''ignis'' meaning fire), or magmatic rock, is one of the three main The three types of rocks, rock types, the others being Sedimentary rock, sedimentary and metamorphic rock, metamorphic. Igneous rock ...
s in southern
Victoria Land Victoria Land is a region in eastern Antarctica which fronts the western side of the Ross Sea and the Ross Ice Shelf, extending southward from about 70°30'S to 78°00'S, and westward from the Ross Sea to the edge of the Antarctic Plateau. It ...
,
East Antarctica East Antarctica, also called Greater Antarctica, constitutes the majority (two-thirds) of the Antarctic continent, lying on the Indian Ocean side of the continent, separated from West Antarctica by the Transantarctic Mountains. It lies almost ...
*Pan-African deformation and the potential links to the lapetus opening * The changing magmatic and tectonic styles along the paleo‐Pacific margin of
Gondwana Gondwana () was a large landmass, often referred to as a supercontinent, that formed during the late Neoproterozoic (about 550 million years ago) and began to break up during the Jurassic period (about 180 million years ago). The final stages ...
and the onset of early
Paleozoic The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ' ...
magmatism in Antarctica *
Gondwana Gondwana () was a large landmass, often referred to as a supercontinent, that formed during the late Neoproterozoic (about 550 million years ago) and began to break up during the Jurassic period (about 180 million years ago). The final stages ...
assembly: The view from Southern Africa and East
Gondwana Gondwana () was a large landmass, often referred to as a supercontinent, that formed during the late Neoproterozoic (about 550 million years ago) and began to break up during the Jurassic period (about 180 million years ago). The final stages ...
* Magnetic Data from Subglacial Clasts,
West Antarctic Ice Sheet The Western Antarctic Ice Sheet (WAIS) is the segment of the continental ice sheet that covers West Antarctica, the portion of Antarctica on the side of the Transantarctic Mountains that lies in the Western Hemisphere. The WAIS is classified as ...


Awards and honors

* Fellow of the Geological Society of America * Chairman of the SCAR Antarctic Expert Group on Antarctic Geological Heritage and Geoconservation * Nominated to the U.S Board on Geographic Names * Antarctic peak named after her (Grunow Peak) * Antarctic Service Medal


References

{{DEFAULTSORT:Grunow, Anne Living people Year of birth missing (living people) Scientists from New Jersey Absegami High School alumni People from Galloway Township, New Jersey Wellesley College alumni Columbia University alumni 20th-century American geologists 21st-century American geologists American women geologists Ohio State University staff Fellows of the Geological Society of America 20th-century American women scientists 21st-century American women scientists