Peter Barrett | |
---|---|
Born | Peter John Barrett 11 August 1940 Hamilton, New Zealand |
Alma mater | Ohio State University |
Known for | Discovery of the first tetrapod fossils (Antarctica, 1967) |
Spouse |
Maxine Frances Stone
(m. 1977) |
Children | 6 |
Scientific career | |
Institutions | Victoria University of Wellington |
Theses | |
Doctoral students | Rob McKay |
Other notable students | Nancy Bertler |
Peter John Barrett NZAM (born 11 August 1940) is a New Zealand geologist who came to prominence after discovering the first tetrapod fossils in Antarctica in 1967.[1]
Barrett was born in Hamilton on 11 August 1940, and educated at Hamilton High School.[2] He went on to study at Auckland University College from 1958 to 1962, graduating Bachelor of Science in 1961, and Master of Science in 1963.[2] The title of his master's thesis was The Te Kuiti group in the Waitomo-Te Anga area : a study of structures, sedimentation and paleogeography of calcareous sediments.[3]
Barrett married Maxine Frances Stone in 1977; the couple had six children.[2]
Barrett first went to Antarctica with the University of Wisconsin in 1962, but it was during his PhD with the Institute of Polar Studies at Ohio State University in 1966 and 1968 that Barrett discovered the early Triassic period tetrapod remains. His 1968 doctoral thesis at the Institute of Polar Studies had the title The post-glacial Permian and Triassic Beacon rocks in the Beardmore Glacier area, central Transantarctic Mountains, Antarctica.[4] After finishing his PhD, he took up a postdoctoral fellowship at Victoria University of Wellington to run an Antarctic expedition. Recent research has been core sampling in the Antarctic to determine historical conditions.[5]
He is currently a professor in the Antarctic Research Centre (ARC) at Victoria University of Wellington, and was director of the ARC from its founding in 1972 until 2007.[6] One of his PhD students was Nancy Bertler.[7] For many years he was the New Zealand representative on the Scientific Committee on Antarctic Research (SCAR).[8]
Barrett's notable students include Nancy Bertler and Rob McKay.[9]
In 1978, Barrett was awarded the Polar Medal, for good services as a member of New Zealand expeditions to Antarctica in 1974–1975.[10] In 2004, he received the Marsden Medal for his lifetime contributions to science in New Zealand.[11] In 2006, he received the SCAR President's Medal for outstanding achievement in Antarctic science.[12] In 2008, following the death of its patron Sir Edmund Hillary, the New Zealand Antarctic Society invited Barrett to become the new patron, which he accepted.[13] In the 2010 New Year Honours, Barrett was awarded the New Zealand Antarctic Medal for services to Antarctic science.[14] He was made an Honorary Fellow of the Geological Society in 2011.[8][15]
Barrett Glacier in the Prince Olav Mountains of Antarctica was named by the southern party of the 1963–1964 New Zealand Geological Survey Antarctic Expedition for Barrett, who was the party's geologist.[16]
New Zealander Peter Barrett discovered the first tetrapod remains in Antarctica in 1967. Subsequent research that identified the remains provided the first evidence that land vertebrates had roamed Antarctica when its climate was warm, and lent support to the then controversial theories of continental drift and Gondwanaland. But Barrett's contribution to Antarctic science goes beyond his 'serendipitous discovery' as a doctoral student. He has also been acknowledged as the 'supremo' of the geological drilling community in the Antarctic for his work in this area from the 1970s onwards.
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These early projects eventually led to the multi-national Cape Roberts Project, headed by Barrett, now the director of the Antarctic Research Centre at Victoria University. During the late 1990s, three holes drilled near the edge of the mountains recovered a remarkable 'sedimentary tape recorder', confirming that massive ice sheets have covered Antarctica since around 34 million years ago. However, the ice cover was highly dynamic, coming and going in response to perturbations in the Earth's orbit, known as Milankovitch cycles, which affect the amount of radiation the planet receives. For the past 15 million years, the size of the ice cap has been relatively stable.
Professor Barrett has been made an Honorary Fellow of the prestigious Geological Society of London, a title held by only 70 people worldwide.