| Helen Bostock | |
| Nationality: | Australian |
| Fields: | Paleoceanography |
| Workplaces: | University of Queensland |
| Alma Mater: | BSc, MSc Jesus College, Cambridge PhD Australian National University |
Helen Clare Bostock, is an oceanographer researching past, present and future conditions in the Southern Ocean. In 2011 she led a research voyage on board the RV Tangaroa to the Solander Trough region of the Tasman Sea. Two years later she was deputy voyage leader for an expedition to the Mertz Polynya, Antarctica. In 2016 she was awarded the McKay Hammer, for her combined research achievements between 2013 and 2016.
Bostock was born in Perth, Australia and grew up there, Nigeria, the Netherlands, Oman, Scotland, England, and New Zealand. She went to high school in Abbotsholme School in England.
Bostock was awarded her PhD by the Australian National University, Australia. Her work focused on geochemical tracing of the intermediate and surface waters in the Tasman Sea and was supervised by Bradley Opdyke and John Marshall. Prior to that she completed a MSc and BSc at Jesus College, University of Cambridge, UK.
Her early career was as a researcher at Geoscience Australia. For a time she also worked as the coordinator for the Australian ODP/IODP Office, coordinating the activities and developing proposals on behalf of the marine geoscience community in Australia in the transition between the end of the Ocean Drilling Program (in 2003) and joining the Integrated Ocean Drilling Program. She then joined the New Zealand National Institute of Water and Atmospheric Research prior to taking up an Associate Professorship at the University of Queensland.
Bostock's primary research focus is on the paleoceanography and oceanography of the Southwest Pacific and Southern Ocean using sedimentology, microfossils, isotopes and geochemical tracers to understand present and past changes in ocean circulation and their influence on climate.[1] She also works on sediment transport processes and sources, and multidisciplinary topics such as Ocean Acidification,[2] climate change, the onset of the Anthropocene and paleo-seismicity.
The voyage that she led to the Solander Trough region, named after Daniel Solander, directly south of the south-west corner of New Zealand (Puysegur Point) was part of a sequence of voyages seeking to characterise the present and past configuration and mechanics controlling the Subtropical front which is a significant oceanographic feature found in both hemispheres but with the southern front extending more or less continually around the globe.[3]
She was deputy voyage leader for a 2013 expedition to the Mertz polynya region in East Antarctica.[4] The polynya was consistently found in the lee of the Mertz Glacier Tongue until its break-away in 2010.[5] This large floating glacier was named after Xavier Mertz who lost his life in the region in 1913 on the Australasian Antarctic Expedition led by Douglas Mawson. The voyage sought to determine changes brought about by the glacier calving.[6]
She has researched and communicated on the concept of the Anthropocene.[7] A major conclusion of the work was that, in the longer-term future, tectonic and volcanic processes are likely to have a stronger impact on New Zealand, as a landmass, than foreseeable future climate change.[8]
In 2012 she was the scientist aboard HMNZS Canterbury on a voyage to Raoul Island in the Kermadec Ridge region to the northeast of New Zealand. Along with NZ Department of Conservation (New Zealand) staff, a science team sent by Pew Environment Group (including Rebecca Priestley), and a group of students on a Sir Peter Blake Expedition. They left New Zealand in August, a day after both Mount Tongariro and Whakaari / White Island erupted, which meant that the volcanologist who was scheduled to be on board the ship remained in New Zealand.[9] Very early into the voyage they encountered massive pumice rafts caused by the 2012 Kermadec Islands eruption.[10] This was so large that it was visible from trans-Pacific aircraft.[11]
In 2000 Bostock led a climbing expedition to Louise Boyd Land in western Greenland, (73°30' N, 28°00' W). The expedition achieved 15 first ascents on formations over 2000 meters high, three granite rock spires and a granite wall were discovered and climbed and two new routes were put up on the previously unclimbed northwest face of Petermann Bjerg. As well as first ascents, they put up two new routes on the unclimbed northwest face of the mountain, the highest (2,943 m) in the High Arctic. All climbing was carried out during the night when it was colder and the snow was in better condition.[12]
In 2016 she was awarded the New Zealand Geoscience Society top award, the McKay Hammer, for a body of research work between 2013 and 2016.[13] Previous winners include Harold Wellman the discoverer of the Alpine Fault. She was also awarded the 2004 KSW Campbell award for teaching at the Australian National University – named in honour of Ken Campbell.