Beryllium isotope signatures of ice shelves and sub-ice shelf circulation
dc.contributor.author | White, DA | en_AU |
dc.contributor.author | Fink, D | en_AU |
dc.contributor.author | Post, AL | en_AU |
dc.contributor.author | Simon, KJ | en_AU |
dc.contributor.author | Galton-Fenzi, BK | en_AU |
dc.contributor.author | Foster, S | en_AU |
dc.contributor.author | Fujioka, T | en_AU |
dc.contributor.author | Jeromson, MR | en_AU |
dc.contributor.author | Blaxell, M | en_AU |
dc.contributor.author | Yokoyama, Y | en_AU |
dc.date.accessioned | 2021-12-16T21:22:15Z | en_AU |
dc.date.available | 2021-12-16T21:22:15Z | en_AU |
dc.date.issued | 2019-01-01 | en_AU |
dc.date.statistics | 2021-11-16 | en_AU |
dc.description.abstract | Be isotopes are a useful tracer of sediment source and transport pathways but have not been widely tested in glacio-marine environments. We measured Be isotopes in a range of depositional environments from open marine, sub-ice shelf and subglacial settings throughout Prydz Bay, one of Antarctica's largest ice drainage systems. We find that strong sub-ice shelf and bottom current circulations can advect 10Be-rich open marine sediments into an ice shelf cavity, and 10Be-poor terrestrial sediments onto the continental shelf at the ice shelf outflow, meaning that 10Be concentrations reflect sub-ice shelf circulation patterns rather than depositional environment. However, HCl-extractable 10Be/9Be ratios can provide a more robust discrimination of sediment deposited in open marine and sub-ice shelf settings. Thus, Be isotopes are a useful tracer of both environmental setting and sub-ice shelf circulation strength in both modern and paleo-ice sheet margins. Crown Copyright © 2018 Published by Elsevier B.V. | en_AU |
dc.identifier.citation | White, D. A., Fink, D., Post, A. L., Simon, K., Galton-Fenzi, B., Foster, S., Fujioka, T., Jeromson, M. R., Blaxell, M., Yokoyama, Y. (2019). Beryllium isotope signatures of ice shelves and sub-ice shelf circulation. Earth and Planetary Science Letters, 505, 86-95, doi:10.1016/j.epsl.2018.10.004 | en_AU |
dc.identifier.issn | 0012-821X | en_AU |
dc.identifier.journaltitle | Earth and Planetary Science Letters | en_AU |
dc.identifier.pagination | 86-95 | en_AU |
dc.identifier.uri | https://doi.org/10.1016/j.epsl.2018.10.004 | en_AU |
dc.identifier.uri | https://apo.ansto.gov.au/dspace/handle/10238/12507 | en_AU |
dc.identifier.volume | 505 | en_AU |
dc.language.iso | en | en_AU |
dc.publisher | Elsevier | en_AU |
dc.subject | Ice | en_AU |
dc.subject | Beryllium 10 | en_AU |
dc.subject | Isotopes | en_AU |
dc.subject | Sediments | en_AU |
dc.subject | Antarctica | en_AU |
dc.subject | Advection | en_AU |
dc.title | Beryllium isotope signatures of ice shelves and sub-ice shelf circulation | en_AU |
dc.type | Journal Article | en_AU |