van Ginneken Matthias, Wozniakiewicz Penelope J, Brownlee Donald E, Debaille Vinciane, Della Corte Vincenzo, Delauche Lucie, Duprat Jean, Engrand Cecile, Folco Luigi, Fries Marc, Gattacceca Jérôme, Genge Matthew J, Goderis Steven, Gounelle Matthieu, Harvey Ralph P, Jonker Guido, Krämer Ruggiu Lisa, Larsen Jon, Lever James H, Noguchi Takaaki, Peterson Scott, Rochette Pierre, Rojas Julien, Rotundi Alessandra, Rudraswami N G, Suttle Martin D, Taylor Susan, Van Maldeghem Flore, Zolensky Michael
Centre for Astrophysics and Planetary Science, School of Physics and Astronomy, University of Kent , Canterbury CT2 7NH, UK.
Department of Astronomy, University of Washington , Seattle, WA 98195, USA.
Philos Trans A Math Phys Eng Sci. 2024 Jun 9;382(2273):20230195. doi: 10.1098/rsta.2023.0195. Epub 2024 May 13.
Micrometeorites are estimated to represent the main part of the present flux of extraterrestrial matter found on the Earth's surface and provide valuable samples to probe the interplanetary medium. Here, we describe large and representative collections of micrometeorites currently available to the scientific community. These include Antarctic collections from surface ice and snow, as well as glacial sediments from the eroded top of nunataks-summits outcropping from the icesheet-and moraines. Collections extracted from deep-sea sediments (DSS) produced a large number of micrometeorites, in particular, iron-rich cosmic spherules that are rarer in other collections. Collections from the old and stable surface of the Atacama Desert show that finding large numbers of micrometeorites is not restricted to polar regions or DSS. The advent of rooftop collections marks an important step into involving citizen science in the study of micrometeorites, as well as providing potential sampling locations over all latitudes to explore the modern flux. We explore their strengths of the collections to address specific scientific questions and their potential weaknesses. The future of micrometeorite research will involve the finding of large fossil micrometeorite collections and benefit from recent advances in sampling cosmic dust directly from the air. This article is part of the theme issue 'Dust in the Solar System and beyond'.
据估计,微陨石是目前在地球表面发现的外星物质通量的主要组成部分,并为探测行星际介质提供了有价值的样本。在此,我们描述了目前科学界可获得的大量且具有代表性的微陨石样本。这些样本包括来自地表冰雪的南极样本,以及来自冰原中露出的平顶山山顶侵蚀顶部的冰川沉积物和冰碛物。从深海沉积物(DSS)中提取的样本产生了大量微陨石,特别是富含铁的宇宙球粒,这些在其他样本中较为罕见。来自阿塔卡马沙漠古老且稳定表面的样本表明,发现大量微陨石并不局限于极地地区或深海沉积物。屋顶样本的出现标志着公民科学参与微陨石研究的重要一步,同时也为探索现代通量提供了所有纬度的潜在采样地点。我们探讨了这些样本在解决特定科学问题方面的优势及其潜在弱点。微陨石研究的未来将包括发现大型化石微陨石样本,并受益于最近直接从空气中采样宇宙尘埃的进展。本文是主题为“太阳系及其他区域的尘埃”的一部分。