Abstract
The presence of nanometer-sized diamonds in purported Younger Dryas (YD) boundary-dated sediments, carbon spherules, and Greenland ice was cited as evidence of a YD impact event (1). Although cubic and hexagonal (lonsdaleite) diamond have been found in shocked metamorphosed meteorites and are associated with terrestrial impact structures, cubic diamonds are well known to occur in terrestrial deposits that have no associations with impact processes. For example, submicron and smaller cubic diamond crystals have been found recently in carbonaceous spherules isolated in upper soils from various German and Belgian sites (2). Lacking links to impact structures, these diamonds are evidently not products of impact …
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
