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==Occurrence== [[File:Popigai nanodiamonds.jpg|thumb|Diamond samples from the [[Popigai impact structure]]: (a) is pure diamond, while (b) is diamond with some lonsdaleite impurities.]] Lonsdaleite occurs as microscopic crystals associated with diamond in several meteorites: [[Canyon Diablo meteorite|Canyon Diablo]],<ref name="Lea 2022">{{cite web |last=Lea |first=Robert |title=Dwarf planet collision may have sent strange ultra-hard diamonds to Earth |website=Space.com |date=2022-09-12 |url=https://www.space.com/meteorite-strange-form-of-diamond |access-date=2022-09-13}}</ref> [[Kenna meteorite|Kenna]], and [[Allan Hills 77283]]. It is also naturally occurring in non-bolide diamond [[placer deposit]]s in the [[Sakha Republic]].<ref> {{cite journal |author=Kaminskii, F.V. |author2=G.K. Blinova |author3=E.M. Galimov |author4=G.A. Gurkina |author5=Y.A. Klyuev |author6=L.A. Kodina |author7=V.I. Koptil |author8=V.F. Krivonos |author9=L.N. Frolova |author10=A.Y. Khrenov |date=1985 |title=Polycrystalline aggregates of diamond with lonsdaleite from Yakutian [Sakhan] placers |journal=Mineral. Zhurnal |volume=7 |pages=27β36 }} </ref> Material with d-spacings consistent with Lonsdaleite has been found in sediments with highly uncertain dates at [[Lake Cuitzeo]], in the state of [[Guanajuato]], Mexico, by proponents of the controversial [[Younger Dryas impact hypothesis]],<ref> {{cite journal |last1=Israde-Alcantara |first1=I. |last2=Bischoff |first2=J.L. |last3=Dominguez-Vazquez |first3=G. |last4=Li |first4=H.-C. |last5=Decarli |first5=P.S. |last6=Bunch |first6=T.E. |last7=Wittke |first7=J.H. |last8=Weaver |first8=J.C. |last9=Firestone |first9=R.B. |last10=West |first10=A. |last11=Kennett |first11=J.P. |last12=Mercer |first12=C. |last13=Xie |first13=S. |last14=Richman |first14=E.K. |last15=Kinzie |first15=C.R. |last16=Wolbach |first16=W.S. |display-authors=6 |year=2012 |title=Evidence from central Mexico supporting the Younger Dryas extraterrestrial impact hypothesis |journal=Proceedings of the National Academy of Sciences |volume=109 |issue=13 |pages=E:738β747 |pmid=22392980 |doi=10.1073/pnas.1110614109 |bibcode=2012PNAS..109E.738I |pmc=3324006 |doi-access=free }} </ref> which is now refuted by earth scientists and planetary impact specialists.<ref>{{Cite journal |last=Holliday |first=Vance T. |last2=Daulton |first2=Tyrone L. |last3=Bartlein |first3=Patrick J. |last4=Boslough |first4=Mark B. |last5=Breslawski |first5=Ryan P. |last6=Fisher |first6=Abigail E. |last7=Jorgeson |first7=Ian A. |last8=Scott |first8=Andrew C. |last9=Koeberl |first9=Christian |last10=Marlon |first10=Jennifer |last11=Severinghaus |first11=Jeffrey |last12=Petaev |first12=Michail I. |last13=Claeys |first13=Philippe |date=2023-07-26 |title=Comprehensive refutation of the Younger Dryas Impact Hypothesis (YDIH) |url=https://linkinghub.elsevier.com/retrieve/pii/S0012825223001915 |journal=Earth-Science Reviews |language=en |pages=104502 |doi=10.1016/j.earscirev.2023.104502|doi-access=free }}</ref> Claims of Lonsdaleite and other nanodiamonds in a layer of the Greenland ice sheet that could be of Younger Dryas age have not been confirmed and are now disputed.<ref name="Kurbatov Mayewski Steffensen West 2022">{{cite web |last1=Kurbatov |first1=Andrei V. |last2=Mayewski |first2=Paul A. |last3=Steffensen |first3=Jorgen P. |last4=West |first4=Allen |last5=Kennett |first5=Douglas J. |last6=Kennett |first6=James P. |last7=Bunch |first7=Ted E. |last8=Handley |first8=Mike |last9=Introne |first9=Douglas S. |last10=Hee |first10=Shane S. Que |last11=Mercer |first11=Christopher |last12=Sellers |first12=Marilee |last13=Shen |first13=Feng |last14=Sneed |first14=Sharon B. |last15=Weaver |first15=James C. |last16=Wittke |first16=James H. |last17=Stafford |first17=Thomas W. |last18=Donovan |first18=John J. |last19=Xie |first19=Sujing |last20=Razink |first20=Joshua J. |last21=Stich |first21=Adrienne |last22=Kinzie |first22=Charles R. |last23=Wolbach |first23=Wendy S. |title=Discovery of a nanodiamond-rich layer in the Greenland ice sheet |website=PubPeer |date=2022-09-20 |url=https://pubpeer.com/publications/28B83ADB820618B3F374667D5FBB92 |access-date=2022-09-28}}</ref> Its presence in local peat deposits is claimed as evidence for the [[Tunguska event]] being caused by a meteor rather than by a cometary fragment.<ref> {{cite journal |last1=Kvasnytsya |first1=Victor |last2=Wirth |last3=Dobrzhinetskaya |last4=Matzel |last5=Jacobsend |last6=Hutcheon |last7=Tappero |last8=Kovalyukh |date=August 2013 |title=New evidence of meteoritic origin of the Tunguska cosmic body |journal=Planetary and Space Science |volume=84 |pages=131β140 |doi=10.1016/j.pss.2013.05.003 |bibcode=2013P&SS...84..131K |url=http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:247242 }} </ref><ref> {{cite news |last=Redfern |first=Simon |title=Russian meteor shockwave circled globe twice |work=BBC News |date=28 June 2013 |publisher=[[British Broadcasting Corporation]] |url=https://www.bbc.co.uk/news/science-environment-23066055 |access-date=28 June 2013 }} </ref>
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