[meteorite-list] The Antarctic Meteorites: Classification and Curation at the Smithsonian Institution
From: Shawn Alan <photophlow_at_meteoritecentral.com>
Date: Mon, 15 Mar 2010 03:56:30 -0700 (PDT) Message-ID: <285385.80761.qm_at_web113605.mail.gq1.yahoo.com> Morning Listers, Here is an article from the 41 Lunar and Planetary Science Conference about the Smithsonian and the challenges they face on the large numbers of meteorites they have to classify?from Antarctic.? ? ?The Antarctic Meteorites: Classification and Curation at the Smithsonian Institution. C. M. Corrigan1, L. C. Welzenbach1, T. J. McCoy1, 1 Department of Mineral Sciences, National Museum of Natural History, Smithsonian Institution, Washington, DC 20560-0119, USA; corriganc at si.edu. ? A Relentless Onslaught: Over the past decade, we have classified between 450-1000 Antarctic mete- orites per year (Figure 1). This pace, and the variabili- ty in staffing levels in the Antarctic Meteorite Program over the past ten years, has caused us to make a few changes at the Smithsonian. We have now entered a period of relative stability following the hire of the author (Corrigan) who has been tasked with managing the day-to-day activities of the Antarctic meteorite collection. In addition, we have implemented some improvements aimed at both saving time and creating a more robust classification process. The first of these includes a ?first-pass? classification during initial han- dling at the Smithsonian, during which we give a pre- liminary grouping to each meteorite (ordinary chon- drite, carbonaceous chondrite, achondrite) which al- lows us to separate out those unique types that will need to be sectioned right away. This initial classifica- tion is then confirmed or refuted using a variety of techniques. These include further visual examination with binocular microscopes for all meteorites, oil im- mersion of a few olivine grains for equilibrated ordi- nary chondrites, and thin section examination and mi- croprobe analyses for other types of meteorites (carbo- naceous chondrites, enstatite chondrites, achondrites, iron meteorites and ?unknowns?, which are occasio- nally found to be terrestrial samples from Antarctic glacial moraines). Our goal is to have all of the An- tarctic meteorites classified within two years of their return from the ice, a standard now codified in a U.S. Federal Regulation on Antarctic meteorites. In this context, newly collected meteorites have always ar- rived before all the previous year?s meteorites have been classified. Reducing Complexity while Maintaining Objec- tivity: A significant challenge to timely classification is simplifying the process by comparing meteorites from a single field area. Pairing groups are common and classification can be accomplished more quickly if focus is maintained on a single field area. This has been increasingly challenging during the past few years, with multiple field parties working in several ice fields returning meteorites from many geographically and glaciologically distinct areas in a single year. While the meteoritics research community tends to subdivide groupings and attach significance to abun- dances of different groups, the classifications we com- plete must have a level of robustness that is consistent and can be maintained. As examples, we avoid sub- classifying eucrites and while we attach both chemical groups and petrologic types to ordinary chondrites classified with only visual examination and oil immer- sion, we advise due caution in overinterpreting abun- dances within these groups. While the overall percen- tage of ordinary chondrites is probably a robust statis- tic, comparing abundances of L5 vs. LL4 is fraught with peril. Curation of the Antarctic Meteorites: The meteorites that are returned from Antarctica are, in the long term, stored and curated by the staff at the Smith- sonian. On hand (and onsite at the National Museum of Natural History, NMNH), we house a chip of each meteorite returned from the ice and the reference thin section (those used in the initial classification) of each meteorite of significant scientific interest to the mete- orite community. All Antarctic meteorites are even- tually sent from the Johnson Space Center (JSC) to the Smithsonian for indefinite curation. Exceptions to this rule are those meteorites of intense scientific interest to the community (i.e., those that receive a large number of requests for sampling for research projects from the community). These meteorites, which include those on the Meteorite Working Group?s ?special list? (a list of rare/small designed to prevent the over-allocation of any individual meteorite), are housed and allocated from the specialized facilities at JSC. Meteorites are transferred to the Smithsonian Institution permanently after three years without requests by the scientific community and become the responsibility of the SI for future allocation. At the Smithsonian, meteorites are housed in a special facility designed for the long-term curation of meteorites (Figure 2). That facility, which is fashioned after the Meteorite Processing Lab at Johnson Space Center, includes stainless steel nitrogen atmosphere cabinets for the storage of meteorites along with a larger, updated facility currently under con- struction. At the current rates of collection, this facili- ty should be sufficient to house incoming samples for approximately 20 years. This new facility will also house the meteorites in a ?Class 10,000? clean room. The Science of Antarctic Meteorites: Overall, our job is to provide a preliminary classification of each meteorite that ANSMET recovers and returns, not to answer the individual compelling scientific ques- tions surrounding each meteorite, no matter how tanta- lizing the meteorite may be. Our overarching goal is to provide the Antarctic meteorite material to the scientific community in a timely fashion, with suffi- cient information that individual researchers can re- quest the samples that will most benefit their research. Sample Requests and Education: Sample Re- quests: Twice a year the newly classified Antarctic meteorites are announced in the Antarctic Meteorite Newsletter [2]. Request deadlines are included in the Newsletter (and are generally about a month after its publication) as is the link to the sample request form. The Meteorite Working Group (MWG) meets bian- nually as well, usually in Houston the weekend after the LPSC and sometime in September at the NSF Headquarters in Arlington, VA. All requests for An- tarctic meteorites that are not considered ?curatorial? are processed at these meetings and allocations are completed following the meetings. ?Curatorial? re- quests (includes iron meteorites and those samples that have been permanently transferred into the SI collec- tion) are currently being dealt with individually by the SI and/or JSC, and many of those are dealt with on a rolling basis. Additionally, MWG is reviewing some requests via email between meetings. Education: In addition to samples being allocated for research purposes, we also provide samples for education and public outreach. Many PIs request and receive samples from the SI collection that are availa- ble for use in exhibits. Suites of samples have been put together for classes on meteorite petrology by JSC and should be requested through the education sample curator there (currently Mary Luckey). These can be of immense importance to graduate students who may otherwise come out of graduate school having seen only the types of meteorites they work on, or only spectra of other bodies that may (or may not!) relate to the actual rocks we have in our collections. Ground truthing these samples, and putting them into perspec- tive with other material from throughout the Solar Sys- tem is a hugely beneficial exercise. Finally, individual researchers are welcome to come view thin sections within the SI collection at any time. We have the facilities for viewing and photo- graphing the library sections for the Antarctic Mete- orites. Many individuals have found it invaluable to sit and spend a few days looking at all of the sections of one particular type of meteorites, for example. References: [1] Corrigan C.M. et al. (2008) Work- shop on Antarctic Meteorites: Search Recovery and Classification, MAPS 43 Suppl., A180. [2] http://www- curator.jsc.nasa.gov/antmet/amn/amn.cfm ? http://www.lpi.usra.edu/meetings/lpsc2010/pdf/2332.pdf ? Shawn Alan Received on Mon 15 Mar 2010 06:56:30 AM PDT |
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