Academic Journal
Brine residues and organics in the Urvara basin on Ceres.
| Τίτλος: | Brine residues and organics in the Urvara basin on Ceres. |
|---|---|
| Συγγραφείς: | Nathues A; Max Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, 37077, Goettingen, Germany. nathues@mps.mpg.de., Hoffmann M; Max Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, 37077, Goettingen, Germany., Schmedemann N; Institut für Planetologie, WWU Münster, Münster, Germany., Sarkar R; Max Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, 37077, Goettingen, Germany., Thangjam G; School of Earth and Planetary Sciences, National Institute of Science Education and Research, NISER, HBNI, Bhubaneswar, India., Mengel K; Max Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, 37077, Goettingen, Germany., Hernandez J; Max Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, 37077, Goettingen, Germany., Hiesinger H; Institut für Planetologie, WWU Münster, Münster, Germany., Pasckert JH; Institut für Planetologie, WWU Münster, Münster, Germany. |
| Πηγή: | Nature communications [Nat Commun] 2022 Feb 22; Vol. 13 (1), pp. 927. Date of Electronic Publication: 2022 Feb 22. |
| Τύπος έκδοσης: | Journal Article; Research Support, Non-U.S. Gov't |
| Γλώσσα: | English |
| Στοιχεία περιοδικού: | Publisher: Nature Pub. Group Country of Publication: England NLM ID: 101528555 Publication Model: Electronic Cited Medium: Internet ISSN: 2041-1723 (Electronic) Linking ISSN: 20411723 NLM ISO Abbreviation: Nat Commun Subsets: MEDLINE |
| Imprint Name(s): | Original Publication: [London] : Nature Pub. Group |
| Ιατρικοί όροι (MeSH): | Evolution, Planetary* , Salts*, Earth, Planet ; Geology |
| Περίληψη: | Ceres is a partially differentiated dwarf planet, as confirmed by NASA's Dawn mission. The Urvara basin (diameter ~170 km) is its third-largest impact feature, enabling insights into the cerean crust. Urvara's geology and mineralogy suggest a potential brine layer at the crust-mantle transition. Here we report new findings that help in understanding the structure and composition of the cerean crust. These results were derived by using the highest-resolution Framing Camera images acquired by Dawn at Ceres. Unexpectedly, we found meter-scale concentrated exposures of bright material (salts) along the crater's upper central ridge, which originate from an enormous depth, possibly from a deep-seated brine or salt reservoir. An extended resurfacing modified the southern floor ~100 Myr after crater formation (~250 Myr), long after the dissipation of the impact-generated heat. In this resurfaced area, one floor scarp shows a granular flow pattern of bright material, showing spectra consistent with the presence of organic material, the first such finding on Ceres beyond the vast Ernutet area. Our results strengthen the hypothesis that Ceres is and has been a geologically active world even in recent epochs, with salts and organic-rich material playing a major role in its evolution. (© 2022. The Author(s).) |
| References: | Science. 2012 May 11;336(6082):700-4. (PMID: 22582258) Nature. 2015 Dec 10;528(7581):241-4. (PMID: 26659184) Nature. 2015 Dec 10;528(7581):237-40. (PMID: 26659183) Science. 2016 Sep 2;353(6303):1008-1010. (PMID: 27701107) Science. 2017 Feb 17;355(6326):719-722. (PMID: 28209893) Science. 2016 Sep 2;353(6303):. (PMID: 27701089) Nature. 2016 Aug 4;536(7614):54-7. (PMID: 27362221) Geophys Res Lett. 2017 Jul 16;44(13):6570-6578. (PMID: 28989206) |
| Substance Nomenclature: | 0 (Salts) 0 (brine) |
| Entry Date(s): | Date Created: 20220223 Date Completed: 20220412 Latest Revision: 20220412 |
| Update Code: | 20260130 |
| PubMed Central ID: | PMC8863799 |
| DOI: | 10.1038/s41467-022-28570-8 |
| PMID: | 35194036 |
| Βάση Δεδομένων: | MEDLINE |
| FullText | Links: – Type: other Url: https://resolver.ebsco.com:443/public/rma-ftfapi/ejs/direct?AccessToken=4DD2B6B14DEA3D135C9C&Show=Object Text: Availability: 0 CustomLinks: – Url: https://dx.doi.org/doi:10.1038/s41467-022-28570-8 Name: EDS - Springer Nature Journals (s7799221) Category: fullText Text: View record at Springer |
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| Header | DbId: cmedm DbLabel: MEDLINE An: 35194036 AccessLevel: 3 PubType: Academic Journal PubTypeId: academicJournal PreciseRelevancyScore: 0 |
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| Items | – Name: Title Label: Title Group: Ti Data: Brine residues and organics in the Urvara basin on Ceres. – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AU" term="%22Nathues+A%22">Nathues A</searchLink>; Max Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, 37077, Goettingen, Germany. nathues@mps.mpg.de.<br /><searchLink fieldCode="AU" term="%22Hoffmann+M%22">Hoffmann M</searchLink>; Max Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, 37077, Goettingen, Germany.<br /><searchLink fieldCode="AU" term="%22Schmedemann+N%22">Schmedemann N</searchLink>; Institut für Planetologie, WWU Münster, Münster, Germany.<br /><searchLink fieldCode="AU" term="%22Sarkar+R%22">Sarkar R</searchLink>; Max Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, 37077, Goettingen, Germany.<br /><searchLink fieldCode="AU" term="%22Thangjam+G%22">Thangjam G</searchLink>; School of Earth and Planetary Sciences, National Institute of Science Education and Research, NISER, HBNI, Bhubaneswar, India.<br /><searchLink fieldCode="AU" term="%22Mengel+K%22">Mengel K</searchLink>; Max Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, 37077, Goettingen, Germany.<br /><searchLink fieldCode="AU" term="%22Hernandez+J%22">Hernandez J</searchLink>; Max Planck Institute for Solar System Research, Justus-von-Liebig-Weg 3, 37077, Goettingen, Germany.<br /><searchLink fieldCode="AU" term="%22Hiesinger+H%22">Hiesinger H</searchLink>; Institut für Planetologie, WWU Münster, Münster, Germany.<br /><searchLink fieldCode="AU" term="%22Pasckert+JH%22">Pasckert JH</searchLink>; Institut für Planetologie, WWU Münster, Münster, Germany. – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22101528555%22">Nature communications</searchLink> [Nat Commun] 2022 Feb 22; Vol. 13 (1), pp. 927. <i>Date of Electronic Publication: </i>2022 Feb 22. – Name: TypePub Label: Publication Type Group: TypPub Data: Journal Article; Research Support, Non-U.S. Gov't – Name: Language Label: Language Group: Lang Data: English – Name: TitleSource Label: Journal Info Group: Src Data: <i>Publisher: </i><searchLink fieldCode="PB" term="%22Nature+Pub%2E+Group%22">Nature Pub. Group </searchLink><i>Country of Publication: </i>England <i>NLM ID: </i>101528555 <i>Publication Model: </i>Electronic <i>Cited Medium: </i>Internet <i>ISSN: </i>2041-1723 (Electronic) <i>Linking ISSN: </i><searchLink fieldCode="IS" term="%2220411723%22">20411723 </searchLink><i>NLM ISO Abbreviation: </i>Nat Commun <i>Subsets: </i>MEDLINE – Name: PublisherInfo Label: Imprint Name(s) Group: PubInfo Data: <i>Original Publication</i>: [London] : Nature Pub. Group – Name: SubjectMESH Label: MeSH Terms Group: Su Data: <searchLink fieldCode="MM" term="%22Evolution%2C+Planetary%22">Evolution, Planetary*</searchLink> <br /><searchLink fieldCode="MM" term="%22Salts%22">Salts*</searchLink><br /><searchLink fieldCode="MH" term="%22Earth%2C+Planet%22">Earth, Planet</searchLink> ; <searchLink fieldCode="MH" term="%22Geology%22">Geology</searchLink> – Name: Abstract Label: Abstract Group: Ab Data: Ceres is a partially differentiated dwarf planet, as confirmed by NASA's Dawn mission. The Urvara basin (diameter ~170 km) is its third-largest impact feature, enabling insights into the cerean crust. Urvara's geology and mineralogy suggest a potential brine layer at the crust-mantle transition. Here we report new findings that help in understanding the structure and composition of the cerean crust. These results were derived by using the highest-resolution Framing Camera images acquired by Dawn at Ceres. Unexpectedly, we found meter-scale concentrated exposures of bright material (salts) along the crater's upper central ridge, which originate from an enormous depth, possibly from a deep-seated brine or salt reservoir. An extended resurfacing modified the southern floor ~100 Myr after crater formation (~250 Myr), long after the dissipation of the impact-generated heat. In this resurfaced area, one floor scarp shows a granular flow pattern of bright material, showing spectra consistent with the presence of organic material, the first such finding on Ceres beyond the vast Ernutet area. Our results strengthen the hypothesis that Ceres is and has been a geologically active world even in recent epochs, with salts and organic-rich material playing a major role in its evolution.<br /> (© 2022. The Author(s).) – Name: Ref Label: References Group: RefInfo Data: Science. 2012 May 11;336(6082):700-4. (PMID: <searchLink fieldCode="PM" term="%2222582258%22">22582258)</searchLink><br />Nature. 2015 Dec 10;528(7581):241-4. (PMID: <searchLink fieldCode="PM" term="%2226659184%22">26659184)</searchLink><br />Nature. 2015 Dec 10;528(7581):237-40. (PMID: <searchLink fieldCode="PM" term="%2226659183%22">26659183)</searchLink><br />Science. 2016 Sep 2;353(6303):1008-1010. (PMID: <searchLink fieldCode="PM" term="%2227701107%22">27701107)</searchLink><br />Science. 2017 Feb 17;355(6326):719-722. (PMID: <searchLink fieldCode="PM" term="%2228209893%22">28209893)</searchLink><br />Science. 2016 Sep 2;353(6303):. (PMID: <searchLink fieldCode="PM" term="%2227701089%22">27701089)</searchLink><br />Nature. 2016 Aug 4;536(7614):54-7. (PMID: <searchLink fieldCode="PM" term="%2227362221%22">27362221)</searchLink><br />Geophys Res Lett. 2017 Jul 16;44(13):6570-6578. (PMID: <searchLink fieldCode="PM" term="%2228989206%22">28989206)</searchLink> – Name: NumberCAS Label: Substance Nomenclature Group: ID Data: 0 (Salts)<br />0 (brine) – Name: DateEntry Label: Entry Date(s) Group: Date Data: <i>Date Created: </i>20220223 <i>Date Completed: </i>20220412 <i>Latest Revision: </i>20220412 – Name: DateUpdate Label: Update Code Group: Date Data: 20260130 – Name: PubmedCentralID Label: PubMed Central ID Group: ID Data: PMC8863799 – Name: DOI Label: DOI Group: ID Data: 10.1038/s41467-022-28570-8 – Name: AN Label: PMID Group: ID Data: 35194036 |
| PLink | https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&db=cmedm&AN=35194036 |
| RecordInfo | BibRecord: BibEntity: Identifiers: – Type: doi Value: 10.1038/s41467-022-28570-8 Languages: – Code: eng Text: English PhysicalDescription: Pagination: StartPage: 927 Subjects: – SubjectFull: Earth, Planet Type: general – SubjectFull: Geology Type: general – SubjectFull: Evolution, Planetary Type: general – SubjectFull: Salts Type: general Titles: – TitleFull: Brine residues and organics in the Urvara basin on Ceres. Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: Nathues A – PersonEntity: Name: NameFull: Hoffmann M – PersonEntity: Name: NameFull: Schmedemann N – PersonEntity: Name: NameFull: Sarkar R – PersonEntity: Name: NameFull: Thangjam G – PersonEntity: Name: NameFull: Mengel K – PersonEntity: Name: NameFull: Hernandez J – PersonEntity: Name: NameFull: Hiesinger H – PersonEntity: Name: NameFull: Pasckert JH IsPartOfRelationships: – BibEntity: Dates: – D: 22 M: 02 Text: 2022 Feb 22 Type: published Y: 2022 Identifiers: – Type: issn-electronic Value: 2041-1723 Numbering: – Type: volume Value: 13 – Type: issue Value: 1 Titles: – TitleFull: Nature communications Type: main |
| ResultId | 1 |