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  • PublicationMetadata only
    An evaporite sequence from ancient brine recorded in Bennu samples
    (Springer Science and Business Media LLC, 2025-01-29) McCoy, TJ; Russell, SS; Zega, TJ; Thomas-Keprta, KL; Singerling, SA; Brenker, FE; Timms, NE; Rickard, WDA; Barnes, JJ; Libourel, G; Ray, S; Corrigan, CM; Haenecour, P; Gainsforth, Z; Dominguez, G; King, AJ; Keller, LP; Thompson, MS; Sandford, SA; Jones, RH; Yurimoto, H; Righter, K; Eckley, SA; Bland, PA; Marcus, MA; DellaGiustina, DN; Ireland, TR; Almeida, NV; Harrison, CS; Bates, HC; Schofield, PF; Seifert, LB; Sakamoto, N; Kawasaki, N; Jourdan, F; Reddy, SM; Saxey, DW; Ong, IJ; Prince, BS; Ishimaru, K; Smith, LR; Benner, MC; Kerrison, NA; Portail, M; Guigoz, V; Zanetta, P-M; Wardell, LR; Gooding, T; Rose, TR; Salge, T; Le, L; Tu, VM; Zeszut, Z; Mayers, C; Sun, X; Hill, DH; Lunning, NG; Hamilton, VE; Glavin, DP; Dworkin, JP; Kaplan, HH; Franchi, IA; Tait, KT; Tachibana, S; Connolly, HC; Lauretta, DS
    Abstract: Evaporation or freezing of water-rich fluids with dilute concentrations of dissolved salts can produce brines, as observed in closed basins on Earth1 and detected by remote sensing on icy bodies in the outer Solar System2,3. The mineralogical evolution of these brines is well understood in regard to terrestrial environments4, but poorly constrained for extraterrestrial systems owing to a lack of direct sampling. Here we report the occurrence of salt minerals in samples of the asteroid (101955) Bennu returned by the OSIRIS-REx mission5. These include sodium-bearing phosphates and sodium-rich carbonates, sulfates, chlorides and fluorides formed during evaporation of a late-stage brine that existed early in the history of Bennu’s parent body. Discovery of diverse salts would not be possible without mission sample return and careful curation and storage, because these decompose with prolonged exposure to Earth’s atmosphere. Similar brines probably still occur in the interior of icy bodies Ceres and Enceladus, as indicated by spectra or measurement of sodium carbonate on the surface or in plumes2,3.
  • PublicationMetadata only
    An overview of the petrography and petrology of particles from aggregate sample from asteroid Bennu
    (Wiley, 2025-05-09) Connolly, Harold C; Lauretta, Dante S; McCoy, Timothy J; Russell, Sara S; Haenecour, Pierre; Polit, Anjani; Barnes, Jessica J; Zega, Thomas J; Yurimoto, Hisayoshi; Kawasaki, Noriyuki; Righter, Kevin; Libourel, Guy; Portail, Marc; Guigoz, Vincent; King, Ashley J; Keller, Lindsay P; Thomas‐Keprta, Kathy; Le, Loan; Tu, Valarie; Eckley, Scott A; Corrigan, Catherine M; Gooding, Timothy; Rose, Timothy; Wardell, Rob; Ray, Soumya; Hamilton, Victoria E; Lunning, Nicole G; Snead, Christopher J; McCubbin, Francis M; Thompson, Michelle S; Jones, Rhian H; Domanik, Kenneth; Hill, Dolores; Smith, Lucas; Ong, Iunn J; Salge, T; Almeida, Natasha; Harrison, Catherine; Bates, Helena; Schofield, Paul; Franchi, Ian A; May, Brian H; Manzoni, Claudia; Ryan, Andrew J; Ballouz, Ronald‐Louis; Macke, Robert J; Dworkin, Jason P; Lorentson, Charles C; Tait, Kimberly; Jawin, Erica R; Kaplan, Hannah H; DellaGuistina, Daniella N; Walsh, Kevin J; Moreau, Michael C; Enos, Heather L; Wolner, CWV; Roper, Heather L; Tachibana, Shogo
    Abstract: The OSIRIS‐REx mission returned a sample of regolith from the carbonaceous asteroid Bennu in September 2023. We present preliminary in situ investigations of the petrology and petrography of selected particles ranging in size from 0.5 to 3 mm. Using a combination of optical and electron beam techniques, we investigate whole specimens and polished sections belonging to morphologically and visually distinct categories of particles. We find that morphological differences in the particles are reflective of petrographic and petrologic differences, leading to the conclusion that we have at least two distinct major lithologies in the bulk sample. Our findings support predictions from remote sensing, suggesting that the morphological differences observed in the boulder population of Bennu correspond to petrologic differences. Our data provide insight into the geologic activity on Bennu's parent body and the petrographic framework needed to contextualize the detailed analyses of this pristine asteroidal material.
  • PublicationMetadata only
    Origin of the Jadar Volcano-Sedimentary Li-B Deposit, Serbia
    (Society of Economic Geologists, Inc., 2025-03-12) Putzolu, F; Armstrong, RN; Boyce, AJ; Hepburn, LE; Bompard, N; Najorka, J; Lefebvre-Desanois, M; Milton, AJ; Salge, T; Erak, D; Abad, I; Herrington, RJ
    Abstract: The Jadar deposit (Serbia) is a unique end member of the volcano-sedimentary Li deposit class, where the main ore mineral is jadarite (LiNaSiB3O7(OH)), to date only recorded at the Jadar locality. We provide the first account of the features of the Jadar deposit based on the study of drill hole material, complemented by petrographic analysis, whole-rock, and isotopic geochemistry. The Li-B mineralization is hosted by sediments interlayered with tuffs that were deposited in a fault-bounded lacustrine basin. Mineralization processes initially involved alteration of volcanic glass through near-neutral and heated meteoric fluids, which resulted in the formation of hectorite. Lithium clays were later overprinted by higher-pH brines, which underwent significant evaporation, combined with conditions of Na+ and SiO2(aq) saturation, resulting in formation of siliceous gels that were the precursors to jadarite formation and extensive zeolitization of the intrabasinal sediments. Formation of jadarite occurred in two stages: (1) early diagenesis accompanied by zeolitization and precipitation of primary dolomite, which resulted in the sediment-hosted Li mineralization, (2) late remobilization of Li(B-Na)–saturated fluids, leading to formation of epigenetic jadarite-albite infills of fractured rocks. Isotopic geochemistry combined with mineral chemistry proxies indicate that early mineralizing processes were largely dominated by diagenetic fluids that experienced a thermal influence from the coeval cooling of the Miocene S-type granite member of the nearby Cer Mountain Complex. Late thermal maturation of organic matter then resulted in acidic fluids that dissolved the early ore assemblage and led to formation of late diagenetic lithiophosphate and low-Na borates.
  • PublicationMetadata only
    Coastal seawater turbidity and thermal stress control growth of reef-building Porites spp. corals in Fiji
    (Springer Science and Business Media LLC, 2025-05-17) Samperiz, Ana; Sosdian, Sindia; Hendy, Erica; Johnson, Kenneth; John, Eleanor H; Jupiter, Stacy D; Albert, Simon
    Nearshore reefs, at the interface of land-sea interactions, provide essential ecosystem services, but are susceptible to multiple global and local stressors. These stressors can detrimentally impact coral growth and the continuity of the reef framework. Here, we analyse coral growth records (1998 – 2016) of massive Porites spp. colonies from nearshore reefs in Fiji. Our aim is to assess the role of thermal stress and turbidity on coral growth across a range of environments. Our findings reveal a negative linear relationship between linear extension and seawater turbidity across locations (GLM, R2 = 0.42, p < 0.001), indicating that average coral growth is significantly influenced by local environmental conditions. On interannual timescales, all locations experienced a 14% to 30% decrease in linear extension in response to acute thermal stress during the 2013 – 2016 period. This finding highlights the existence of compounding effects between water quality and thermal stress. We suggest that inshore, long-lived massive hard corals in areas of high turbidity are more vulnerable to increasing SSTs due to an already reduced mean growth. Integrated management strategies in these regions that considers managing for multiple, interacting local stressors are warranted to enhance resilience.
  • PublicationOpen Access
    The northernmost known observation of Myrmecophilus acervorum and the first records of Myrmecophilidae (Orthoptera, Ensifera) from Latvia
    (Pensoft, 2025-04-25) Balodis, Aleksandrs; Starka, Rūta; Telnov, Dmitry
    The first observations of myrmecophilous ant cricket Myrmecophilus acervorum (Panzer, 1799) and the family Myrmecophilidae from Latvia are presented. The observations were made in two locations subject to flooding in springtime. Adult and juvenile female individuals were observed. The discussed records appear to be the northernmost known distribution limit of this species.