{"dp_type": "Dataset", "free_text": "Fluorescence"}
[{"awards": "2040571 Smith, Walker", "bounds_geometry": ["POLYGON((168 -76.2,168.2 -76.2,168.4 -76.2,168.6 -76.2,168.8 -76.2,169 -76.2,169.2 -76.2,169.4 -76.2,169.6 -76.2,169.8 -76.2,170 -76.2,170 -76.28,170 -76.36,170 -76.44,170 -76.52,170 -76.6,170 -76.68,170 -76.76,170 -76.84,170 -76.92,170 -77,169.8 -77,169.6 -77,169.4 -77,169.2 -77,169 -77,168.8 -77,168.6 -77,168.4 -77,168.2 -77,168 -77,168 -76.92,168 -76.84,168 -76.76,168 -76.68,168 -76.6,168 -76.52,168 -76.44,168 -76.36,168 -76.28,168 -76.2))"], "date_created": "Wed, 07 Jan 2026 00:00:00 GMT", "description": "The data were collected by two gliders deployed in the southern Ross Sea from November, 2022 to January, 2023. They include water column data on temperature, salinity, optical backscatter at two wave lengths, fluorescence, and photosynthetically active radiation.", "east": 170.0, "geometry": ["POINT(169 -76.6)"], "keywords": "Adelie Penguin; Antarctica; Chlorophyll; Cryosphere; Oceans; Ross Sea; Salinity; Temperature", "locations": "Antarctica; Ross Sea", "north": -76.2, "nsf_funding_programs": "Antarctic Integrated System Science", "persons": "Smith, Walker", "project_titles": "NSFGEO-NERC: Collaborative Research \"P2P: Predators to Plankton -Biophysical Controls in Antarctic Polynyas\"", "projects": [{"proj_uid": "p0010273", "repository": "USAP-DC", "title": "NSFGEO-NERC: Collaborative Research \"P2P: Predators to Plankton -Biophysical Controls in Antarctic Polynyas\""}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -77.0, "title": "Water column data collected by sea gliders in the Ross Sea in 2022 and 2023", "uid": "602017", "west": 168.0}, {"awards": "1846837 Bowman, Jeff", "bounds_geometry": ["POINT(-64.053 -64.77)"], "date_created": "Tue, 13 May 2025 00:00:00 GMT", "description": "Raw flow cytometry data from Palmer Station for the 2023-2023 field season. Includes CSV files and raw FCS files for SYBR Green, autofluorescence, RedoxSensor Green. Data are included for environmental samples collected at Palmer LTER Station E and for bacterial mortality (dilution) experiments.", "east": -64.053, "geometry": ["POINT(-64.053 -64.77)"], "keywords": "Antarctica; Cryosphere; Palmer Station", "locations": "Palmer Station; Antarctica", "north": -64.77, "nsf_funding_programs": "Antarctic Organisms and Ecosystems", "persons": "Bowman, Jeff; Connors, Elizabeth", "project_titles": "CAREER: Understanding microbial heterotrophic processes in coastal Antarctic waters", "projects": [{"proj_uid": "p0010201", "repository": "USAP-DC", "title": "CAREER: Understanding microbial heterotrophic processes in coastal Antarctic waters"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -64.77, "title": "Raw flow cytometry data from Palmer Peninsula", "uid": "601930", "west": -64.053}, {"awards": "1744871 Robinson, Rebecca", "bounds_geometry": null, "date_created": "Wed, 30 Aug 2023 00:00:00 GMT", "description": "This dataset is the results of 3 experiments in which the spore-forming diatom Chaetoceros socialis was grown in culture and induced into resting spores by nitrate limitation. The nitrogen isotopic composition of accumulated biomass (\u03b415Nbiomass; \u2030 vs air) and of diatom-bound organic N (\u03b415Ndb; \u2030 vs air) are reported at two timepoints from each experiment: prior to and after resting spore formation. Experiments 1 and 2 provide measurements for CRS mixed with vegetative Chaetoceros cells, while Experiment 3 provides measurements for isolated CRS. Fluorescence and nitrate concentration was tracked throughout each experiment, with dissolved silica, ammonium, and total reduced nitrogen also measured in Experiment 3.", "east": null, "geometry": null, "keywords": "Antarctica", "locations": "Antarctica; Antarctica", "north": null, "nsf_funding_programs": "Antarctic Earth Sciences", "persons": "Dove, Isabel", "project_titles": "The nitrogen isotopic composition of diatom resting spores in Southern Ocean sediments: A source of bias and/or paleoenvironmental information?", "projects": [{"proj_uid": "p0010234", "repository": "USAP-DC", "title": "The nitrogen isotopic composition of diatom resting spores in Southern Ocean sediments: A source of bias and/or paleoenvironmental information?"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": null, "title": "Dissolved nutrients, cell counts, and nitrogen isotope measurements from Chaetoceros socialis culture experiments", "uid": "601727", "west": null}, {"awards": "1644155 Twining, Benjamin", "bounds_geometry": ["POLYGON((-78.1833 -68.4333,-78.16499 -68.4333,-78.14668 -68.4333,-78.12837 -68.4333,-78.11006 -68.4333,-78.09175 -68.4333,-78.07344 -68.4333,-78.05513 -68.4333,-78.03682 -68.4333,-78.01851 -68.4333,-78.0002 -68.4333,-78.0002 -68.43664,-78.0002 -68.43998,-78.0002 -68.44332,-78.0002 -68.44666000000001,-78.0002 -68.45,-78.0002 -68.45334,-78.0002 -68.45668,-78.0002 -68.46002,-78.0002 -68.46336000000001,-78.0002 -68.4667,-78.01851 -68.4667,-78.03682 -68.4667,-78.05513 -68.4667,-78.07344 -68.4667,-78.09175 -68.4667,-78.11006 -68.4667,-78.12837 -68.4667,-78.14668 -68.4667,-78.16499 -68.4667,-78.1833 -68.4667,-78.1833 -68.46336000000001,-78.1833 -68.46002,-78.1833 -68.45668,-78.1833 -68.45334,-78.1833 -68.45,-78.1833 -68.44666000000001,-78.1833 -68.44332,-78.1833 -68.43998,-78.1833 -68.43664,-78.1833 -68.4333))"], "date_created": "Mon, 12 Dec 2022 00:00:00 GMT", "description": "Varying depth samples from Ace, Deep, \u0026 Organic Lake were obtained between 2013-2014. These samples were size fractionated by filtration for metagenomic analyses. Viral and bacterial abundances were determine on the filtrate fractions by flow cytometric analysis. Glutaraldehyde-fixed samples were stained with SYBR Green I fluorescence dye and virus-like particle (VLP) and bacteria-like cell (BLC) populations were discriminated based on green fluorescence and side scatter flow cytometry signals. Several distinct VLP and BLC populations where enumerated from Ace Lake and Organic Lake samples that revealed temporal and depth differences. Discrete VLP and BLC populations could not be discerned from Deep Lake samples. These files include the original flow cytometry particle counts (raw data), the gating templates used to count VLP and BLC populations (analysis_templates), and the resulting particle counts (analyzed).", "east": -78.0002, "geometry": ["POINT(-78.09175 -68.45)"], "keywords": "Ace Lake; Antarctica; Deep Lake; Organic Lake; Vestfold Hills", "locations": "Antarctica; Antarctica; Ace Lake; Vestfold Hills; Organic Lake; Deep Lake", "north": -68.4333, "nsf_funding_programs": "Antarctic Organisms and Ecosystems", "persons": "Twining, Benjamin; Martinez-Martinez, Joaquin", "project_titles": "Viral control of microbial communities in Antarctic lakes", "projects": [{"proj_uid": "p0010237", "repository": "USAP-DC", "title": "Viral control of microbial communities in Antarctic lakes"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -68.4667, "title": "Flow cytometry enumeration of virus-like and bacteria-like abundance in Ace, Deep, \u0026 Organic lakes (Antarctica)", "uid": "601626", "west": -78.1833}, {"awards": "1738942 Wellner, Julia", "bounds_geometry": ["POLYGON((-107.38 -74.64,-107.065 -74.64,-106.75 -74.64,-106.435 -74.64,-106.12 -74.64,-105.805 -74.64,-105.49 -74.64,-105.175 -74.64,-104.86 -74.64,-104.545 -74.64,-104.23 -74.64,-104.23 -74.683,-104.23 -74.726,-104.23 -74.769,-104.23 -74.812,-104.23 -74.855,-104.23 -74.898,-104.23 -74.941,-104.23 -74.984,-104.23 -75.027,-104.23 -75.07,-104.545 -75.07,-104.86 -75.07,-105.175 -75.07,-105.49 -75.07,-105.805 -75.07,-106.12 -75.07,-106.435 -75.07,-106.75 -75.07,-107.065 -75.07,-107.38 -75.07,-107.38 -75.027,-107.38 -74.984,-107.38 -74.941,-107.38 -74.898,-107.38 -74.855,-107.38 -74.812,-107.38 -74.769,-107.38 -74.726,-107.38 -74.683,-107.38 -74.64))"], "date_created": "Thu, 27 Jan 2022 00:00:00 GMT", "description": "This dataset contains measurements from grain-size, x-ray fluorescence (XRF), and physical properties (including magnetic susceptibility, water content, and shear strength) analyses of five sediment cores collected offshore Thwaites Glacier during cruises NBP19-02 (cores KC04, KC08, and KC23) and NBP20-02 (cores KC33 and KC67). We estimate the cores, which are between 213.5 and 297.5 cm in length, reflect deposition during the last ~10 kyr, consistent with published constraints of deglaciation of this region. Data are organized in Microsoft Excel spreadsheets and core locations are provided in a PDF.", "east": -104.23, "geometry": ["POINT(-105.805 -74.855)"], "keywords": "Antarctica; Chemistry:sediment; Chemistry:Sediment; Glaciomarine Sediment; Grain Size; Magnetic Susceptibility; Marine Geoscience; Marine Sediments; NBP1902; NBP2002; Physical Properties; R/v Nathaniel B. Palmer; Sediment Core Data; Thwaites Glacier; Trace Elements; XRF", "locations": "Thwaites Glacier; Antarctica", "north": -74.64, "nsf_funding_programs": "Antarctic Earth Sciences", "persons": "Lepp, Allison", "project_titles": "NSF-NERC: THwaites Offshore Research (THOR)", "projects": [{"proj_uid": "p0010062", "repository": "USAP-DC", "title": "NSF-NERC: THwaites Offshore Research (THOR)"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": "Thwaites (ITGC)", "south": -75.07, "title": "Physical and geochemical data from five sediment cores collected offshore Thwaites Glacier", "uid": "601514", "west": -107.38}, {"awards": "1341663 O\u0027Brien, Kristin; 1341602 Crockett, Elizabeth", "bounds_geometry": null, "date_created": "Thu, 24 Dec 2020 00:00:00 GMT", "description": "Antarctic notothenioids are noted for extreme stenothermy, yet underpinnings of their thermal limits are not fully understood. We hypothesized that properties of ventricular membranes could explain previously observed differences among notothenioids in temperature onset of cardiac arrhythmias and persistent asystole. Microsomes were prepared using ventricles from six species of notothenioids, including four species from the hemoglobin-less (Hb-) family Channichthyidae (icefishes), which also differentially express cardiac myoglobin (Mb), and two species from the (Hb+) Nototheniidae. We determined membrane fluidity and structural integrity by quantifying fluorescence depolarization of 1,6-diphenyl-1,3,5-hexatriene (DPH) and leakage of 5(6)-carboxyfluorescein, respectively, over a temperature range from ambient (0 \u00b0C) to 20 \u00b0C. Compositions of membrane phospholipids and cholesterol contents were also quantified. Membranes from all four species of icefishes exhibited greater fluidity than membranes from the red-blooded species N. coriiceps. Thermal sensitivity of fluidity did not vary among species. The greatest thermal sensitivity to leakage occurred between 0 and 5 \u00b0C for all species, while membranes from the icefish, Chaenocephalus aceratus (Hb-/Mb-) displayed leakage that was nearly 1.5-fold greater than leakage in N. coriiceps (Hb+/Mb+). Contents of phosphatidylethanolamine (PE) were approximately 1.5-fold greater in icefishes than in red-blooded fishes, and phospholipids had a higher degree of unsaturation in icefishes than in Hb + notothenioids. Cholesterol contents were lowest in Champsocephalus gunnari (Hb-/Mb-) and highest in the two Hb+/Mb + species, G. gibberifrons and N. coriiceps. Our results reveal marked differences in membrane properties and indicate a breach in membrane fluidity and structural integrity at a lower temperature in icefishes than in red-blooded notothenioids. ", "east": null, "geometry": null, "keywords": "Antarctica; Antarctic Peninsula", "locations": "Antarctic Peninsula; Antarctica", "north": null, "nsf_funding_programs": "Antarctic Organisms and Ecosystems; Antarctic Organisms and Ecosystems", "persons": "O\u0027Brien, Kristin; Evans, Elizabeth; Farnoud, Amir; Crockett, Elizabeth", "project_titles": "Collaborative Research: The Physiological and Biochemical Underpinnings of Thermal Tolerance in Antarctic Notothenioid Fishes", "projects": [{"proj_uid": "p0010084", "repository": "USAP-DC", "title": "Collaborative Research: The Physiological and Biochemical Underpinnings of Thermal Tolerance in Antarctic Notothenioid Fishes"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": null, "title": "Thermal sensitivity of membrane fluidity and integrity in hearts of Antarctic fishes that vary in expression of hemoglobin and myoglobin", "uid": "601414", "west": null}, {"awards": "0087401 Smith, Walker", "bounds_geometry": ["POLYGON((-179.999 -77,-179.1991 -77,-178.3992 -77,-177.5993 -77,-176.7994 -77,-175.9995 -77,-175.1996 -77,-174.3997 -77,-173.5998 -77,-172.7999 -77,-172 -77,-172 -77.07,-172 -77.14,-172 -77.21,-172 -77.28,-172 -77.35,-172 -77.42,-172 -77.49,-172 -77.56,-172 -77.63,-172 -77.7,-172.7999 -77.7,-173.5998 -77.7,-174.3997 -77.7,-175.1996 -77.7,-175.9995 -77.7,-176.7994 -77.7,-177.5993 -77.7,-178.3992 -77.7,-179.1991 -77.7,-179.999 -77.7,-179.999 -77.63,-179.999 -77.56,-179.999 -77.49,-179.999 -77.42,-179.999 -77.35,-179.999 -77.28,-179.999 -77.21,-179.999 -77.14,-179.999 -77.07,-179.999 -77))"], "date_created": "Wed, 17 Jun 2020 00:00:00 GMT", "description": "This data set was acquired with a Turner Designs 10-AU-005 Fluorometer and WET Labs FLSB Fluorometer on moorings deployed in the Ross Sea in December 2005. Moorings were retrieved during Nathaniel B. Palmer expedition NBP0601A conducted in 2006 (Chief Scientist: Dr. Walker Smith; Investigator(s): Dr. Vernon Asper). These data files are of ASCII format and include Fluorescence data. Data were acquired as part of the project(s): Interannual variability in the Antarctic - Ross Sea (IVARS): Nutrients, and funding was provided by NSF grant(s): ANT00-87401.", "east": -172.0, "geometry": ["POINT(-175.9995 -77.35)"], "keywords": "Antarctica; Flourometer; Mooring; NBP0601A; Ross Sea; Southern Ocean", "locations": "Antarctica; Southern Ocean; Ross Sea", "north": -77.0, "nsf_funding_programs": "Antarctic Organisms and Ecosystems", "persons": "Asper, Vernon; Smith, Walker", "project_titles": "Interannual Variability in the Antarctic-Ross Sea (IVARS): Nutrients and Seasonal Production", "projects": [{"proj_uid": "p0000803", "repository": "USAP-DC", "title": "Interannual Variability in the Antarctic-Ross Sea (IVARS): Nutrients and Seasonal Production"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -77.7, "title": "Fluorometer Data acquired on Moorings deployed the Ross Sea and recovered during the Nathaniel B. Palmer expedition NBP0601A (2006)", "uid": "601333", "west": -179.999}, {"awards": "1141978 Foreman, Christine", "bounds_geometry": ["POINT(161.667 -77.117)"], "date_created": "Tue, 19 Dec 2017 00:00:00 GMT", "description": "Metadata presented include Fourier transform ion cyclotron resonance mass spectrometry characterization of carbon source material molecular composition for three isolated lyophilized OM samples: Cotton Glacier Supraglacial stream, IHSS Pony Lake, and IHSS Suwannee River", "east": 161.667, "geometry": ["POINT(161.667 -77.117)"], "keywords": "Antarctica; Biota; Chemistry:fluid; Chemistry:Fluid; Fluorescence Spectroscopy; Mass Spectrometry", "locations": "Antarctica", "north": -77.117, "nsf_funding_programs": "Antarctic Organisms and Ecosystems", "persons": "D\u0027Andrilli, Juliana; Foreman, Christine", "project_titles": "Multidimensional \"omics\" characterization of microbial metabolism and dissolved organic matter in Antarctica", "projects": [{"proj_uid": "p0000408", "repository": "USAP-DC", "title": "Multidimensional \"omics\" characterization of microbial metabolism and dissolved organic matter in Antarctica"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -77.117, "title": "FT-ICR MS Metadata", "uid": "601077", "west": 161.667}, {"awards": "1141978 Foreman, Christine", "bounds_geometry": ["POINT(161.667 -77.117)"], "date_created": "Tue, 19 Dec 2017 00:00:00 GMT", "description": "Metadata presented include high resolution respiration data from Janthinobacterium sp. CG3 for three dissolved organic matter samples Cotton Glacier Supraglacial stream, Pony Lake fulvic acid, and Suwannee River Natural Organic Matter (NOM).", "east": 161.667, "geometry": ["POINT(161.667 -77.117)"], "keywords": "Antarctica; Biota; Chemistry:fluid; Chemistry:Fluid; Fluorescence Spectroscopy; Mass Spectrometry", "locations": "Antarctica", "north": -77.117, "nsf_funding_programs": "Antarctic Organisms and Ecosystems", "persons": "Foreman, Christine; Smith, Heidi", "project_titles": "Multidimensional \"omics\" characterization of microbial metabolism and dissolved organic matter in Antarctica", "projects": [{"proj_uid": "p0000408", "repository": "USAP-DC", "title": "Multidimensional \"omics\" characterization of microbial metabolism and dissolved organic matter in Antarctica"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -77.117, "title": "Respiration Metadata", "uid": "601076", "west": 161.667}, {"awards": "0839075 Priscu, John", "bounds_geometry": ["POINT(-112.08648 -79.46763)"], "date_created": "Mon, 06 Mar 2017 00:00:00 GMT", "description": "This data set include depth (WDC06A-7 dating) and fluorescence intensity measurements for five fluorophore regions (A, C, M, B, and T) commonly found in natural organic matter. Data from 1300-1700m, 1700-2100m, and 2100-2700m correspond to the early Holocene, deglaciation period, and the Last Glacial Maximum.", "east": -112.08648, "geometry": ["POINT(-112.08648 -79.46763)"], "keywords": "Antarctica; Fluorescence Spectroscopy; Glaciers/ice Sheet; Glaciers/Ice Sheet; Glaciology; Ice Core Records; Physical Properties; WAIS Divide; WAIS Divide Ice Core", "locations": "Antarctica; WAIS Divide", "north": -79.46763, "nsf_funding_programs": null, "persons": "Priscu, John; D\u0027Andrilli, Juliana", "project_titles": "Collaborative Research: Integrated High Resolution Chemical and Biological Measurements on the Deep WAIS Divide Core", "projects": [{"proj_uid": "p0000273", "repository": "USAP-DC", "title": "Collaborative Research: Integrated High Resolution Chemical and Biological Measurements on the Deep WAIS Divide Core"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": "WAIS Divide Ice Core", "south": -79.46763, "title": "Fluorescence spectroscopy data from the West Antarctic Ice Sheet (WAIS) Divide ice core, WDC06A", "uid": "601006", "west": -112.08648}, {"awards": "0838970 Foreman, Christine", "bounds_geometry": ["POINT(161.667 -77.117)"], "date_created": "Wed, 01 Jan 2014 00:00:00 GMT", "description": "Dissolved organic matter (DOM) comprises a significant pool of Earth\u0027s organic carbon that dwarfs the amount present in living aquatic organisms. The properties and reactivity of DOM are not well defined, and the evolution of autochthonous DOM from its precursor materials in freshwater has not been observed. Recent sampling of a supraglacial stream formed on the Cotton Glacier in the Transantarctic Mountains revealed DOM that more closely resembles an assemblage of recognizable precursor organic compounds, based upon its UV-VIS and fluorescence spectra. It is suggested that the DOM from this water evolved over time to resemble materials present in marine and many inland surface waters. The transient nature of the system i.e., it reforms seasonally, also prevents any accumulation of the refractory DOM present in most surface waters. Thus, the Cotton Glacier provides us with a unique environment to study the formation of DOM from precursor materials. An interdisciplinary team will study the biogeochemistry of this progenitor DOM and how microbes modify it. By focusing on the chemical composition of the DOM as it shifts from precursor material to the more humified fractions, the investigators will relate this transition to bioavailability, enzymatic activity, community composition and microbial growth efficiency. This project will support education at all levels, K-12, high school, undergraduate, graduate and post-doc and will increase participation by under-represented groups in science. Towards these goals, the investigators have established relationships with girls\u0027 schools and Native American programs. Additional outreach will be carried out in coordination with PolarTREC, PolarPalooza, and if possible, an Antarctic Artist and Writer.\n", "east": 161.667, "geometry": ["POINT(161.667 -77.117)"], "keywords": "Antarctica; Biota; Glaciers/ice Sheet; Glaciers/Ice Sheet; Glaciology; Microbiology", "locations": "Antarctica", "north": -77.117, "nsf_funding_programs": null, "persons": "Foreman, Christine", "project_titles": "Collaborative Research: The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica", "projects": [{"proj_uid": "p0000458", "repository": "USAP-DC", "title": "Collaborative Research: The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -77.117, "title": "The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica", "uid": "600104", "west": 161.667}, {"awards": "9814810 Bales, Roger", "bounds_geometry": ["POLYGON((-124 -76,-120 -76,-116 -76,-112 -76,-108 -76,-104 -76,-100 -76,-96 -76,-92 -76,-88 -76,-84 -76,-84 -77.4,-84 -78.8,-84 -80.2,-84 -81.6,-84 -83,-84 -84.4,-84 -85.8,-84 -87.2,-84 -88.6,-84 -90,-88 -90,-92 -90,-96 -90,-100 -90,-104 -90,-108 -90,-112 -90,-116 -90,-120 -90,-124 -90,-124 -88.6,-124 -87.2,-124 -85.8,-124 -84.4,-124 -83,-124 -81.6,-124 -80.2,-124 -78.8,-124 -77.4,-124 -76))"], "date_created": "Tue, 16 Jun 2009 00:00:00 GMT", "description": "This data set contains atmospheric mixing ratios of hydrogen peroxide and methylhydroperoxide at 21 sites on the West Antarctic Ice Sheet (WAIS) were obtained from 2000 to 2003 during the US International Trans-Antarctic Scientific Expedition (US ITASE) deployments. Sample location from the WAIS region (76-90\u00baS / 84-124\u00baW) were approximately 100-300 km apart and correspond to US ITASE ice core sites. At each site, ambient air from 1 m above the snow surface was sampled between two to five days. Atmospheric hydroperoxides (ROOH) were continuously scrubbed from the sample air with a glass coil scrubber and subsequently quantified using a fluorescence detection method.\n\nData are available via FTP as ASCII text files (.txt).", "east": -84.0, "geometry": ["POINT(-104 -83)"], "keywords": "Antarctica; Atmosphere; Chemistry:fluid; Chemistry:Fluid; Geochemistry; Glaciers/ice Sheet; Glaciers/Ice Sheet; ITASE; WAIS", "locations": "Antarctica; WAIS", "north": -76.0, "nsf_funding_programs": "Antarctic Glaciology", "persons": "McConnell, Joseph; Bales, Roger; Frey, Markus", "project_titles": "Hydrogen Peroxide, Formaldehyde, and Sub-Annual Snow Accumulation in West Antarctica: Participation in West Antarctic Traverse", "projects": [{"proj_uid": "p0000253", "repository": "USAP-DC", "title": "Hydrogen Peroxide, Formaldehyde, and Sub-Annual Snow Accumulation in West Antarctica: Participation in West Antarctic Traverse"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -90.0, "title": "Atmospheric Mixing Ratios of Hydroperoxides above the West Antarctic Ice Sheet", "uid": "609394", "west": -124.0}, {"awards": "0536870 Rogers, Scott", "bounds_geometry": ["POINT(106.8 -72.4667)"], "date_created": "Tue, 01 Jan 2008 00:00:00 GMT", "description": "The large subglacial Lake Vostok in Antarctica is unique ecological site with a novel microbial biota. The temperatures, pressures and lack of light all select for organisms that may not exist anywhere else on Earth. The accretion ice (lake water frozen to the bottom of the lower surface of the glacier) has preserved microbial samples from each region of Lake Vostok as the glacier passes over and into the lake. Thus, without contaminating the lake with microorganisms from the surface, microbes originating from the lake can be collected, transported to the laboratory and studied. Two of the deepest ice cores sections in this project are part of the international allocation. \n\nThe will be shared between four researchers (Sergey Bulat from Russia, Jean-Robert Petit and Daniel Prieur from France, Scott Rogers from USA). The United States team will study, isolate, and characterize bacteria, fungi, and viruses that have been sampled from the lake through the process of ice accretion to the lower surface of 3500+m thick glacier overriding the lake. The project will involve a suite of methods, including molecular, morphological, and cultural. This includes observation and description by fluorescence, light, and electron microscopy, isolation on thirteen separate cultural media, polymerase chain reaction amplification, DNA sequencing, and phylogenetic analyses. Eleven accretion ice core sections, as well as two glacial ice core sections. As well as two glacial ice core sections will be studied. The accretion ice core sections, as well as two glacial ice core sections will be studied. The accretion ice core sections represent all of the major regions of the lake that have been sampled by the accretion process in the vicinity of the Vostok 5G ice core. The broader impacts of the work relate to the impact the results will have on the filed. These long=isolated lakes, deep below the Antarctic ice sheet may contain novel uniquely adapted organisms. Glacial ice contains an enormous diversity of entrapped microbes, some of which may be metabolically active in the ice. The microbes from Lake Vostok are of special interest, since they are adapted to cold, dark, and high pressure. Thus, their enzyme systems and biochemical pathways may be significantly different from those in the microbes that are the subject of current studies. As such, these organisms may form compounds that may have useful applications. Also, study of the accretion ice, and eventually the water, from Lake Vostok will provide a basis for the study of other subglacial lakes. Additionally, study of the microbes in the accretion ice will be useful to those planning to study analogous systems on ice-covered planets and moons.", "east": 106.8, "geometry": ["POINT(106.8 -72.4667)"], "keywords": "Antarctica; Biota; Cryosphere; Glaciers/ice Sheet; Glaciers/Ice Sheet; Glaciology; Hydrothermal Vent; Lake Vostok; Microbes; Subglacial Lake", "locations": "Antarctica; Lake Vostok", "north": -72.4667, "nsf_funding_programs": null, "persons": "Rogers, Scott O.", "project_titles": "Comprehensive Biological Study of Vostok Accretion Ice", "projects": [{"proj_uid": "p0000566", "repository": "USAP-DC", "title": "Comprehensive Biological Study of Vostok Accretion Ice"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -72.4667, "title": "Comprehensive Biological Study of Vostok Accretion Ice", "uid": "600052", "west": 106.8}]
X
X
Help on the Results MapX
This window can be dragged by its header, and can be resized from the bottom right corner.
Clicking the Layers button - the blue square in the top left of the Results Map - will display a list of map layers you can add or remove
from the currently displayed map view.
The Results Map and the Results Table
- The Results Map displays the centroids of the geographic bounds of all the results returned by the search.
- Results that are displayed in the current map view will be highlighted in blue and brought to the top of the Results Table.
- As the map is panned or zoomed, the highlighted rows in the table will update.
- If you click on a centroid on the map, it will turn yellow and display a popup with details for that project/dataset - including a link to the landing page. The bounds for the project(s)/dataset(s) selected will be displayed in red. The selected result(s) will be highlighted in red and brought to the top of the table.
- The default table sorting order is: Selected, Visible, Date (descending), but this can be changed by clicking on column headers in the table.
- Selecting Show on Map for an individual row will both display the geographic bounds for that result on a mini map, and also display the bounds and highlight the centroid on the Results Map.
- Clicking the 'Show boundaries' checkbox at the top of the Results Map will display all the bounds for the filtered results.
Defining a search area on the Results Map
- If you click on the Rectangle or Polygon icons in the top right of the Results Map, you can define a search area which will be added to any other search criteria already selected.
- After you have drawn a polygon, you can edit it using the Edit Geometry dropdown in the search form at the top.
- Clicking Clear in the map will clear any drawn polygon.
- Clicking Search in the map, or Search on the form will have the same effect.
- The returned results will be any projects/datasets with bounds that intersect the polygon.
- Use the Exclude project/datasets checkbox to exclude any projects/datasets that cover the whole Antarctic region.
Viewing map layers on the Results Map
To sort the table of search results, click the header of the column you wish to search by. To sort by multiple columns, hold down the shift key whilst selecting the sort columns in order.
| Dataset Title/Abstract/Map | NSF Award(s) | Date Created | PIs / Scientists | Project Links | Abstract | Bounds Geometry | Geometry | Selected | Visible |
|---|---|---|---|---|---|---|---|---|---|
|
Water column data collected by sea gliders in the Ross Sea in 2022 and 2023
|
2040571 |
2026-01-07 | Smith, Walker |
NSFGEO-NERC: Collaborative Research "P2P: Predators to Plankton -Biophysical Controls in Antarctic Polynyas" |
The data were collected by two gliders deployed in the southern Ross Sea from November, 2022 to January, 2023. They include water column data on temperature, salinity, optical backscatter at two wave lengths, fluorescence, and photosynthetically active radiation. | ["POLYGON((168 -76.2,168.2 -76.2,168.4 -76.2,168.6 -76.2,168.8 -76.2,169 -76.2,169.2 -76.2,169.4 -76.2,169.6 -76.2,169.8 -76.2,170 -76.2,170 -76.28,170 -76.36,170 -76.44,170 -76.52,170 -76.6,170 -76.68,170 -76.76,170 -76.84,170 -76.92,170 -77,169.8 -77,169.6 -77,169.4 -77,169.2 -77,169 -77,168.8 -77,168.6 -77,168.4 -77,168.2 -77,168 -77,168 -76.92,168 -76.84,168 -76.76,168 -76.68,168 -76.6,168 -76.52,168 -76.44,168 -76.36,168 -76.28,168 -76.2))"] | ["POINT(169 -76.6)"] | false | false |
|
Raw flow cytometry data from Palmer Peninsula
|
1846837 |
2025-05-13 | Bowman, Jeff; Connors, Elizabeth |
CAREER: Understanding microbial heterotrophic processes in coastal Antarctic waters |
Raw flow cytometry data from Palmer Station for the 2023-2023 field season. Includes CSV files and raw FCS files for SYBR Green, autofluorescence, RedoxSensor Green. Data are included for environmental samples collected at Palmer LTER Station E and for bacterial mortality (dilution) experiments. | ["POINT(-64.053 -64.77)"] | ["POINT(-64.053 -64.77)"] | false | false |
|
Dissolved nutrients, cell counts, and nitrogen isotope measurements from Chaetoceros socialis culture experiments
|
1744871 |
2023-08-30 | Dove, Isabel |
The nitrogen isotopic composition of diatom resting spores in Southern Ocean sediments: A source of bias and/or paleoenvironmental information? |
This dataset is the results of 3 experiments in which the spore-forming diatom Chaetoceros socialis was grown in culture and induced into resting spores by nitrate limitation. The nitrogen isotopic composition of accumulated biomass (δ15Nbiomass; ‰ vs air) and of diatom-bound organic N (δ15Ndb; ‰ vs air) are reported at two timepoints from each experiment: prior to and after resting spore formation. Experiments 1 and 2 provide measurements for CRS mixed with vegetative Chaetoceros cells, while Experiment 3 provides measurements for isolated CRS. Fluorescence and nitrate concentration was tracked throughout each experiment, with dissolved silica, ammonium, and total reduced nitrogen also measured in Experiment 3. | [] | [] | false | false |
|
Flow cytometry enumeration of virus-like and bacteria-like abundance in Ace, Deep, & Organic lakes (Antarctica)
|
1644155 |
2022-12-12 | Twining, Benjamin; Martinez-Martinez, Joaquin |
Viral control of microbial communities in Antarctic lakes |
Varying depth samples from Ace, Deep, & Organic Lake were obtained between 2013-2014. These samples were size fractionated by filtration for metagenomic analyses. Viral and bacterial abundances were determine on the filtrate fractions by flow cytometric analysis. Glutaraldehyde-fixed samples were stained with SYBR Green I fluorescence dye and virus-like particle (VLP) and bacteria-like cell (BLC) populations were discriminated based on green fluorescence and side scatter flow cytometry signals. Several distinct VLP and BLC populations where enumerated from Ace Lake and Organic Lake samples that revealed temporal and depth differences. Discrete VLP and BLC populations could not be discerned from Deep Lake samples. These files include the original flow cytometry particle counts (raw data), the gating templates used to count VLP and BLC populations (analysis_templates), and the resulting particle counts (analyzed). | ["POLYGON((-78.1833 -68.4333,-78.16499 -68.4333,-78.14668 -68.4333,-78.12837 -68.4333,-78.11006 -68.4333,-78.09175 -68.4333,-78.07344 -68.4333,-78.05513 -68.4333,-78.03682 -68.4333,-78.01851 -68.4333,-78.0002 -68.4333,-78.0002 -68.43664,-78.0002 -68.43998,-78.0002 -68.44332,-78.0002 -68.44666000000001,-78.0002 -68.45,-78.0002 -68.45334,-78.0002 -68.45668,-78.0002 -68.46002,-78.0002 -68.46336000000001,-78.0002 -68.4667,-78.01851 -68.4667,-78.03682 -68.4667,-78.05513 -68.4667,-78.07344 -68.4667,-78.09175 -68.4667,-78.11006 -68.4667,-78.12837 -68.4667,-78.14668 -68.4667,-78.16499 -68.4667,-78.1833 -68.4667,-78.1833 -68.46336000000001,-78.1833 -68.46002,-78.1833 -68.45668,-78.1833 -68.45334,-78.1833 -68.45,-78.1833 -68.44666000000001,-78.1833 -68.44332,-78.1833 -68.43998,-78.1833 -68.43664,-78.1833 -68.4333))"] | ["POINT(-78.09175 -68.45)"] | false | false |
|
Physical and geochemical data from five sediment cores collected offshore Thwaites Glacier
|
1738942 |
2022-01-27 | Lepp, Allison |
NSF-NERC: THwaites Offshore Research (THOR) |
This dataset contains measurements from grain-size, x-ray fluorescence (XRF), and physical properties (including magnetic susceptibility, water content, and shear strength) analyses of five sediment cores collected offshore Thwaites Glacier during cruises NBP19-02 (cores KC04, KC08, and KC23) and NBP20-02 (cores KC33 and KC67). We estimate the cores, which are between 213.5 and 297.5 cm in length, reflect deposition during the last ~10 kyr, consistent with published constraints of deglaciation of this region. Data are organized in Microsoft Excel spreadsheets and core locations are provided in a PDF. | ["POLYGON((-107.38 -74.64,-107.065 -74.64,-106.75 -74.64,-106.435 -74.64,-106.12 -74.64,-105.805 -74.64,-105.49 -74.64,-105.175 -74.64,-104.86 -74.64,-104.545 -74.64,-104.23 -74.64,-104.23 -74.683,-104.23 -74.726,-104.23 -74.769,-104.23 -74.812,-104.23 -74.855,-104.23 -74.898,-104.23 -74.941,-104.23 -74.984,-104.23 -75.027,-104.23 -75.07,-104.545 -75.07,-104.86 -75.07,-105.175 -75.07,-105.49 -75.07,-105.805 -75.07,-106.12 -75.07,-106.435 -75.07,-106.75 -75.07,-107.065 -75.07,-107.38 -75.07,-107.38 -75.027,-107.38 -74.984,-107.38 -74.941,-107.38 -74.898,-107.38 -74.855,-107.38 -74.812,-107.38 -74.769,-107.38 -74.726,-107.38 -74.683,-107.38 -74.64))"] | ["POINT(-105.805 -74.855)"] | false | false |
|
Thermal sensitivity of membrane fluidity and integrity in hearts of Antarctic fishes that vary in expression of hemoglobin and myoglobin
|
1341663 1341602 |
2020-12-24 | O'Brien, Kristin; Evans, Elizabeth; Farnoud, Amir; Crockett, Elizabeth |
Collaborative Research: The Physiological and Biochemical Underpinnings of Thermal Tolerance in Antarctic Notothenioid Fishes |
Antarctic notothenioids are noted for extreme stenothermy, yet underpinnings of their thermal limits are not fully understood. We hypothesized that properties of ventricular membranes could explain previously observed differences among notothenioids in temperature onset of cardiac arrhythmias and persistent asystole. Microsomes were prepared using ventricles from six species of notothenioids, including four species from the hemoglobin-less (Hb-) family Channichthyidae (icefishes), which also differentially express cardiac myoglobin (Mb), and two species from the (Hb+) Nototheniidae. We determined membrane fluidity and structural integrity by quantifying fluorescence depolarization of 1,6-diphenyl-1,3,5-hexatriene (DPH) and leakage of 5(6)-carboxyfluorescein, respectively, over a temperature range from ambient (0 °C) to 20 °C. Compositions of membrane phospholipids and cholesterol contents were also quantified. Membranes from all four species of icefishes exhibited greater fluidity than membranes from the red-blooded species N. coriiceps. Thermal sensitivity of fluidity did not vary among species. The greatest thermal sensitivity to leakage occurred between 0 and 5 °C for all species, while membranes from the icefish, Chaenocephalus aceratus (Hb-/Mb-) displayed leakage that was nearly 1.5-fold greater than leakage in N. coriiceps (Hb+/Mb+). Contents of phosphatidylethanolamine (PE) were approximately 1.5-fold greater in icefishes than in red-blooded fishes, and phospholipids had a higher degree of unsaturation in icefishes than in Hb + notothenioids. Cholesterol contents were lowest in Champsocephalus gunnari (Hb-/Mb-) and highest in the two Hb+/Mb + species, G. gibberifrons and N. coriiceps. Our results reveal marked differences in membrane properties and indicate a breach in membrane fluidity and structural integrity at a lower temperature in icefishes than in red-blooded notothenioids. | [] | [] | false | false |
|
Fluorometer Data acquired on Moorings deployed the Ross Sea and recovered during the Nathaniel B. Palmer expedition NBP0601A (2006)
|
0087401 |
2020-06-17 | Asper, Vernon; Smith, Walker |
Interannual Variability in the Antarctic-Ross Sea (IVARS): Nutrients and Seasonal Production |
This data set was acquired with a Turner Designs 10-AU-005 Fluorometer and WET Labs FLSB Fluorometer on moorings deployed in the Ross Sea in December 2005. Moorings were retrieved during Nathaniel B. Palmer expedition NBP0601A conducted in 2006 (Chief Scientist: Dr. Walker Smith; Investigator(s): Dr. Vernon Asper). These data files are of ASCII format and include Fluorescence data. Data were acquired as part of the project(s): Interannual variability in the Antarctic - Ross Sea (IVARS): Nutrients, and funding was provided by NSF grant(s): ANT00-87401. | ["POLYGON((-179.999 -77,-179.1991 -77,-178.3992 -77,-177.5993 -77,-176.7994 -77,-175.9995 -77,-175.1996 -77,-174.3997 -77,-173.5998 -77,-172.7999 -77,-172 -77,-172 -77.07,-172 -77.14,-172 -77.21,-172 -77.28,-172 -77.35,-172 -77.42,-172 -77.49,-172 -77.56,-172 -77.63,-172 -77.7,-172.7999 -77.7,-173.5998 -77.7,-174.3997 -77.7,-175.1996 -77.7,-175.9995 -77.7,-176.7994 -77.7,-177.5993 -77.7,-178.3992 -77.7,-179.1991 -77.7,-179.999 -77.7,-179.999 -77.63,-179.999 -77.56,-179.999 -77.49,-179.999 -77.42,-179.999 -77.35,-179.999 -77.28,-179.999 -77.21,-179.999 -77.14,-179.999 -77.07,-179.999 -77))"] | ["POINT(-175.9995 -77.35)"] | false | false |
|
FT-ICR MS Metadata
|
1141978 |
2017-12-19 | D'Andrilli, Juliana; Foreman, Christine |
Multidimensional "omics" characterization of microbial metabolism and dissolved organic matter in Antarctica |
Metadata presented include Fourier transform ion cyclotron resonance mass spectrometry characterization of carbon source material molecular composition for three isolated lyophilized OM samples: Cotton Glacier Supraglacial stream, IHSS Pony Lake, and IHSS Suwannee River | ["POINT(161.667 -77.117)"] | ["POINT(161.667 -77.117)"] | false | false |
|
Respiration Metadata
|
1141978 |
2017-12-19 | Foreman, Christine; Smith, Heidi |
Multidimensional "omics" characterization of microbial metabolism and dissolved organic matter in Antarctica |
Metadata presented include high resolution respiration data from Janthinobacterium sp. CG3 for three dissolved organic matter samples Cotton Glacier Supraglacial stream, Pony Lake fulvic acid, and Suwannee River Natural Organic Matter (NOM). | ["POINT(161.667 -77.117)"] | ["POINT(161.667 -77.117)"] | false | false |
|
Fluorescence spectroscopy data from the West Antarctic Ice Sheet (WAIS) Divide ice core, WDC06A
|
0839075 |
2017-03-06 | Priscu, John; D'Andrilli, Juliana |
Collaborative Research: Integrated High Resolution Chemical and Biological Measurements on the Deep WAIS Divide Core |
This data set include depth (WDC06A-7 dating) and fluorescence intensity measurements for five fluorophore regions (A, C, M, B, and T) commonly found in natural organic matter. Data from 1300-1700m, 1700-2100m, and 2100-2700m correspond to the early Holocene, deglaciation period, and the Last Glacial Maximum. | ["POINT(-112.08648 -79.46763)"] | ["POINT(-112.08648 -79.46763)"] | false | false |
|
The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica
|
0838970 |
2014-01-01 | Foreman, Christine |
Collaborative Research: The Biogeochemical Evolution of Dissolved Organic Matter in a Fluvial System on the Cotton Glacier, Antarctica |
Dissolved organic matter (DOM) comprises a significant pool of Earth's organic carbon that dwarfs the amount present in living aquatic organisms. The properties and reactivity of DOM are not well defined, and the evolution of autochthonous DOM from its precursor materials in freshwater has not been observed. Recent sampling of a supraglacial stream formed on the Cotton Glacier in the Transantarctic Mountains revealed DOM that more closely resembles an assemblage of recognizable precursor organic compounds, based upon its UV-VIS and fluorescence spectra. It is suggested that the DOM from this water evolved over time to resemble materials present in marine and many inland surface waters. The transient nature of the system i.e., it reforms seasonally, also prevents any accumulation of the refractory DOM present in most surface waters. Thus, the Cotton Glacier provides us with a unique environment to study the formation of DOM from precursor materials. An interdisciplinary team will study the biogeochemistry of this progenitor DOM and how microbes modify it. By focusing on the chemical composition of the DOM as it shifts from precursor material to the more humified fractions, the investigators will relate this transition to bioavailability, enzymatic activity, community composition and microbial growth efficiency. This project will support education at all levels, K-12, high school, undergraduate, graduate and post-doc and will increase participation by under-represented groups in science. Towards these goals, the investigators have established relationships with girls' schools and Native American programs. Additional outreach will be carried out in coordination with PolarTREC, PolarPalooza, and if possible, an Antarctic Artist and Writer. | ["POINT(161.667 -77.117)"] | ["POINT(161.667 -77.117)"] | false | false |
|
Atmospheric Mixing Ratios of Hydroperoxides above the West Antarctic Ice Sheet
|
9814810 |
2009-06-16 | McConnell, Joseph; Bales, Roger; Frey, Markus |
Hydrogen Peroxide, Formaldehyde, and Sub-Annual Snow Accumulation in West Antarctica: Participation in West Antarctic Traverse |
This data set contains atmospheric mixing ratios of hydrogen peroxide and methylhydroperoxide at 21 sites on the West Antarctic Ice Sheet (WAIS) were obtained from 2000 to 2003 during the US International Trans-Antarctic Scientific Expedition (US ITASE) deployments. Sample location from the WAIS region (76-90ºS / 84-124ºW) were approximately 100-300 km apart and correspond to US ITASE ice core sites. At each site, ambient air from 1 m above the snow surface was sampled between two to five days. Atmospheric hydroperoxides (ROOH) were continuously scrubbed from the sample air with a glass coil scrubber and subsequently quantified using a fluorescence detection method. Data are available via FTP as ASCII text files (.txt). | ["POLYGON((-124 -76,-120 -76,-116 -76,-112 -76,-108 -76,-104 -76,-100 -76,-96 -76,-92 -76,-88 -76,-84 -76,-84 -77.4,-84 -78.8,-84 -80.2,-84 -81.6,-84 -83,-84 -84.4,-84 -85.8,-84 -87.2,-84 -88.6,-84 -90,-88 -90,-92 -90,-96 -90,-100 -90,-104 -90,-108 -90,-112 -90,-116 -90,-120 -90,-124 -90,-124 -88.6,-124 -87.2,-124 -85.8,-124 -84.4,-124 -83,-124 -81.6,-124 -80.2,-124 -78.8,-124 -77.4,-124 -76))"] | ["POINT(-104 -83)"] | false | false |
|
Comprehensive Biological Study of Vostok Accretion Ice
|
0536870 |
2008-01-01 | Rogers, Scott O. |
Comprehensive Biological Study of Vostok Accretion Ice |
The large subglacial Lake Vostok in Antarctica is unique ecological site with a novel microbial biota. The temperatures, pressures and lack of light all select for organisms that may not exist anywhere else on Earth. The accretion ice (lake water frozen to the bottom of the lower surface of the glacier) has preserved microbial samples from each region of Lake Vostok as the glacier passes over and into the lake. Thus, without contaminating the lake with microorganisms from the surface, microbes originating from the lake can be collected, transported to the laboratory and studied. Two of the deepest ice cores sections in this project are part of the international allocation. The will be shared between four researchers (Sergey Bulat from Russia, Jean-Robert Petit and Daniel Prieur from France, Scott Rogers from USA). The United States team will study, isolate, and characterize bacteria, fungi, and viruses that have been sampled from the lake through the process of ice accretion to the lower surface of 3500+m thick glacier overriding the lake. The project will involve a suite of methods, including molecular, morphological, and cultural. This includes observation and description by fluorescence, light, and electron microscopy, isolation on thirteen separate cultural media, polymerase chain reaction amplification, DNA sequencing, and phylogenetic analyses. Eleven accretion ice core sections, as well as two glacial ice core sections. As well as two glacial ice core sections will be studied. The accretion ice core sections, as well as two glacial ice core sections will be studied. The accretion ice core sections represent all of the major regions of the lake that have been sampled by the accretion process in the vicinity of the Vostok 5G ice core. The broader impacts of the work relate to the impact the results will have on the filed. These long=isolated lakes, deep below the Antarctic ice sheet may contain novel uniquely adapted organisms. Glacial ice contains an enormous diversity of entrapped microbes, some of which may be metabolically active in the ice. The microbes from Lake Vostok are of special interest, since they are adapted to cold, dark, and high pressure. Thus, their enzyme systems and biochemical pathways may be significantly different from those in the microbes that are the subject of current studies. As such, these organisms may form compounds that may have useful applications. Also, study of the accretion ice, and eventually the water, from Lake Vostok will provide a basis for the study of other subglacial lakes. Additionally, study of the microbes in the accretion ice will be useful to those planning to study analogous systems on ice-covered planets and moons. | ["POINT(106.8 -72.4667)"] | ["POINT(106.8 -72.4667)"] | false | false |

