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  • 1
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    PANGAEA
    In:  Supplement to: Skinner, Luke C; Fallon, Robert D; Waelbroeck, Claire; Michel, Elisabeth; Barker, S (2010): Ventilation of the Deep Southern Ocean and Deglacial CO2 Rise. Science, 328(5982), 1147-1151, https://doi.org/10.1126/science.1183627
    Publication Date: 2023-05-12
    Description: Past glacial-interglacial increases in the concentration of atmospheric carbon dioxide (CO2) are thought to arise from the rapid release of CO2 sequestered in the deep sea, primarily via the Southern Ocean. Here, we present radiocarbon evidence from the Atlantic sector of the Southern Ocean that strongly supports this hypothesis. We show that during the last glacial period, deep water circulating around Antarctica was more than two times older than today relative to the atmosphere. During deglaciation, the dissipation of this old and presumably CO2-enriched deep water played an important role in the pulsed rise of atmospheric CO2 through its variable influence on the upwelling branch of the Antarctic overturning circulation.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 2
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    PANGAEA
    In:  Supplement to: Puga-Bernabeu, Angel; Webster, Jody M; Braga, Juan-Carlos; Clague, David A; Dutton, Andrea; Eggins, Stephen M; Fallon, Robert D; Jacobsen, Geraldine; Paduan, Jennifer B; Potts, Donald C (2016): Morphology and evolution of drowned carbonate terraces during the last two interglacial cycles, off Hilo, NE Hawaii. Marine Geology, 371, 57-81, https://doi.org/10.1016/j.margeo.2015.10.016
    Publication Date: 2023-01-21
    Description: The eastern side of Hawaii Island is a rapidly subsiding margin dominated by drowned carbonate platforms. We present detailed bathymetric and backscatter data, remotely operated vehicle and submersible observations, sedimentological and 14C accelerator mass spectrometry and U/Th age data from seven submerged terraces (H7, H2a-d, H1a-b) in water depths between 1100 and 25 m off Hilo, north-eastern Hawaii. The main carbonate deposits on these terraces are coral deposits, rhodolith beds, coralline algal mounds, crusts, pavements and tabular sheets. We identified five previously described sedimentary shallow- to deep-water facies and one new facies type that are consistent with reef drowning on a rapidly subsiding margin. We used palaeobathymetric data derived from the sedimentary facies, age versus depth relationships, and published sea-level curves, to estimate a uniform long-term subsidence rate of 2.80 ± 0.36 m/ky for the eastern side of Hawaii over the last 150 ky. Terrace H7 developed about 380 ka based on data from the western side of the island. Active coral growth on terrace H2d occurred during the Marine Isotope Stage (MIS) 6 to 5 transition, and the terrace drowned during the peak of MIS 5e when sea level rose faster than reefs could grow. Favoured by the gentle platform gradient, reefs established progressively landwards with a backstepping pattern during MIS 5e to form the terraces H2c and H2b 122 ka. Final turn-off of shallow water carbonate production on terraces H2b-d coincided with the relative sea-level rise of the interstadial MIS 5a. Bathymetry and submersible data suggest that carbonate sediments on terraces H2a and H1b were deposited over an antecedent topography of local lava deltas emplaced during rising sea levels at ca. 85 and 65 ka, while terrace H1a established on lava delta substrates of the Mauna Loa volcano ca. 11 ka. We conclude that the initiation, growth and drowning of coral-reef terraces off Hilo differ in some ways from the pattern observed in the submerged terraces in the western side of Hawaii and that the platform evolution off Hilo is more strongly influenced by emplacement of offshore lava flows.
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 3
    Publication Date: 2023-01-21
    Keywords: Age, 14C calibrated, CALIB 7.0.2; Age, dated; Age, dated material; Age, dated standard error; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; Calendar age, standard error; DEPTH, water; Event label; Hawaiian Islands, North Central Pacific; HSDP-1_H1a-01; HSDP-1 (H1a); Laboratory code/label; Latitude of event; Longitude of event; MULT; Multiple investigations; Off-Hilo_H1b-01; Off-Hilo_H1b-02; Off-Hilo_H1b-03; Off-Hilo_H1b-04; Off-Hilo_H1b-05; Off-Hilo_H1b-06; Off-Hilo_H2a-01; Off Hilo (H1b); Off Hilo (H2a); Optional event label; Reference of data; Sample comment; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 307 data points
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  • 4
    Publication Date: 2023-05-12
    Keywords: Age, 14C AMS; Age, dated; Age, dated standard deviation; Age, difference; Age, difference error; Age, maximum/old; Age, minimum/young; Age, standard deviation; Age model; Age model, optional; Calypso Square Core System; CASQS; DEPTH, sediment/rock; IMAGES XV - Pachiderme; Laboratory code/label; Marion Dufresne (1995); MD07-3076; MD07-3076Q; MD159; Reservoir effect/correction
    Type: Dataset
    Format: text/tab-separated-values, 594 data points
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  • 5
    Publication Date: 2023-05-12
    Keywords: Age, 14C AMS; Age, 14C calibrated; Age, dated; Age, dated material; Age, dated standard deviation; Age, standard deviation; Age model; Calendar age; Calypso Square Core System; CASQS; DEPTH, sediment/rock; IMAGES XV - Pachiderme; Laboratory code/label; Marion Dufresne (1995); MD07-3076; MD07-3076Q; MD159; Reservoir effect/correction
    Type: Dataset
    Format: text/tab-separated-values, 472 data points
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  • 6
    Publication Date: 2023-06-27
    Keywords: 90b; Age, 14C AMS; Age, dated; Age, dated standard deviation; Age model; Calendar age; DEPTH, sediment/rock; IMAGES V; KAL; Kasten corer; Laboratory code/label; Marion Dufresne (1995); MD114; MD99-2334; Reference/source
    Type: Dataset
    Format: text/tab-separated-values, 51 data points
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  • 7
    Publication Date: 2023-07-05
    Keywords: Age, dated; Age, dated material; Age, dated standard error; Age, error; Age model; DEPTH, water; Event label; Hawaiian Islands, North Central Pacific; HSDP-1_H1a-02; HSDP-1 (H1a)a; Isotopic event; Latitude of event; Longitude of event; MC-ICP-MS Thermo-Finnigan Neptune; MULT; Multiple investigations; Off-Hilo_H2b-01; Off-Hilo_H2c-01; Off-Hilo_H2c-02; Off-Hilo_H2d-01; Off-Hilo_H2d-02; Off-Hilo_H2d-03; Off Hilo (H2b)b; Off Hilo (H2c)b; Off Hilo (H2d)b; Optional event label; Reference of data; Sample comment; Sample ID; Thorium-230/Uranium-238, standard deviation; Thorium-230/Uranium-238 ratio; Thorium-232; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation; Uranium-238; δ234 Uranium; δ234 Uranium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 317 data points
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Freshwater biology 11 (1981), S. 0 
    ISSN: 1365-2427
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. Microcystis, an important bloom-forming blue-green alga in Lake Mendota, Wisconsin, was found to accumulate at the lake bottom and overwinter there. Microcystis collected from winter sediments were photosynthetically active, showing temperature and light optima similar to summer and autumn populations. Sediments incubated under in situ conditions in the laboratory maintained photosynthetic activity for at least four months. Such a maintenance ability may be part of an overall strategy by Microcystis populations to ensure a suitable inoculum for the following growth season.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    FEMS microbiology ecology 13 (1994), S. 0 
    ISSN: 1574-6941
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Abstract The microorganisms participating in the anaerobic biodegradation of cyanide were characterized using 16S rRNA genes as genetic markers of diversity. Segments of mixed population 16S rRNA genes were amplified using the polymerase chain reaction (PCR) and prokaryote-specific amplification primers. Restriction fragment length polymorphism (RFLPs) and screening with the 926f universal sequencing primer were used to categorized the cloned PCR products. Six unique prokaryote sequence were obtained, including four similar to methanogens and two similar to Gram-positive eubacteria.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Biodegradation 7 (1989), S. 111-129 
    ISSN: 1572-9729
    Keywords: methanogenesis ; lipid synthesis ; acetate oxidation ; phospholipids ; ether lipids ; bacterial productivity
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract In anoxic salt marsh sediments of Sapelo Island, GA, USA, the vertical distribution of CH4 production was measured in the upper 20 cm of surface sediments in ten locations. In one section of high marsh sediments, the concentration and oxidation of acetate in sediment porewaters and the rate and amount of14C acetate and14CO2 incorporation into cellular lipids of the microbial population were investigated. CH4 production rates ranged from 〈1 to 493 nM CH4 gram sediment−1 day−1 from intact subcores incubated under nitrogen. Replacement with H2 stimulated the rate of methane release up to nine fold relative to N2 incubations. Rates of lipid synthesis from CO2 averaged 39.2 ×10−2nanomoles lipid carbon cm3 sediment−1 hr−1, suggesting that CO2 may be an important carbon precursor for microbial membrane synthesis in marsh sediments under anoxic conditions. Qualitative measurements of lipid synthesis rates from acetate were found to average 8.7 × 10−2 nanomoles. Phospholipids were the dominant lipids synthesized by both substrates in sediment cores, accounting for an average of 76.6% of all lipid radioactivity. Small amounts of ether lipids indicative of methanogenic bacteria were observed in cores incubated for 7 days, with similar rates of synthesis for both CO2 and acetate. The low rate of ether lipid synthesis suggests that either methanogen lipid biosynthesis is very slow or that methanogens represent a small component of total microbial lipid synthesis in anoxic sediments.
    Type of Medium: Electronic Resource
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