GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 201-1226B; 201-1226D; 201-1226E; 201-1227A; 201-1227D; 201-1228A; 201-1228E; 201-1230A; 201-1230B; 201-1231A; 201-1231B; 201-1231E; 301-U1301C; 307-U1317A; 308-U1319A; 308-U1320A; 308-U1322B; 308-U1324B; 315-C0001E; 315-C0001F; 315-C0002D; 316-C0004C; 316-C0006C; 316-C0006D; 316-C0006E; 316-C0007A; 316-C0007B; 316-C0007C; 316-C0008A; 316-C0008C; 329-U1365C; 329-U1365D; 329-U1366F; 329-U1367D; 329-U1368D; 329-U1369E; 329-U1370F; 329-U1371E; 329-U1371F; 346-U1423A; 346-U1424A; 346-U1426A; 346-U1428A; 347-M0059E; 347-M0060B; 347-M0063E; 347-M0065C; 353-U1443A; 353-U1444A; 354-U1450A; Asian Monsoon; Baltic Sea, Bornholm Basin; Baltic Sea, Kattegat; Baltic Sea, Landsort Deep; Baltic Sea, Lille Belt; Baltic Sea Paleoenvironment; Bengal Fan; BSB-1; BSB-3; BSB-7C; BSB-9; CDRILL; Center for Marine Environmental Sciences; Chikyu; CK06-06; Core drilling; DARCSEAS II; DEPTH, sediment/rock; Dipicolinic acid concentration per g dry weight; DRILL; Drilling/drill rig; Elevation of event; Event label; Exp301; Exp307; Exp308; Exp315; Exp316; Exp329; Exp346; Exp347; Exp353; EXP354; GC; GeoB15103-1; GeoB15104-2; GeoB15105-1; GeoB17302-4; GeoB17304-3; GeoB17306-2; GeoB17307-8; GeoB17308-4; Gravity corer; Greatship Manisha; Gulf of Mexico Hydrogeology; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Juan de Fuca Hydrogeology; Juan de Fuca Ridge, North Pacific Ocean; KN223; KN223_site12; KN223_site15; KN223_site3; Knorr; Latitude of event; Leg201; Longitude of event; M84/1; M84/1_119-1; M84/1_123-1; M84/1_126-1; MARUM; Meteor (1986); NanTroSEIZE Stage 1: Megasplay Riser Pilot; NanTroSEIZE Stage 1: Shallow Megaslay and Frontal Thrusts; Porcupine Basin Carbonate Mounds; POS450; POS450_576-4; POS450_580-3; POS450_585-3; POS450_586-1; POS450_587-1; Poseidon; Sample code/label; Sea of Japan/East Sea; South Pacific Gyre Microbiology; South Pacific Ocean; Western Mediterranean Sea  (1)
  • 201-1226B; 201-1226E; 201-1227A; 201-1227D; 201-1230A; 301-U1301C; 301-U1301D; Archaeal 16S rRNA gene copy number ratio; Archaeal 16S rRNA gene copy number ratio, standard deviation; CK06-06; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Exp301; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Juan de Fuca Hydrogeology; Juan de Fuca Ridge, North Pacific Ocean; Leg201; Ocean Drilling Program; ODP; Q-PCR, Power SYBR Green PCR Master Mix; SBH, slot-blot hybridization analysis; South Pacific Ocean  (1)
  • 301-U1301C; 301-U1301D; DRILL; Drilling/drill rig; Exp301; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Juan de Fuca Hydrogeology; Juan de Fuca Ridge, North Pacific Ocean  (1)
  • 370-C0023A; Alkenones (peak area); Chikyu; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diols (peak area); DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Exp370; High Performance Liquid Chromatography - Mass spectrometry (HPLC-MS); Hole A; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; IODP Expedition 370; J-CORES sample ID; Nankai Trough; Sample code/label; Sample ID; Site C0023  (1)
Document type
Keywords
Publisher
  • 1
    Publication Date: 2023-06-14
    Description: The dataset includes solid-phase geochemistry data of sediment cores from Site C0023 (Hole A) that was recovered during International Ocean Discovery Program (IODP) Expedition 370 in the Nankai Trough offshore Japan in the Pacific Ocean (Drilling vessel Chikyu). Site C0023 was established on 17 September 2016. Coring terminated on 3 November 2016. Algal lipid biomarker analysis was performed after Sturt et al. (2004) and HPLC-MS analyses after Becker et al. (2015). Biomarker concentrations are reported as the integrated peak area of the sum of all detected diols normalized to kg extracted sediment (PA/kg).
    Keywords: 370-C0023A; Alkenones (peak area); Chikyu; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diols (peak area); DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Exp370; High Performance Liquid Chromatography - Mass spectrometry (HPLC-MS); Hole A; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; IODP Expedition 370; J-CORES sample ID; Nankai Trough; Sample code/label; Sample ID; Site C0023
    Type: Dataset
    Format: text/tab-separated-values, 180 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2023-06-27
    Description: In deep subsurface sediments of the Juan de Fuca Ridge Flank, porewater acetate that is depleted in 13C relative to sedimentary organic matter indicates an acetogenic component to total acetate production. Thermodynamic calculations indicate common fermentation products or lignin monomers as potential substrates for acetogenesis. The classic autotrophic reaction may contribute as well, provided that dihydrogen (H2) concentrations are not drawn down to the thermodynamic thresholds of the energetically more favorable processes of sulfate reduction and methanogenesis. A high diversity of novel formyl tetrahydrofolate synthetase (fhs) genes throughout the upper half of the sediment column indicates the genetic potential for acetogenesis. Our results suggest that a substantial fraction of the acetate produced in marine sediment porewaters may derive from acetogenesis, in addition to the conventionally invoked sources fermentation and sulfate reduction.
    Keywords: 301-U1301C; 301-U1301D; DRILL; Drilling/drill rig; Exp301; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Juan de Fuca Hydrogeology; Juan de Fuca Ridge, North Pacific Ocean
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Lipp, Julius S; Morono, Yuki; Inagaki, Fumio; Hinrichs, Kai-Uwe (2008): Significant contribution of Archaea to extant biomass in marine subsurface sediments. Nature, 454(t207), 991-994, https://doi.org/10.1038/nature07174
    Publication Date: 2024-01-09
    Description: Deep drilling into the marine sea floor has uncovered a vast sedimentary ecosystem of microbial cells (Parkes et al., 1994, doi:10.1038/371410a0; D'Hondt et al., 2004, doi:10.1126/science.1101155). Extrapolation of direct counts of stained microbial cells to the total volume of habitable marine subsurface sediments suggests that between 56 Pg (Parkes et al., 1994, doi:10.1038/371410a0) and 303 Pg (Whitman et al., 1998) of cellular carbon could be stored in this largely unexplored habitat. From recent studies using various culture-independent techniques, no clear picture has yet emerged as to whether Archaea or Bacteria are more abundant in this extensive ecosystem (Schippers et al., doi:10.1038/nature03302; Inagaki et al., doi:10.1073/pnas.0511033103 ; Mauclaire et al., doi:10.1111/j.1472-4677.2004.00035.x; Biddle et al., doi:10.1073/pnas.0600035103). Here we show that in subsurface sediments buried deeper than 1 m in a wide range of oceanographic settings at least 87% of intact polar membrane lipids, biomarkers for the presence of live cells (Biddle et al., doi:10.1073/pnas.0600035103; Sturt et al., 2004, doi:10.1002/rcm.1378), are attributable to archaeal membranes, suggesting that Archaea constitute a major fraction of the biomass. Results obtained from modified quantitative polymerase chain reaction and slot-blot hybridization protocols support the lipid-based evidence and indicate that these techniques have previously underestimated archaeal biomass. The lipid concentrations are proportional to those of total organic carbon. On the basis of this relationship, we derived an independent estimate of amounts of cellular carbon in the global marine subsurface biosphere. Our estimate of 90 Pg of cellular carbon is consistent, within an order of magnitude, with previous estimates, and underscores the importance of marine subsurface habitats for global biomass budgets.
    Keywords: 201-1226B; 201-1226E; 201-1227A; 201-1227D; 201-1230A; 301-U1301C; 301-U1301D; Archaeal 16S rRNA gene copy number ratio; Archaeal 16S rRNA gene copy number ratio, standard deviation; CK06-06; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Exp301; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Juan de Fuca Hydrogeology; Juan de Fuca Ridge, North Pacific Ocean; Leg201; Ocean Drilling Program; ODP; Q-PCR, Power SYBR Green PCR Master Mix; SBH, slot-blot hybridization analysis; South Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 133 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Wörmer, Lars; Hoshino, Tatsuhiko; Bowles, Marshall W; Viehweger, Bernhard; Adhikari, Rishi Ram; Xiao, Nan; Uramoto, Goichiro; Könneke, Martin; Lazar, Cassandre Sara; Morono, Yuki; Inagaki, Fumio; Hinrichs, Kai-Uwe (2019): Microbial dormancy in the marine subsurface: Global endospore abundance and response to burial. Science Advances, 5(2), eaav1024, https://doi.org/10.1126/sciadv.aav1024
    Publication Date: 2024-06-26
    Description: Marine sediments host an unexpectedly large microbial biosphere, suggesting unique microbial mechanisms for surviving burial and slow metabolic turnover. Although dormancy is generally considered an important survival strategy, its specific role in subsurface sediments remains unclear. We quantified dormant bacterial endospores in 331 marine sediment samples from diverse depositional types and geographical origins. The abundance of endospores relative to vegetative cells increased with burial depth and endospores became dominant below 25 m, with an estimated population of 2.5 × 1028 to 1.9 × 1029 endospores in the uppermost kilometer of sediment and a corresponding biomass carbon of 4.6 to 35 Pg surpassing that of vegetative cells. Our data further identify distinct endospore subgroups with divergent resistance to burial and aging. Endospores may shape the deep biosphere by providing a core population for colonization of new habitats and/or through low-frequency germination to sustain slow growth in this environment.
    Keywords: 201-1226B; 201-1226D; 201-1226E; 201-1227A; 201-1227D; 201-1228A; 201-1228E; 201-1230A; 201-1230B; 201-1231A; 201-1231B; 201-1231E; 301-U1301C; 307-U1317A; 308-U1319A; 308-U1320A; 308-U1322B; 308-U1324B; 315-C0001E; 315-C0001F; 315-C0002D; 316-C0004C; 316-C0006C; 316-C0006D; 316-C0006E; 316-C0007A; 316-C0007B; 316-C0007C; 316-C0008A; 316-C0008C; 329-U1365C; 329-U1365D; 329-U1366F; 329-U1367D; 329-U1368D; 329-U1369E; 329-U1370F; 329-U1371E; 329-U1371F; 346-U1423A; 346-U1424A; 346-U1426A; 346-U1428A; 347-M0059E; 347-M0060B; 347-M0063E; 347-M0065C; 353-U1443A; 353-U1444A; 354-U1450A; Asian Monsoon; Baltic Sea, Bornholm Basin; Baltic Sea, Kattegat; Baltic Sea, Landsort Deep; Baltic Sea, Lille Belt; Baltic Sea Paleoenvironment; Bengal Fan; BSB-1; BSB-3; BSB-7C; BSB-9; CDRILL; Center for Marine Environmental Sciences; Chikyu; CK06-06; Core drilling; DARCSEAS II; DEPTH, sediment/rock; Dipicolinic acid concentration per g dry weight; DRILL; Drilling/drill rig; Elevation of event; Event label; Exp301; Exp307; Exp308; Exp315; Exp316; Exp329; Exp346; Exp347; Exp353; EXP354; GC; GeoB15103-1; GeoB15104-2; GeoB15105-1; GeoB17302-4; GeoB17304-3; GeoB17306-2; GeoB17307-8; GeoB17308-4; Gravity corer; Greatship Manisha; Gulf of Mexico Hydrogeology; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Juan de Fuca Hydrogeology; Juan de Fuca Ridge, North Pacific Ocean; KN223; KN223_site12; KN223_site15; KN223_site3; Knorr; Latitude of event; Leg201; Longitude of event; M84/1; M84/1_119-1; M84/1_123-1; M84/1_126-1; MARUM; Meteor (1986); NanTroSEIZE Stage 1: Megasplay Riser Pilot; NanTroSEIZE Stage 1: Shallow Megaslay and Frontal Thrusts; Porcupine Basin Carbonate Mounds; POS450; POS450_576-4; POS450_580-3; POS450_585-3; POS450_586-1; POS450_587-1; Poseidon; Sample code/label; Sea of Japan/East Sea; South Pacific Gyre Microbiology; South Pacific Ocean; Western Mediterranean Sea
    Type: Dataset
    Format: text/tab-separated-values, 551 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...