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  • Data  (12,437)
  • PANGAEA  (12,437)
  • American Institute of Physics (AIP)
  • 2015-2019  (12,437)
  • 2016  (12,437)
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  • 2015-2019  (12,437)
Year
  • 1
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Description: The upper air soundings are normally performed once a day to measure vertical profiles of air pressure, temperature, relative humidity and the wind vector. Helium filled balloons (TOTEX 600 g, 800 g) were used to carry Vaisala RS92-SGPW radiosondes. Whenever possible, the launches were performed about 10 UTC. Condensed measurements (TEMP Format FM-35) were transferred without delay into the Global Telecommunication System GTS were they contribute for the world wide weather forecasts. The profile data were taken every 5-10 seconds which result in a vertical profile resolution of about 25-50 meter. The profiles start at the helideck 10 m above sea level and terminate at the burst level of the balloons, normally at heights between 25 and 37 km.
    Keywords: AWI_Meteo; Meteorological Long-Term Observations @ AWI
    Type: Dataset
    Format: application/zip, 136 datasets
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  • 2
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    PANGAEA
    In:  Supplement to: Ramisch, Arne; Lockot, Gregori; Haberzettl, Torsten; Hartmann, Kai; Kuhn, Gerhard; Lehmkuhl, Frank; Schimpf, Stefan; Schulte, Philipp; Stauch, Georg; Wang, Rong; Wünnemann, Bernd; Yan, Dada; Zhang, Yongzhan; Diekmann, Bernhard (2016): A persistent northern boundary of Indian Summer Monsoon precipitation over Central Asia during the Holocene. Scientific Reports, 6, 25791, https://doi.org/10.1038/srep25791
    Publication Date: 2023-03-13
    Description: Extra-tropical circulation systems impede poleward moisture advection by the Indian Summer Monsoon. In this context, the Himalayan range is believed to insulate the south Asian circulation from extra-tropical influences and to delineate the northern extent of the Indian Summer Monsoon in central Asia. Paleoclimatic evidence, however, suggests increased moisture availability in the Early Holocene north of the Himalayan range which is attributed to an intensification of the Indian Summer Monsoon. Nevertheless, mechanisms leading to a surpassing of the Himalayan range and the northern maximum extent of summer monsoonal influence remain unknown. Here we show that the Kunlun barrier on the northern Tibetan Plateau [~36°N] delimits Indian Summer Monsoon precipitation during the Holocene. The presence of the barrier relocates the insulation effect 1,000 km further north, allowing a continental low intensity branch of the Indian Summer Monsoon which is persistent throughout the Holocene. Precipitation intensities at its northern extent seem to be driven by differentiated solar heating of the Northern Hemisphere indicating dependency on energy-gradients rather than absolute radiation intensities. The identified spatial constraints of monsoonal precipitation will facilitate the prediction of future monsoonal precipitation patterns in Central Asia under varying climatic conditions.
    Keywords: AWI_PerDyn; Permafrost Research (Periglacial Dynamics) @ AWI
    Type: Dataset
    Format: application/zip, 17 datasets
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  • 3
    Publication Date: 2023-03-14
    Keywords: Acidity; Alkalinity, total; Ammonium; AWI_PerDyn; AWI_POK-01; AWI Arctic Land Expedition; Bottom water temperature; Conductivity, electrolytic; DATE/TIME; Depth, bottom/max; DEPTH, water; Hardness description; Kytalyk-Pokhodsk_2012, Kolyma2012; Monitoring station; MONS; Nitrate; Oxygen; Permafrost Research (Periglacial Dynamics) @ AWI; pH; Phosphate; RU-Land_2012_Kytalyk_Kolyma; Sample code/label; Siberia, Russia; Temperature, air; Temperature, water; Thaw depth of active layer
    Type: Dataset
    Format: text/tab-separated-values, 126 data points
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  • 4
    Publication Date: 2023-03-14
    Keywords: AWI_PerDyn; AWI_Pi01; AWI_Pi02; AWI_Pi03; AWI_Pi04; AWI_Pi05; AWI_Pi06; AWI_Pi07; AWI_Pi08; AWI_Pi09; AWI_Pi10; AWI_Pi11; AWI_Pi12; AWI_Pi13; AWI_Pi14; AWI_PiL; AWI Arctic Land Expedition; DEPTH, soil; Depth, soil, maximum; Depth, soil, minimum; East Siberia; Event label; islet1; islet2.center; islet2.wall; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; pH; RU-Land_2012_Kytalyk_Kolyma; Sampling/measurement on land; Siberia, Russia; Soil horizon; Soil type
    Type: Dataset
    Format: text/tab-separated-values, 195 data points
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  • 5
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD-Acoustic Doppler Current Profiler; CTD-ADCP; CTD-ADCP_20140822; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 22440 data points
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  • 6
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD-Acoustic Doppler Current Profiler; CTD-ADCP; CTD-ADCP_20150828; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 46315 data points
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  • 7
    Publication Date: 2023-03-14
    Keywords: BIOACID; BIOACID 2 PNG2013; Biological Impacts of Ocean Acidification; DATE/TIME; DIVER; Environment; LATITUDE; Layer description; Location; LONGITUDE; M.V. Chertan; Number; Papua_New_Guinea_CO2_vent; pH; Sample code/label; Sample ID; Sampling by diver
    Type: Dataset
    Format: text/tab-separated-values, 112 data points
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  • 8
    Publication Date: 2023-03-14
    Keywords: Change; Darlington; DATE/TIME; EXP; Experiment; Oxygen saturation; pH; pH change; Replicate; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 168 data points
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  • 9
    Publication Date: 2023-03-14
    Keywords: Darlington; DATE/TIME; DEPTH, water; Event label; EXP; Experiment; Fortescue_Bay; Habitat; LATITUDE; LONGITUDE; Oxygen; pH; ph electrode; pHTempion; Replicate; Salinity; SeaPHOX; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 9497 data points
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  • 10
    Publication Date: 2023-03-13
    Keywords: AWI_PerDyn; AWI Arctic Land Expedition; Calculated; China2011,China2012/1,China2012/2,China2012/3; Cluster membership; CN-Land_2012; Date/Time of event; DEPTH, sediment/rock; Event label; HAND; HH-11154; HH-11163; HH-11192; HH-11199; HH-11211; HH-11278; HH-11285; HH-11286; HH-11287; HH-11316; HH-2012-08-20-001; HH-2012-08-20-003; HH-2012-08-20-004; HH-2012-08-20-005; HH-2012-08-20-006; HH-2012-08-20-007; HH-2012-08-20-008; HH-2012-08-20-010; HH-2012-08-20-011; HH-2012-08-20-012; HH-2012-08-20-013; HH-2012-08-20-014; HH-2012-08-20-016; HH-2012-08-20-017a; HH-2012-08-20-017b; HH-2012-08-20-018; HH-2012-08-20-019; HH-2012-08-20-020; HH-2012-08-20-021; HH-2012-08-20-022; HH-2012-08-20-023a; HH-2012-08-20-023b; HH-2012-08-20-024; HH-2012-08-20-025; HH-2012-08-20-029; HH-2012-08-21-001; HH-2012-08-21-002; HH-2012-08-21-004; HH-2012-08-21-006; HH-2012-08-21-007; HH-2012-08-21-008; HH-2012-08-21-009; HH-2012-08-23-001; HH-2012-08-23-004; HH-2012-08-23-006; HH-2012-08-23-007; HH-2012-08-23-008; HH-2012-08-23-009b; HH-2012-08-23-010; HH-2012-08-23-011; HH-2012-08-23-012; HH-9739; HH-9912; HH-9914; HH-9918; HH-9919; HH-9951; HH-9952; Lake Heihai, Qinghai, China; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; Sampling by hand
    Type: Dataset
    Format: text/tab-separated-values, 232 data points
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  • 11
    Publication Date: 2023-03-13
    Keywords: Chlorophyll total; CTD/Rosette; CTD-RO; Dana01/16; Dana01/16_103; Dana01/16_104; Dana01/16_105; Dana01/16_106; Dana01/16_113; Dana01/16_114; Dana01/16_117; Dana01/16_118; Dana01/16_119; Dana01/16_127; Dana01/16_128; Dana01/16_129; Dana01/16_137; Dana01/16_138; Dana01/16_139; Dana01/16_141; Dana01/16_142; Dana01/16_148; Dana01/16_149; Dana01/16_150; Dana01/16_151; Dana01/16_160; Dana01/16_161; Dana01/16_162; Dana01/16_163; Dana01/16_171; Dana01/16_172; Dana01/16_177; Dana01/16_178; Dana01/16_179; Dana01/16_180; Dana01/16_186; Dana01/16_187; Dana01/16_188; Dana01/16_189; Dana01/16_197; Dana01/16_198; Dana01/16_199; Dana01/16_200; Dana01/16_207; Dana01/16_208; Dana01/16_209; Dana01/16_210; Dana01/16_213; Dana01/16_214; Dana01/16_215; Dana01/16_216; Dana II; Date/Time of event; DEPTH, water; Elevation of event; Event label; International Young Fish Survey/International Bottom Trawl Survey; IYFS/IBTS; Kattegat; Latitude of event 2; Longitude of event; Nitrate; Nitrite; Nitrogen, total; Oxygen; Phosphate; Phosphorus, total; Pressure, water; Salinity; Silicate; Skagerrak; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2654 data points
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  • 12
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    PANGAEA
    Publication Date: 2023-03-13
    Keywords: CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; International Young Fish Survey/International Bottom Trawl Survey; IYFS/IBTS; Latitude of event; Longitude of event; North Sea; Norwegian Sea; Pressure, water; Salinity; Scotia; Scotia16/1; Scotia16/1_10; Scotia16/1_11; Scotia16/1_12; Scotia16/1_13; Scotia16/1_14; Scotia16/1_15; Scotia16/1_16; Scotia16/1_17; Scotia16/1_18; Scotia16/1_19; Scotia16/1_20; Scotia16/1_21; Scotia16/1_22; Scotia16/1_23; Scotia16/1_24; Scotia16/1_25; Scotia16/1_26; Scotia16/1_27; Scotia16/1_28; Scotia16/1_29; Scotia16/1_30; Scotia16/1_31; Scotia16/1_32; Scotia16/1_33; Scotia16/1_34; Scotia16/1_35; Scotia16/1_36; Scotia16/1_37; Scotia16/1_38; Scotia16/1_39; Scotia16/1_40; Scotia16/1_41; Scotia16/1_42; Scotia16/1_43; Scotia16/1_44; Scotia16/1_45; Scotia16/1_46; Scotia16/1_47; Scotia16/1_48; Scotia16/1_49; Scotia16/1_50; Scotia16/1_51; Scotia16/1_52; Scotia16/1_53; Scotia16/1_9; South Atlantic Ocean; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 2688 data points
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  • 13
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    PANGAEA
    In:  Supplement to: Putranto, Thomas Triadi; Rüde, Thomas (2016): Hydrogeological model of an urban city in a coastal area, case study: Semarang, Indonesia. Indonesian Journal on Geoscience, 3(1), 17-27, https://doi.org/10.17014/ijog.3.1.17-27
    Publication Date: 2023-03-14
    Description: In Semarang City, groundwater has been exploited as a natural resource since 1841. The groundwater exploited in deep wells is concentrated in confined aquifers. The previous hydrogeological model was developed in one unit of aquifer and refined then by using several hydrostratigraphical units following a regional hydrogeological map without any further analysis. At present, there is a lack of precise hydrogeological model which integrates geological and hydrogeological data, in particular for multiple aquifers in Semarang. Thus, the aim of this paper is to develop a hydrogeological model for the multiple aquifers in Semarang using an integrated data approach. Groundwater samples in the confined aquifers have been analyzed to define the water type and its lateral distribution. Two hydrogeological cross sections were then created based on several borelog data to define a hydrostratigraphical unit (HSU). The HSU result indicates the hydrogeological model of Semarang consists of two aquifers, three aquitards, and one aquiclude. Aquifer 1 is unconfined, while Aquifer 2 is confined. Aquifer 2 is classified into three groups (2a, 2b, and 2c) based on analyses of major ion content and hydrostratigraphical cross sections.
    Keywords: Aquifer type; Area/locality; Balance; Bicarbonate ion; Calcium; Calculated; Chloride; Conductivity, electrical; DATE/TIME; Depth, well; ELEVATION; Event label; Facies name/code; Handheld GPS, Garmin; Java Island, northern coast; Latitude of event; Longitude of event; Magnesium; N_1; N_2; N_3; N_7; pH; Portable water detector; Portable water quality meter (Hanna Instruments); Potassium; Sample position; Sampling Well; SB_100; SB_112; SB_120; SB_176; SB_185; SB_189; SB_190; SB_198; SB_206; SB_210; SB_211; SB_213; SB_214; SB_215; SB_217; SB_219; SB_220; SB_225; SB_226; SB_235; SB_256; SB_262; SB_265; SB_270; SB_271; SB_273; SB_278; SB_281; SB_282; SB_283; SB_297; SB_299; SB_321; SB_325; SB_33; SB_332; SB_344; SB_347; SB_348; SB_36; SB_590; SB_60; SB_726; SB_758; SB_790; SB_793; SB_92; SB_951; Sodium; SP_136; SP_138; SP_139; SP_341; SP_342; SP_764; Spectrophotometric; Sulfate; Total dissolved solids; UTM Easting, Universal Transverse Mercator; UTM Northing, Universal Transverse Mercator; UTM Zone, Universal Transverse Mercator; Water level; WELL
    Type: Dataset
    Format: text/tab-separated-values, 1131 data points
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  • 14
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    PANGAEA
    In:  Alfred Wegener Institute - Research Unit Potsdam
    Publication Date: 2023-03-14
    Keywords: 06-CYak-01; 06-CYak-02; 06-CYak-03; 06-CYak-04; 06-CYak-05; 06-NYak-01; 06-NYak-02; 06-NYak-03; 06-NYak-04; 06-NYak-05; 06-NYak-06; 06-NYak-07; 06-NYak-08; 06-NYak-09; 06-NYak-10; 06-NYak-11; 06-NYak-12; 06-NYak-13; 06-NYak-14; 06-NYak-15; Alaas; AWI_PerDyn; AWI Arctic Land Expedition; Ayan; Central Yakutia, Russia; Chat; Comment of event; Conductivity; Date/Time of event; Depth of Secchi Disk; Dulla; Etektyak; Event label; Ilimniir; Ivanovka; Kerdugen; Ketitiki; Krestyak; Latitude of event; Longitude of event; MULT; Multiple investigations; Nami-Kuel; North_Yakutia_2006; North Yakutia, Russia; Oibon-Kuel; Oloror; Oppoyao; Optional event label; Otto; Oxygen; Oxygen saturation; Permafrost Research (Periglacial Dynamics) @ AWI; pH; RU-Land_2006_Yakutia; Spasskoe; Suturuoka; Temperature, water; Thee-Bihii; Timpi; Ushepes
    Type: Dataset
    Format: text/tab-separated-values, 120 data points
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  • 15
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    PANGAEA
    In:  Alfred Wegener Institute - Research Unit Potsdam
    Publication Date: 2023-03-14
    Keywords: 09-TIK-01; 09-TIK-02; 09-TIK-03; 09-TIK-04; 09-TIK-05; 09-TIK-08; 09-TIK-09; 09-TIK-10; 09-TIK-11; 09-TIK-12; 09-TIK-13; 09-TIK-14; Alkalinity, total; AWI_PerDyn; AWI Arctic Land Expedition; Byluyng Kjuel; Comment of event; Conductivity; Date/Time of event; Depth of Secchi Disk; Elgene Kjuel; Event label; Latitude of event; Longitude of event; MULT; Multiple investigations; Permafrost Research (Periglacial Dynamics) @ AWI; pH; RU-Land_2009_Lena-transect; Tiksi2009; Vegetation type
    Type: Dataset
    Format: text/tab-separated-values, 52 data points
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  • 16
    Publication Date: 2023-03-14
    Keywords: 90BYBA40; 90BYBA40-track; Chlorophyll a; Chlorophyll b; Chlorophyll c; CT; Dalniye Zelentsy; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 7172 data points
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  • 17
    Publication Date: 2023-03-14
    Keywords: 90PD9E40; 90PD9E40-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Professor Deryugin; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 4574 data points
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  • 18
    Publication Date: 2023-03-14
    Keywords: 90DI9D20; 90DI9D20-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; Diana; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1941 data points
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  • 19
    Publication Date: 2023-03-14
    Keywords: 90PD9F70; 90PD9F70-track; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Professor Deryugin; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 380 data points
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  • 20
    Publication Date: 2023-03-14
    Keywords: 90PD9F50; 90PD9F50-track; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Professor Deryugin; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1018 data points
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  • 21
    Publication Date: 2023-03-14
    Keywords: 90PD9F80; 90PD9F80-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Professor Deryugin; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 9627 data points
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  • 22
    Publication Date: 2023-03-14
    Keywords: 90SBC810; 90SBC810-track; Ammonium; Coastal station Kola Bay; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Nitrogen, total; pH; Phosphate; Phosphorus, total; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 2939 data points
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  • 23
    Publication Date: 2023-03-14
    Keywords: 90XX9BA0; 90XX9BA0-track; Alkalinity, total; CT; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 282 data points
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  • 24
    Publication Date: 2023-03-14
    Keywords: 90XX9C20; 90XX9C20-track; Alkalinity, total; CT; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 283 data points
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  • 25
    Publication Date: 2023-03-14
    Keywords: 34AR9D7A; 34AR9D7A-track; Alkalinity, total; Ammonium; Aranda (1953); CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; pH; Phosphate; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 5073 data points
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  • 26
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    PANGAEA
    In:  Supplement to: Endres, Sonja; Galgani, Luisa; Riebesell, Ulf; Schulz, Kai Georg; Engel, Anja (2014): Stimulated Bacterial Growth under Elevated pCO2: Results from an Off-Shore Mesocosm Study. PLoS ONE, 9(6), e99228, https://doi.org/10.1371/journal.pone.0099228
    Publication Date: 2023-03-14
    Description: Marine bacteria are the main consumers of freshly produced organic matter. Many enzymatic processes involved in the bacterial digestion of organic compounds were shown to be pH sensitive in previous studies. Due to the continuous rise in atmospheric CO2 concentration, seawater pH is presently decreasing at a rate unprecedented during the last 300 million years but the consequences for microbial physiology, organic matter cycling and marine biogeochemistry are still unresolved. We studied the effects of elevated seawater pCO2 on a natural plankton community during a large-scale mesocosm study in a Norwegian fjord. Nine Kiel Off-Shore Mesocosms for Future Ocean Simulations (KOSMOS) were adjusted to different pCO2 levels ranging initially from ca. 280 to 3000 µatm and sampled every second day for 34 days. The first phytoplankton bloom developed around day 5. On day 14, inorganic nutrients were added to the enclosed, nutrient-poor waters to stimulate a second phytoplankton bloom, which occurred around day 20. Our results indicate that marine bacteria benefit directly and indirectly from decreasing seawater pH. During the first phytoplankton bloom, 5-10% more transparent exopolymer particles were formed in the high pCO2 mesocosms. Simultaneously, the efficiency of the protein-degrading enzyme leucine aminopeptidase increased with decreasing pH resulting in up to three times higher values in the highest pCO2/lowest pH mesocosm compared to the controls. In general, total and cell-specific aminopeptidase activities were elevated under low pH conditions. The combination of enhanced enzymatic hydrolysis of organic matter and increased availability of gel particles as substrate supported up to 28% higher bacterial abundance in the high pCO2 treatments. We conclude that ocean acidification has the potential to stimulate the bacterial community and facilitate the microbial recycling of freshly produced organic matter, thus strengthening the role of the microbial loop in the surface ocean.
    Keywords: Abundance per volume; BIOACID; Biological Impacts of Ocean Acidification; Chlorophyll a; DATE/TIME; Day of experiment; KOSMOS_2011_Bergen; Leucine aminopeptidase activity; MESO; Mesocosm experiment; pH; Raunefjord; Sample code/label; Transparent exopolymer particles as Gum Xanthan equivalents per volume; Transparent exopolymer particles as Gum Xanthan equivalents per volume, std dev
    Type: Dataset
    Format: text/tab-separated-values, 2053 data points
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  • 27
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120822_St1; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 23155 data points
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  • 28
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120822_St3; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 9960 data points
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  • 29
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120828_St1; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 12530 data points
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  • 30
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD-Acoustic Doppler Current Profiler; CTD-ADCP; CTD-ADCP_20130904; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 31030 data points
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  • 31
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120828_St4; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 1635 data points
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  • 32
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Aragonite saturation state; Bicarbonate ion; BIOACID; Biological Impacts of Ocean Acidification; Carbon, inorganic, dissolved; Carbonate ion; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Ratio; Salinity; Sample code/label; Standard deviation; Temperature, water; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 506 data points
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  • 33
    Publication Date: 2023-03-14
    Keywords: Acidity; Alkalinity, total; Ammonium; Area/locality; AWI_PerDyn; AWI_POK-02; AWI_POK-03; AWI_POK-04; AWI_POK-05; AWI_POK-06; AWI_POK-07; AWI_POK-08; AWI_POK-09; AWI_POK-10; AWI_POK-11; AWI_POK-12; AWI_POK-13; AWI_POK-14; AWI_POK-15; AWI_POK-16; AWI_POK-17; AWI_POK-18; AWI_POK-19; AWI_POK-20; AWI_POK-21; AWI_POK-22; AWI_POK-23; AWI_POK-24; AWI_POK-25; AWI_POK-26; AWI_POK-27; AWI_POK-28; AWI_POK-29; AWI_POK-30; AWI_POK-31; AWI Arctic Land Expedition; Bottom water temperature; Comment; Conductivity, electrolytic; DATE/TIME; Depth, bottom/max; Event label; Hardness description; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Latitude of event; Longitude of event; Nitrate; Oxygen; Permafrost Research (Periglacial Dynamics) @ AWI; pH; Phosphate; RU-Land_2012_Kytalyk_Kolyma; Sampling/measurement on land; Siberia, Russia; Size; Temperature, air; Temperature, water; Type
    Type: Dataset
    Format: text/tab-separated-values, 445 data points
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  • 34
    Publication Date: 2023-03-14
    Keywords: AWI_PerDyn; AWI Arctic Land Expedition; Conductivity, electrolytic; DEPTH, sediment/rock; Description; Distance; East Siberia; Height; Ice content; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Permafrost Research (Periglacial Dynamics) @ AWI; pH; pingo_exposure; RU-Land_2012_Kytalyk_Kolyma; Sample code/label; Sample type; Sampling/measurement on land; Shirokovsky_Kholm
    Type: Dataset
    Format: text/tab-separated-values, 437 data points
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  • 35
    Publication Date: 2023-03-14
    Keywords: AWI_L-24; AWI_L-25; AWI_L-31; AWI_L-34; AWI_L-36; AWI_L-38; AWI_L-6; AWI_L-62; AWI_L-66; AWI_L-80; AWI_PerDyn; AWI Arctic Land Expedition; Conductivity, electrical; DATE/TIME; DEPTH, water; Event label; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; pH; RU-Land_2012_Kytalyk_Kolyma; Sample code/label; Sampling/measurement on land; Siberia, Russia
    Type: Dataset
    Format: text/tab-separated-values, 70 data points
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  • 36
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120822_St2; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 19395 data points
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  • 37
    Publication Date: 2023-03-14
    Keywords: Conductivity; CTD_20120828_St2; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Fluorescence; Salinity; Temperature, water; Tyrrhenian Sea
    Type: Dataset
    Format: text/tab-separated-values, 10530 data points
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  • 38
    Publication Date: 2023-03-14
    Keywords: 9038B970; 9038B970-track; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Pomor; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1000 data points
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  • 39
    Publication Date: 2023-03-14
    Keywords: 90BYB8C0; 90BYB8C0-track; CT; Dalniye Zelentsy; DATE/TIME; Depth, bathymetric; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Nitrogen, total; Oxygen; Oxygen saturation; pH; Phosphate; Phosphorus, total; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1307 data points
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  • 40
    Publication Date: 2023-03-14
    Keywords: 90BYBA60; 90BYBA60-track; Chlorophyll a; Chlorophyll b; Chlorophyll c; CT; Dalniye Zelentsy; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Nitrate; Nitrite; Nitrogen, total; Oxygen; Oxygen saturation; pH; Phosphate; Phosphorus, total; Salinity; Silicate; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1687 data points
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  • 41
    Publication Date: 2023-03-14
    Keywords: 90DI9CA0; 90DI9CA0-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; Diana; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1181 data points
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  • 42
    Publication Date: 2023-03-14
    Keywords: 90DI9D10; 90DI9D10-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; Diana; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 929 data points
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  • 43
    Publication Date: 2023-03-14
    Keywords: 90DI9CB0; 90DI9CB0-track; Alkalinity, total; CT; DATE/TIME; Depth, bathymetric; DEPTH, water; Diana; LATITUDE; LONGITUDE; Nitrate; Nitrite; Oxygen; Oxygen saturation; pH; Phosphate; Salinity; Station label; Temperature, water; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1623 data points
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  • 44
    Publication Date: 2023-03-16
    Keywords: DATE/TIME; Dive, duration; Dive, time depth profile; FIL2014; FIL2014_wed_a_f_06; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Polarstern; PS82; Southern Ocean - Atlantic Sector; wd06-07-13
    Type: Dataset
    Format: text/tab-separated-values, 73203 data points
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  • 45
    Publication Date: 2023-03-16
    Keywords: DATE/TIME; Dive, duration; Dive, time depth profile; FIL2014; FIL2014_wed_a_m_03; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Polarstern; PS82; Southern Ocean - Atlantic Sector; wd06-03-13
    Type: Dataset
    Format: text/tab-separated-values, 26429 data points
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  • 46
    Publication Date: 2023-03-16
    Keywords: DATE/TIME; Dive, duration; Dive, time depth profile; FIL2014; FIL2014_wed_a_f_01; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Polarstern; PS82; Southern Ocean - Atlantic Sector; wd06-01-13
    Type: Dataset
    Format: text/tab-separated-values, 41145 data points
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  • 47
    Publication Date: 2023-03-16
    Keywords: DATE/TIME; Dive, duration; Dive, time depth profile; FIL2014; FIL2014_wed_a_f_05; LATITUDE; LONGITUDE; Marine endotherm; Marine Mammal Tracking; MET; MMT; Polarstern; PS82; Southern Ocean - Atlantic Sector; wd06-05-13
    Type: Dataset
    Format: text/tab-separated-values, 18369 data points
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  • 48
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: AWI_PhyOce; CT; DATE/TIME; DEPTH, water; HE312/1; HE312/1-track; Heincke; LATITUDE; LONGITUDE; Physical Oceanography @ AWI; Salinity; Temperature, water; Thermosalinograph; TSG; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 2834 data points
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  • 49
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Type: Dataset
    Format: application/zip, 1.6 GBytes
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  • 50
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    PANGAEA
    In:  Instituto Antártico Argentino, Buenos Aires, Argentina
    Publication Date: 2023-03-16
    Keywords: Carlini_Base_C1; Carlini/Jubany Station; DATE/TIME; IMCOAST/IMCONet; Impact of climate induced glacier melt on marine coastal systems, Antarctica; Jubany; Jubany_Station_C1; Potter Cove, King George Island, Antarctic Peninsula; Research station; RS; Uniform resource locator/link to image; Uniform resource locator/link to thumbnail
    Type: Dataset
    Format: text/tab-separated-values, 1798 data points
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  • 51
    Publication Date: 2023-03-16
    Keywords: Carlini_Base_C2; Carlini/Jubany Station; DATE/TIME; IMCOAST/IMCONet; Impact of climate induced glacier melt on marine coastal systems, Antarctica; Jubany; Jubany_Station_C2; Potter Cove, King George Island, Antarctic Peninsula; Research station; RS; Uniform resource locator/link to image; Uniform resource locator/link to thumbnail
    Type: Dataset
    Format: text/tab-separated-values, 1372 data points
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  • 52
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: Additives; Atipamezol; Comment; DATE/TIME; Doxapram; DRE2015; DRE2015_wed_a_f_01; DRE2015_wed_a_f_02; DRE2015_wed_a_f_03; DRE2015_wed_a_f_05; DRE2015_wed_a_f_07; DRE2015_wed_a_f_08; DRE2015_wed_a_f_09; DRE2015_wed_a_f_11; DRE2015_wed_a_m_04; DRE2015_wed_a_m_06; DRE2015_wed_a_m_10; Estimated; Event label; Girth, standard; Injection; Ketamine; Latitude of event; Length, standard; Longitude of event; Marine endotherm; Marine Mammal Tracking; Mass; MET; MMT; NEUMAYER III; Physical restraint; Premedication; Ruler tape; Sample code/label; SEADI, PS96; Southern Ocean - Atlantic Sector; Species code; Time of day; Xylazine
    Type: Dataset
    Format: text/tab-separated-values, 222 data points
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  • 53
    Publication Date: 2023-03-17
    Keywords: Conductivity; CTD, Sea-Bird; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Event label; ICBM_Ot_1603_01; ICBM_Ot_1603_02; ICBM_Ot_1603_03; ICBM_Ot_1603_04; ICBM_Ot_1603_05; ICBM_Ot_1603_06; ICBM_Ot_1603_07; ICBM_Ot_1603_08; ICBM_Ot_1603_09; ICBM_Ot_1603_10; ICBM_Ot_1603_11; ICBM_Ot_1603_12; ICBM_Ot_1603_13; ICBM_Ot_1603_14; Jade Bay; Latitude of event; Longitude of event; Pressure, water; Salinity; Temperature, water; Temperature, water, potential
    Type: Dataset
    Format: text/tab-separated-values, 5712 data points
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  • 54
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: ARK-XIII/2; Calculated; Course; CT; DATE/TIME; LATITUDE; LONGITUDE; Polarstern; PS44; PS44/2-track; Speed; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 14110 data points
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  • 55
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: ARK-XV/2; Calculated; Course; CT; DATE/TIME; LATITUDE; LONGITUDE; Polarstern; PS55; PS55/2-track; Speed; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 14320 data points
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  • 56
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: ARK-XIV/1b; Calculated; Course; CT; DATE/TIME; LATITUDE; LONGITUDE; Polarstern; PS51/1b-track; PS51 Transdrift-V; Speed; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 6336 data points
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  • 57
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: ARK-XXVIII/3 AURORA; AWI_PhyOce; CT; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Physical Oceanography @ AWI; Polarstern; PS86; PS86-track; Salinity; Temperature, water; Thermosalinograph; TSG; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 3866 data points
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  • 58
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    PANGAEA
    In:  Supplement to: Kottmeier, Dorothee; Rokitta, Sebastian D; Rost, Björn (2016): Acidification, not carbonation, is the major regulator of carbon fluxes in the coccolithophore Emiliania huxleyi. New Phytologist, 211(1), 126-137, https://doi.org/10.1111/nph.13885
    Publication Date: 2023-03-16
    Description: - A combined increase in seawater [CO2] and [H+] was recently shown to induce a shift from photosynthetic HCO3- to CO2 uptake in Emiliania huxleyi. This shift occurred within minutes, whereas acclimation to ocean acidification (OA) did not affect the carbon source. - To identify the driver of this shift, we exposed low- and high-light acclimated E. huxleyi to a matrix of two levels of dissolved inorganic carbon (1400, 2800 lmol kg-1) and pH (8.15, 7.85) and directly measured cellular O2, CO2 and HCO3 fluxes under these conditions. - Exposure to increased [CO2] had little effect on the photosynthetic fluxes, whereas increased [H+] led to a significant decline in HCO3- uptake. Low-light acclimated cells overcompensated for the inhibition of HCO3- uptake by increasing CO2 uptake. High-light acclimated cells, relying on higher proportions of HCO3- uptake, could not increase CO2 uptake and photosynthetic O2 evolution consequently became carbon-limited. - These regulations indicate that OA responses in photosynthesis are caused by [H+] rather than by [CO2]. The impaired HCO3- uptake also provides a mechanistic explanation for lowered calcification under OA. Moreover, it explains the OA-dependent decrease in photosynthesis observed in high-light grown phytoplankton.
    Keywords: AWI_Phytochange; Phytochange @ AWI
    Type: Dataset
    Format: application/zip, 16.7 kBytes
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  • 59
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven | Supplement to: Wang, Qiang; Danilov, Sergey; Jung, Thomas; Kaleschke, Lars; Wernecke, Andreas (2016): Sea ice leads in the Arctic Ocean: Model assessment, interannual variability and trends. Geophysical Research Letters, 43(13), 7019-7027, https://doi.org/10.1002/2016GL068696
    Publication Date: 2023-03-16
    Description: Northern Hemisphere sea ice from a Finite-Element Sea-Ice Ocean Model (FESOM) 4.5 km resolution simulation carried out by researchers from Alfred Wegener Institute (AWI), Germany. Concentration is shown with color; thickness is shown with shading. A global 1 degree mesh is used, with the "Arctic Ocean" locally refined to 4.5 km. South of CAA and Fram Strait the resolution is not refined in this simulation. The animation indicates that the 4.5 km model resolution helps to represent the small scale sea ice features, although much higher resolution is required to fully resolve the ice leads. The animation is created by Michael Böttinger from DKRZ (https://www.dkrz.de).
    Keywords: Arctic; DATE/TIME; File content; File format; File size; pan-Arctic; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 60
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Description: Recordings from the PerenniAL Acoustic Observatory in the Antarctic ocean (PALAOA) show seasonal acoustic presence of 4 Antarctic ice-breeding seal species (Ross seal, Ommatophoca rossii, Weddell seal, Leptonychotes weddellii, crabeater, Lobodon carcinophaga, and leopard seal, Hydrurga leptonyx). Apart from Weddell seals, inhabiting the fast-ice in Atka Bay, the other three (pack-ice) species however have to date never (Ross and leopard seal) or only very rarely (crabeater seals) been sighted in the Atka Bay region. The aim of the PASATA project is twofold: the large passive acoustic hydrophone array (hereafter referred to as large array) aims to localize calling pack-ice pinniped species to obtain information on their location and hence the ice habitat they occupy. This large array consists of four autonomous passive acoustic recorders with a hydrophone sensor deployed through a drilled hole in the sea ice. The PASATA recordings are time-stamped and can therefore be coupled to the PALAOA recordings so that the hydrophone array spans the bay almost entirely from east to west. The second, smaller hydrophone array (hereafter referred to as small array), also consists of four autonomous passive acoustic recorders with hydrophone sensors deployed through drilled holes in the sea ice. The smaller array was deployed within a Weddell seal breeding colony, located further south in the bay, just off the ice shelf. Male Weddell seals are thought to defend underwater territories around or near tide cracks and breathing holes used by females. Vocal activity increases strongly during the breeding season and vocalizations are thought to be used underwater by males for the purpose of territorial defense and advertisement. With the smaller hydrophone array we aim to investigate underwater behaviour of vocalizing male and female Weddell seals to provide further information on underwater movement patterns in relation to the location of tide cracks and breathing holes. As a pilot project, one on-ice and three underwater camera systems have been deployed near breathing holes to obtain additional visual information on Weddell seal behavioural activity. Upon each visit in the breeding colony, a census of colony composition on the ice (number of animals, sex, presence of dependent pups, presence and severity of injuries-indicative of competition intensity) as well as GPS readings of breathing holes and positions of hauled out Weddell seals are taken.
    Keywords: Atka Bay; File name; File size; File type; PASATA; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 46774 data points
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  • 61
    Publication Date: 2023-03-16
    Keywords: Bremerhaven_LloydWerft; Bremerhaven, Germany; DATE/TIME; File name; File size; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 62
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: ARK-XXIX/2.2; AWI_PhyOce; CT; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Physical Oceanography @ AWI; Polarstern; PS93.2; PS93.2-track; Salinity; Temperature, water; Thermosalinograph; TSG; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 3482 data points
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  • 63
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: Calculated; Course; CT; DATE/TIME; HE352/1; HE352/1-track; Heincke; LATITUDE; LONGITUDE; Speed; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 1656 data points
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  • 64
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: AWI_PhyOce; CT; DATE/TIME; DEPTH, water; HE439; HE439-track; Heincke; LATITUDE; LONGITUDE; North Sea; Physical Oceanography @ AWI; Salinity; Thermosalinograph; TSG; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 2256 data points
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  • 65
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: AWI_Meteo; Bremerhaven_LloydWerft; Bremerhaven, Germany; DATE/TIME; File name; Laser ceilometer, Vaisala, CL51; Meteorological Long-Term Observations @ AWI; Uniform resource locator/link to raw data file
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
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  • 66
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; SO213/2; SO213/2_83-1TC; Sonne; SOPATRA; South Pacific Ocean; TC; Trigger corer
    Type: Dataset
    Format: unknown
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  • 67
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    PANGAEA
    In:  Supplement to: Hoffmann, Katy; Hassenrück, Christiane; Salman-Carvalho, Verena; Holtappels, Moritz; Bienhold, Christina (2017): Response of bacterial communities to different detritus compositions in Arctic deep-sea sediments. Frontiers in Microbiology, 8, 266, https://doi.org/10.3389/fmicb.2017.00266
    Publication Date: 2023-03-16
    Description: In a multidisciplinary ex situ experiment, benthic bacterial deep-sea communities from 2,500 m water depth at the Long-Term Ecological Research Observatory HAUSGARTEN (stationPS93/050-5 and 6), were retrieved using a TV-guided multiple corer. Surface sediments (0 - 2 cm) of 16 cores were mixed with sterile filtered deep-sea water to a final sediment dilution of 3.5 fold. The slurries were split and supplemented with five different types of habitat-related detritus: chitin, as the most abundant biopolymer in the oceans, and four different naturally occurring Arctic algae species, i.e. Thalassiosira weissflogii, Emiliania huxleyi, Bacillaria sp. and Melosira arctica. Incubations were performed in five replicates, at in situ temperature and at atmospheric pressure, as well as at in situ pressure of 250 atm. At the start of the incubation and after 23 days, changes in key community functions, i.e. extracellular enzymatic activity, oxygen respiration and secondary production of biomass (bacterial cell numbers and biomass), were assessed along with changes in the bacterial community composition based on 16S rRNA gene and 16S rRNA Illumina sequencing. In summary, differences in community structure and in the uptake and remineralization of carbon in the different treatments suggest an effect of organic matter quality on bacterial diversity as well as on carbon turnover at the seafloor.
    Keywords: ABYSS; Accession number, genetics; ARK-XXIX/2.2; Assessment of bacterial life and matter cycling in deep-sea surface sediments; beta-glucosidase activity; Cell counts, standard deviation; Chitobiase activity; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; HG_IV; Incubation duration; Multicorer with television; North Greenland Sea; Oxygen; Polarstern; Pressure; Prokaryotes, abundance as single cells; PS93/050-5/6; PS93.2; Replicates; Respiration rate, oxygen, sediment; Sample type; Station label; Treatment; TVMUC
    Type: Dataset
    Format: text/tab-separated-values, 1540 data points
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  • 68
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: Acoustic Doppler Current Profiling (ADCP), TRDI Ocean Surveyor, 153.6 kHz; ARK-XXX/2, GN05; AWI_PhyOce; CT; File content; File name; Physical Oceanography @ AWI; Polarstern; PS100; PS100-track; Underway cruise track measurements; Uniform resource locator/link to raw data file
    Type: Dataset
    Format: text/tab-separated-values, 33 data points
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  • 69
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    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: ARK-XXX/2, GN05; AWI_Meteo; CT; DATE/TIME; File name; Laser ceilometer, Vaisala, CL51; LATITUDE; LONGITUDE; Meteorological Long-Term Observations @ AWI; Polarstern; PS100; PS100-track; Underway cruise track measurements; Uniform resource locator/link to raw data file
    Type: Dataset
    Format: text/tab-separated-values, 106 data points
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  • 70
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Type: Dataset
    Format: application/zip, 2.9 MBytes
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  • 71
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: Acoustic Doppler Current Profiling (ADCP), TRDI Ocean Surveyor, 153.6 kHz; ARK-XXIX/2.2; AWI_PhyOce; CT; File content; File name; Physical Oceanography @ AWI; Polarstern; PS93.2; PS93.2-track; Underway cruise track measurements; Uniform resource locator/link to raw data file
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
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  • 72
    Publication Date: 2023-03-09
    Description: The dispersal of larvae and their settlement to suitable habitat is fundamental to the replenishment of marine populations and the communities in which they live. Sound plays an important role in this process because for larvae of various species, it acts as an orientational cue towards suitable settlement habitat. Because marine sounds are largely of biological origin, they not only carry information about the location of potential habitat, but also information about the quality of habitat. While ocean acidification is known to affect a wide range of marine organisms and processes, its effect on marine soundscapes and its reception by navigating oceanic larvae remains unknown. Here, we show that ocean acidification causes a switch in role of present-day soundscapes from attractor to repellent in the auditory preferences in a temperate larval fish. Using natural CO2 vents as analogues of future ocean conditions, we further reveal that ocean acidification can impact marine soundscapes by profoundly diminishing their biological sound production. An altered soundscape poorer in biological cues indirectly penalizes oceanic larvae at settlement stage because both control and CO2-treated fish larvae showed lack of any response to such future soundscapes. These indirect and direct effects of ocean acidification put at risk the complex processes of larval dispersal and settlement.
    Keywords: Animalia; Argyrosomus japonicus; Behaviour; Chordata; CO2 vent; Coast and continental shelf; Containers and aquaria (20-1000 L or 〈 1 m**2); Entire community; Field observation; Growth/Morphology; Laboratory experiment; Nekton; OA-ICC; Ocean Acidification International Coordination Centre; Pelagos; Single species; South Pacific; Temperate
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 73
    Publication Date: 2023-03-09
    Description: Soundscapes are multidimensional spaces that carry meaningful information for many species about the location and quality of nearby and distant resources. Because soundscapes are the sum of the acoustic signals produced by individual organisms and their interactions, they can be used as a proxy for the condition of whole ecosystems and their occupants. Ocean acidification resulting from anthropogenic CO2 emissions is known to have profound effects on marine life. However, despite the increasingly recognized ecological importance of soundscapes, there is no empirical test of whether ocean acidification can affect biological sound production. Using field recordings obtained from three geographically separated natural CO2 vents, we show that forecasted end-of-century ocean acidification conditions can profoundly reduce the biological sound level and frequency of snapping shrimp snaps. Snapping shrimp were among the noisiest marine organisms and the suppression of their sound production at vents was responsible for the vast majority of the soundscape alteration observed. To assess mechanisms that could account for these observations, we tested whether long-term exposure (two to three months) to elevated CO2 induced a similar reduction in the snapping behaviour (loudness and frequency) of snapping shrimp. The results indicated that the soniferous behaviour of these animals was substantially reduced in both frequency (snaps per minute) and sound level of snaps produced. As coastal marine soundscapes are dominated by biological sounds produced by snapping shrimp, the observed suppression of this component of soundscapes could have important and possibly pervasive ecological consequences for organisms that use soundscapes as a source of information. This trend towards silence could be of particular importance for those species whose larval stages use sound for orientation towards settlement habitats.
    Keywords: Alpheus novaezealandiae; Animalia; Arthropoda; Benthic animals; Benthos; CO2 vent; Coast and continental shelf; Containers and aquaria (20-1000 L or 〈 1 m**2); Field observation; Laboratory experiment; Mediterranean Sea; OA-ICC; Ocean Acidification International Coordination Centre; Single species; South Pacific; Temperate
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 74
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    PANGAEA
    In:  Supplement to: Niemeyer, Bastian; Epp, Laura Saskia; Stoof-Leichsenring, Kathleen Rosmarie; Pestryakova, Luidmila A; Herzschuh, Ulrike (2017): A comparison of sedimentary DNA and pollen from lake sediments in recording vegetation composition at the Siberian treeline. Molecular Ecology Resources, 17(6), e46-e62, https://doi.org/10.1111/1755-0998.12689
    Publication Date: 2023-03-07
    Description: Reliable information of past vegetation changes are important to project future changes, especially for areas undergoing rapid transitioning such as the boreal treeline. The application of detailed sedDNA records has the potential to enhance our understanding of vegetation changes gained mainly from pollen studies of lake sediments. This study investigates sedDNA and pollen records from 31 lakes along a gradient of increasing larch forest cover in northern Siberia (Taymyr Peninsula) and compares them with vegetation field surveys within the lake's catchment. With respect to vegetation richness, sedDNA recorded 114 taxa, about half of them to species level, while pollen analyses identified 43 pollen taxa. Both approaches exceed the 31 taxa revealed by vegetation field surveys of 400 m**2 plots. From north to south, Larix percentages increase, as is consistently recorded by all three methods. Furthermore, tundra sites are separated from forested sites in the plots of the principal component analyses. Comparison of ordination results by Procrustes and Protest analyses yields a significant fit among all compared pairs of records. Despite the overall comparability of sedDNA and pollen analyses certain idiosyncrasies in the compositional signal are observed, such as high percentages of Alnus and Betula in all pollen spectra and high percentages of Salix in all sedDNA spectra. In conclusion, our results from the treeline show that sedDNA analyses perform better than pollen in recording site-specific richness (i.e. presence/absence of certain vegetation taxa in the direct vicinity of the lake) and perform as good as pollen in tracing regional vegetation composition.
    Keywords: AWI_PerDyn; Permafrost Research (Periglacial Dynamics) @ AWI
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 75
    Publication Date: 2023-03-07
    Keywords: 12-P-0708-1; AWI_12P-1008-1; AWI_12P-1607-1; AWI_12P-1707-1; AWI_12P-1907-1; AWI_12P-1907-2; AWI_12P-2007-1; AWI_12P-2007-2; AWI_12P-2007-3; AWI_12P-2007-4; AWI_12P-2107-1; AWI_12P-2107-2; AWI_12P-2207; AWI_12P-2308; AWI_12P-2507-1; AWI_12P-2707-3; AWI_12P-3007-1; AWI_PerDyn; AWI Arctic Land Expedition; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; Ice content; Ice type; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; POK1_C; POK1_W; POK3_C; POK3_W; POK4_C_Kolyma_flood_plain; POK4_W; POK7; RU-Land_2012_Kytalyk_Kolyma; Sample code/label; Sampling/measurement on land; Sediment type; Siberia, Russia
    Type: Dataset
    Format: text/tab-separated-values, 625 data points
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  • 76
    Publication Date: 2023-03-07
    Keywords: AWI_12-KYT-0507-1; AWI_12-KYT-0607-1; AWI_12-KYT-0607-2; AWI_12-KYT-0807-1; AWI_12-KYT-0807-2; AWI_PerDyn; AWI Arctic Land Expedition; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; Ice content; Ice type; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; RU-Land_2012_Kytalyk_Kolyma; Sample code/label; Sampling/measurement on land; Sediment type; Siberia, Russia
    Type: Dataset
    Format: text/tab-separated-values, 235 data points
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  • 77
    Publication Date: 2023-03-07
    Keywords: Achchagyi-Allaikha; AWI_12-AA-1007; AWI_PerDyn; AWI Arctic Land Expedition; East Siberia; Height above river level; Ice type; Kytalyk-Pokhodsk_2012, Kolyma2012; LAND; Permafrost Research (Periglacial Dynamics) @ AWI; RU-Land_2012_Kytalyk_Kolyma; Sample code/label; Sampling/measurement on land; Sediment type
    Type: Dataset
    Format: text/tab-separated-values, 72 data points
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  • 78
    Publication Date: 2023-03-07
    Keywords: AWI_PerDyn; AWI_POK-01; AWI Arctic Land Expedition; Date/time end; Date/time start; DEPTH, sediment/rock; Kytalyk-Pokhodsk_2012, Kolyma2012; Layer description; Monitoring station; MONS; Permafrost Research (Periglacial Dynamics) @ AWI; RU-Land_2012_Kytalyk_Kolyma; Siberia, Russia; Temperature, ground, annual mean; Temperature, ground, maximum; Temperature, ground, minimum
    Type: Dataset
    Format: text/tab-separated-values, 48 data points
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  • 79
    Publication Date: 2023-03-07
    Keywords: AWI_A-1; AWI_A-10; AWI_A-11; AWI_A-13; AWI_A-2; AWI_A-3; AWI_A-6; AWI_A-8; AWI_PerDyn; AWI Arctic Land Expedition; Description; East Siberia; Event label; LAND; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; Pokhodsk_2013; RU-Land_2013_Pokhodsk; Sample code/label; Sampling/measurement on land
    Type: Dataset
    Format: text/tab-separated-values, 22 data points
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  • 80
    Publication Date: 2023-03-07
    Keywords: AWI_13-POK-2407-1; AWI_13-POK-2407-3; AWI_13-POK-2507-1; AWI_PerDyn; AWI Arctic Land Expedition; DEPTH, sediment/rock; East Siberia; Event label; Ice content; Ice type; LAND; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; Pokhodsk_2013; RU-Land_2013_Pokhodsk; Sample code/label; Sampling/measurement on land; Sediment type
    Type: Dataset
    Format: text/tab-separated-values, 41 data points
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  • 81
    Publication Date: 2023-03-07
    Keywords: Absorption coefficient, colored dissolved organic matter at 254 nm; Absorption coefficient, colored dissolved organic matter at 260 nm; Absorption coefficient, colored dissolved organic matter at 350 nm; Absorption coefficient, colored dissolved organic matter at 375 nm; Absorption coefficient, colored dissolved organic matter at 400 nm; Absorption coefficient, colored dissolved organic matter at 412 nm; Absorption coefficient, colored dissolved organic matter at 440 nm; Absorption coefficient, colored dissolved organic matter at 443 nm; AWI_PerDyn; COLD-Yamal; COmbining remote sensing and field studies for assessment of Landform Dynamics and permafrost state on Yamal; Date/Time of event; DEPTH, water; Event label; LAKE; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; Sampling lake; Spectral slope of colored dissolved organic matter absorption, 275-295 nm; Spectral slope of colored dissolved organic matter absorption, 300-500 nm; Spectral slope of colored dissolved organic matter absorption, 350-400 nm; Spectral slope of colored dissolved organic matter absorption ratio; Vaskiny Dachi; VD11; VD11_LK-001; VD11_LK-002; VD11_LK-003; VD11_LK-004; VD11_LK-006; VD11_LK-007; VD11_LK-008; VD11_LK-009; VD11_LK-010; VD11_LK-012; VD11_LK-013
    Type: Dataset
    Format: text/tab-separated-values, 132 data points
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  • 82
    Publication Date: 2023-03-07
    Keywords: Absorption coefficient, colored dissolved organic matter at 254 nm; Absorption coefficient, colored dissolved organic matter at 260 nm; Absorption coefficient, colored dissolved organic matter at 350 nm; Absorption coefficient, colored dissolved organic matter at 375 nm; Absorption coefficient, colored dissolved organic matter at 400 nm; Absorption coefficient, colored dissolved organic matter at 412 nm; Absorption coefficient, colored dissolved organic matter at 440 nm; Absorption coefficient, colored dissolved organic matter at 443 nm; AWI_PerDyn; COLD-Yamal; COmbining remote sensing and field studies for assessment of Landform Dynamics and permafrost state on Yamal; Date/Time of event; DEPTH, water; Event label; LAKE; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; Sampling lake; Spectral slope of colored dissolved organic matter absorption, 275-295 nm; Spectral slope of colored dissolved organic matter absorption, 300-500 nm; Spectral slope of colored dissolved organic matter absorption, 350-400 nm; Spectral slope of colored dissolved organic matter absorption ratio; Vaskiny Dachi; VD12; VD12_LK-001; VD12_LK-002; VD12_LK-004; VD12_LK-006; VD12_LK-007; VD12_LK-010; VD12_LK-012; VD12_LK-013
    Type: Dataset
    Format: text/tab-separated-values, 94 data points
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  • 83
    Publication Date: 2023-03-07
    Keywords: Absorption coefficient, colored dissolved organic matter at 254 nm; Absorption coefficient, colored dissolved organic matter at 260 nm; Absorption coefficient, colored dissolved organic matter at 350 nm; Absorption coefficient, colored dissolved organic matter at 375 nm; Absorption coefficient, colored dissolved organic matter at 400 nm; Absorption coefficient, colored dissolved organic matter at 412 nm; Absorption coefficient, colored dissolved organic matter at 440 nm; Absorption coefficient, colored dissolved organic matter at 443 nm; AWI_PerDyn; COLD-Yamal; COmbining remote sensing and field studies for assessment of Landform Dynamics and permafrost state on Yamal; Date/Time of event; DEPTH, water; Event label; LAKE; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; Sampling lake; Spectral slope of colored dissolved organic matter absorption, 275-295 nm; Spectral slope of colored dissolved organic matter absorption, 300-500 nm; Spectral slope of colored dissolved organic matter absorption, 350-400 nm; Spectral slope of colored dissolved organic matter absorption ratio; Vaskiny Dachi; VD13; VD13_LK-001; VD13_LK-003; VD13_LK-004; VD13_LK-008; VD13_LK-013; VD13_LK-014; VD13_LK-015; VD13_LK-017; VD13_LK-018; VD13_LK-020; VD13_LK-022; VD13_LK-024; VD13_LK-027
    Type: Dataset
    Format: text/tab-separated-values, 156 data points
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  • 84
    Publication Date: 2023-03-07
    Keywords: Absorption coefficient, colored dissolved organic matter at 254 nm; Absorption coefficient, colored dissolved organic matter at 260 nm; Absorption coefficient, colored dissolved organic matter at 350 nm; Absorption coefficient, colored dissolved organic matter at 375 nm; Absorption coefficient, colored dissolved organic matter at 400 nm; Absorption coefficient, colored dissolved organic matter at 412 nm; Absorption coefficient, colored dissolved organic matter at 440 nm; Absorption coefficient, colored dissolved organic matter at 443 nm; AWI_PerDyn; COLD-Yamal; COmbining remote sensing and field studies for assessment of Landform Dynamics and permafrost state on Yamal; Date/Time of event; DEPTH, water; Event label; LAKE; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; Sampling lake; Spectral slope of colored dissolved organic matter absorption, 275-295 nm; Spectral slope of colored dissolved organic matter absorption, 300-500 nm; Spectral slope of colored dissolved organic matter absorption, 350-400 nm; Spectral slope of colored dissolved organic matter absorption ratio; Vaskiny Dachi; VD14; VD14_LK-001; VD14_LK-002; VD14_LK-004; VD14_LK-006; VD14_LK-007; VD14_LK-008; VD14_LK-010; VD14_LK-012; VD14_LK-013; VD14_LK-015; VD14_LK-016; VD14_LK-017; VD14_LK-018; VD14_LK-019; VD14_LK-020; VD14_LK-024; VD14_LK-025; VD14_LK-027; VD14_LK-035; VD14_LK-036
    Type: Dataset
    Format: text/tab-separated-values, 236 data points
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  • 85
    Publication Date: 2023-03-07
    Keywords: Absorption coefficient, colored dissolved organic matter at 254 nm; Absorption coefficient, colored dissolved organic matter at 260 nm; Absorption coefficient, colored dissolved organic matter at 350 nm; Absorption coefficient, colored dissolved organic matter at 375 nm; Absorption coefficient, colored dissolved organic matter at 400 nm; Absorption coefficient, colored dissolved organic matter at 412 nm; Absorption coefficient, colored dissolved organic matter at 440 nm; Absorption coefficient, colored dissolved organic matter at 443 nm; AWI_PerDyn; COLD-Yamal; COmbining remote sensing and field studies for assessment of Landform Dynamics and permafrost state on Yamal; Date/Time of event; DEPTH, water; Event label; LAKE; Latitude of event; Longitude of event; Permafrost Research (Periglacial Dynamics) @ AWI; Sampling lake; Spectral slope of colored dissolved organic matter absorption, 275-295 nm; Spectral slope of colored dissolved organic matter absorption, 300-500 nm; Spectral slope of colored dissolved organic matter absorption, 350-400 nm; Spectral slope of colored dissolved organic matter absorption ratio; Vaskiny Dachi; VD15; VD15_LK-001; VD15_LK-003; VD15_LK-004; VD15_LK-006; VD15_LK-007; VD15_LK-008; VD15_LK-010; VD15_LK-012; VD15_LK-013; VD15_LK-014; VD15_LK-015; VD15_LK-016; VD15_LK-017; VD15_LK-018; VD15_LK-019; VD15_LK-020; VD15_LK-025; VD15_LK-026; VD15_LK-027; VD15_LK-028; VD15_LK-029; VD15_LK-033; VD15_LK-034
    Type: Dataset
    Format: text/tab-separated-values, 253 data points
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  • 86
    Publication Date: 2023-03-07
    Keywords: AWI_PerDyn; AWI Arctic Land Expedition; MULT; Multiple investigations; Permafrost Research (Periglacial Dynamics) @ AWI; RU-Land_2013_Taymyr; Taymyr_peninsula_2013; Taymyr2013; Taymyr peninsula, northern Siberia
    Type: Dataset
    Format: application/zip, 66.5 kBytes
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  • 87
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    PANGAEA
    In:  Supplement to: Dulias, Katharina; Stoof-Leichsenring, Kathleen Rosmarie; Pestryakova, Luidmila A; Herzschuh, Ulrike (2016): Sedimentary DNA versus morphology in the analysis of diatom-environment relationships. Journal of Paleolimnology, 16 pp, https://doi.org/10.1007/s10933-016-9926-y
    Publication Date: 2023-03-07
    Description: The Arctic treeline ecotone is characterized by a steep vegetation gradient from arctic tundra to northerntaiga forests, which is thought to influence the water chemistry of thermokarst lakes in this region.Environmentally sensitive diatoms respond to such ecological changes in terms of variation in diatomdiversity and richness, which so far has only been documented by microscopic surveys. We applied nextgenerationsequencing to analyse the diatom composition of lake sediment DNA extracted from 32 lakesacross the treeline in the Khatanga region, Siberia, using a short fragment of the rbcL chloroplast gene as agenetic barcode. We compared diatom richness and diversity obtained from the genetic approach withdiatom counts from traditional microscopic analysis. Both datasets were employed to investigate diversityand relationships with environmental variables, using ordination methods. After effective filtering of theraw data, the two methods gave similar results for diatom richness and composition at the genus level(DNA 12 taxa; morphology 19 taxa), even though there was a much higher absolute number of sequencesobtained per genetic sample (median 50,278), compared with microscopic counts (median 426). Dissolvedorganic carbon explained the highest percentage of variance in both datasets (14.2 % DNA; 18.7 %morphology), reflecting the compositional turnover of diatom assemblages along the tundra-taigatransition. Differences between the two approaches are mostly a consequence of the filtering process ofgenetic data and limitations of genetic references in the database, which restricted the determination ofgenetically identified sequence types to the genus level. The morphological approach, however, allowedidentifications mostly to species level, which permits better ecological interpretation of the diatom data.Nevertheless, because of a rapidly increasing reference database, the genetic approach with sediment DNAwill, in the future, enable reliable investigations of diatom composition from lake sediments that will havepotential applications in both paleoecology and environmental monitoring.
    Keywords: AWI_PerDyn; Permafrost Research (Periglacial Dynamics) @ AWI
    Type: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 13.4 kBytes
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  • 88
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    PANGAEA
    In:  Institut für Meereskunde, Universität Hamburg
    Publication Date: 2023-03-10
    Description: RV POSEIDON cruise POS264 was carried out by the Institut für Meereskunde of the University of Hamburg and staff from the Niels Bohr Instituttet for Astronomi, Fysik og Geofysik of the University of Copenhagen also participated. The cruise had several objectives: - to educate undergraduate students in the handling of oceanographic instrumentation and in the collection and analysis of field data, - to map the cold overflow through the Faroe-Bank Channel from the Norwegian Sea into the Icelandic Basin and to study its short-time variability and - to quantify the contributions of the water masses which are involved in the mixing of the overflow plume with its ambient water. The planning and preparation of the cruise involved the participating students and was carried out during seminars, both at the Universities of Hamburg and Copenhagen. Following a review of the recent literature and an analysis of historical data the observational programme was designed. Hydrographic and current profiling stations were occupied along several sections crossing the overflow. The experiment was financed by the University of Hamburg. Temperature, salinity and dissolved oxygen data from CTD stations are presented. The temperature and salinity data were quality controlled and calibrated. Oxygen data are not calibrated as no oxygen samples were taken additionally during the cruise.
    Keywords: CTD; CTD/Rosette; CTD001; CTD002; CTD003; CTD004; CTD005; CTD006; CTD007; CTD008; CTD009; CTD010; CTD011; CTD012; CTD013; CTD014; CTD015; CTD016; CTD017; CTD018; CTD019; CTD020; CTD021; CTD022; CTD023; CTD024; CTD025; CTD026; CTD027; CTD028; CTD029; CTD030; CTD031; CTD032; CTD033; CTD034; CTD035; CTD036; CTD037; CTD038; CTD039; CTD040; CTD041; CTD042; CTD043; CTD044; CTD045; CTD046; CTD047; CTD048; CTD049; CTD050; CTD051; CTD052; CTD053; CTD054; CTD055; CTD056; CTD057; CTD058; CTD059; CTD060; CTD061; CTD062; CTD063; CTD064; CTD065; CTD066; CTD067; CTD068; CTD069; CTD070; CTD071; CTD072; CTD073; CTD074; CTD075; CTD076; CTD077; CTD078; CTD079; CTD080; CTD081; CTD082; CTD083; CTD084; CTD085; CTD086; CTD087; CTD088; CTD089; CTD090; CTD091; CTD092; CTD093; CTD094; CTD095; CTD096; CTD097; CTD098; CTD099; CTD100; CTD101; CTD102; CTD103; CTD104; CTD105; CTD106; CTD107; CTD108; CTD109; CTD110; CTD111; CTD112; CTD113; CTD114; CTD115; CTD116; CTD117; CTD118; CTD119; CTD120; CTD121; CTD122; CTD123; CTD124; CTD125; CTD126; CTD127; CTD128; CTD129; CTD130; CTD131; CTD132; CTD133; CTD134; CTD-RO; Date/Time of event; DEPTH, water; Event label; Latitude of event; Longitude of event; Optional event label; Oxygen; POS264; POS264_327-1; POS264_328-1; POS264_329-1; POS264_330-1; POS264_331-1; POS264_332-1; POS264_333-1; POS264_334-1; POS264_335-1; POS264_336-1; POS264_337-1; POS264_338-1; POS264_339-1; POS264_340-1; POS264_341-1; POS264_342-1; POS264_343-1; POS264_344-1; POS264_345-1; POS264_346-1; POS264_347-1; POS264_348-1; POS264_349-1; POS264_350-1; POS264_351-1; POS264_352-1; POS264_353-1; POS264_354-1; POS264_355-1; POS264_356-1; POS264_357-1; POS264_358-1; POS264_359-1; POS264_360-1; POS264_361-1; POS264_362-1; POS264_363-1; POS264_364-1; POS264_365-1; POS264_366-1; POS264_367-1; POS264_368-1; POS264_369-1; POS264_370-1; POS264_371-1; POS264_372-1; POS264_373-1; POS264_374-1; POS264_375-1; POS264_376-1; POS264_377-1; POS264_378-1; POS264_379-1; POS264_380-1; POS264_381-1; POS264_382-1; POS264_383-1; POS264_384-1; POS264_385-1; POS264_386-1; POS264_387-1; POS264_388-1; POS264_389-1; POS264_390-1; POS264_390-2; POS264_391-1; POS264_392-1; POS264_394-1; POS264_395-1; POS264_396-1; POS264_397-1; POS264_398-1; POS264_399-1; POS264_400-1; POS264_401-1; POS264_402-1; POS264_403-1; POS264_404-1; POS264_405-1; POS264_406-1; POS264_407-1; POS264_408-1; POS264_409-1; POS264_410-1; POS264_411-1; POS264_412-1; POS264_413-1; POS264_414-1; POS264_415-1; POS264_416-1; POS264_417-1; POS264_418-1; POS264_419-1; POS264_420-1; POS264_421-1; POS264_422-1; POS264_423-1; POS264_424-1; POS264_425-1; POS264_426-1; POS264_427-1; POS264_428-1; POS264_429-1; POS264_430-1; POS264_431-1; POS264_432-1; POS264_433-1; POS264_434-1; POS264_435-1; POS264_436-1; POS264_437-1; POS264_438-1; POS264_439-1; POS264_440-1; POS264_441-1; POS264_442-1; POS264_443-1; POS264_444-1; POS264_445-1; POS264_446-1; POS264_447-1; POS264_448-1; POS264_449-1; POS264_450-1; POS264_451-1; POS264_452-1; POS264_453-1; POS264_454-1; POS264_455-1; POS264_456-1; POS264_457-1; POS264_458-1; POS264_459-1; POS264_460-1; Poseidon; Pressure, water; Salinity; South Atlantic Ocean; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 545096 data points
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  • 89
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    In:  Supplement to: Riedinger, Natascha; Brunner, Benjamin; Krastel, Sebastian; Arnold, Gail Lee; Wehrmann, Laura Mariana; Formolo, Michael J; Beck, Antje; Bates, Steven M; Henkel, Susann; Kasten, Sabine; Lyons, Timothy W (2017): Sulfur cycling in an iron oxide-dominated, dynamic marine depositional system: The Argentine continental margin. Frontiers in Earth Science, 5, https://doi.org/10.3389/feart.2017.00033
    Publication Date: 2023-03-03
    Description: The interplay between sediment deposition patterns, organic matter type and the quantity and quality of reactive mineral phases determines the accumulation, speciation and isotope composition of pore water and solid phase sulfur constituents in marine sediments. Here, we present the sulfur geochemistry of siliciclastic sediments from two sites along the Argentine continental slope--a system characterized by dynamic deposition and reworking, which result in non-steady state conditions. The two investigated sites have different depositional histories but have in common that reactive iron phases are abundant and that organic matter is refractory--conditions that result in low organoclastic sulfate reduction rates. Deposition of reworked, isotopically light pyrite and sulfurized organic matter appear to be important contributors to the sulfur inventory, with only minor addition of pyrite from organoclastic sulfate reduction above the sulfate-methane transition (SMT). Pore-water sulfide is limited to a narrow zone at the SMT. The core of that zone is dominated by pyrite accumulation. Iron monosulfide and elemental sulfur accumulate above and below this zone. Iron monosulfide precipitation is driven by the reaction of low amounts of hydrogen sulfide with ferrous iron and is in competition with the oxidation of sulfide by iron (oxyhydr)oxides to form elemental sulfur. The intervals marked by precipitation of intermediate sulfur phases at the margin of the zone with free sulfide are bordered by two distinct peaks in total organic sulfur. Organic matter sulfurization appears to precede pyrite formation in the iron-dominated margins of the sulfide zone, potentially linked to the presence of polysulfides formed by reaction between dissolved sulfide and elemental sulfur. Thus, SMTs can be hotspots for organic matter sulfurization in sulfide-limited, reactive iron-rich marine sedimentary systems. Furthermore, existence of elemental sulfur and iron monosulfide phases meters below the SMT demonstrates that in sulfide-limited systems metastable sulfur constituents are not readily converted to pyrite but can be buried to deeper sediment depths. Our data show that in non-steady state systems, redox zones do not occur in sequence but can reappear or proceed in inverse sequence throughout the sediment column, causing similar mineral alteration processes to occur at the same time at different sediment depths.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 12 datasets
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  • 90
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    In:  Supplement to: Gussone, Nikolaus; Filipsson, Helena L; Kuhnert, Henning (2016): Mg/Ca, Sr/Ca and Ca isotope ratios in benthonic foraminifers related to test structure, mineralogy and environmental controls. Geochimica et Cosmochimica Acta, 173, 142-159, https://doi.org/10.1016/j.gca.2015.10.018
    Publication Date: 2023-03-03
    Description: We analysed Mg/Ca, Sr/Ca and Ca isotope ratios of benthonic foraminifers from sediment core tops retrieved during several research cruises in the Atlantic Ocean, in order to improve the understanding of isotope fractionation and element partitioning resulting from biomineralisation processes and changes in ambient conditions. Species include foraminifers secreting tests composed of hyaline low magnesium calcite, porcelaneous high magnesium calcite as well as aragonite. Our results demonstrate systematic isotope fractionation and element partitioning patterns specific for these foraminiferal groups. Calcium isotope fractionation is similar in porcelaneous and hyaline calcite tests and both groups demonstrate the previously described anomaly with enrichment of heavy isotopes around 3 - 4 °C (Gussone and Filipsson, 2010). Calcium isotope ratios of the aragonitic species Hoeglundina elegans, on the other hand, are about 0.4 per mil lighter compared to the calcitic species, which is in general agreement with stronger fractionation in inorganic aragonite compared to calcite. However, the low and strongly variable Sr content suggests additional processes during test formation, and we propose that transmembrane ion transport or a precursor phase to aragonite may be involved. Porcelaneous tests, composed of high Mg calcite, incorporate higher amounts of Sr compared to hyaline low Mg calcite, in agreement with inorganic calcite systematics, but also porcelaneous tests with reduced Mg/Ca show high Sr/Ca. While calcium isotopes, Sr/Ca and Mg/Ca in benthonic foraminifers primarily appear to fractionate and partition with a dominant inorganic control, d44/40Ca temperature and growth rate dependencies of benthonic foraminifer tests favour a dominant contribution of light Ca by transmembrane transport relative to unfractionated seawater Ca to the calcifying fluid, thus controlling the formation of foraminiferal d44/40Ca and Sr/Ca proxy signals.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 91
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    PANGAEA
    In:  Supplement to: Johnstone, Heather J H; Lee, R W; Schulz, Michael (2016): Effect of preservation state of planktonic foraminifera tests on the decrease in Mg/Ca due to reductive cleaning and on sample loss during cleaning. Chemical Geology, 420, 23-36, https://doi.org/10.1016/j.chemgeo.2015.10.045
    Publication Date: 2023-03-03
    Description: Four species of planktic foraminifera from core-tops spanning a depth transect on the Ontong Java Plateau were prepared for Mg/Ca analysis both with (Cd-cleaning) and without (Mg-cleaning) a reductive cleaning step. Reductive cleaning caused etching of foraminiferal calcite, focused on Mg-rich inner calcite, even on tests which had already been partially dissolved at the seafloor. Despite corrosion, there was no difference in Mg/Ca of Pulleniatina obliquiloculata between cleaning methods. Reductive cleaning decreased Mg/Ca by an average (all depths) of ~ 4% for Globigerinoides ruber white and ~ 10% for Neogloboquadrina dutertrei. Mg/Ca of Globigerinoides sacculifer (above the calcite saturation horizon only) was 5% lower after reductive cleaning. The decrease in Mg/Ca due to reductive cleaning appeared insensitive to preservation state for G. ruber, N. dutertrei and P. obliquiloculata. Mg/Ca of Cd-cleaned G. sacculifer appeared less sensitive to dissolution than that of Mg-cleaned. Mg-cleaning is adequate, but SEM and contaminants (Al/Ca, Fe/Ca and Mn/Ca) show that Cd-cleaning is more effective for porous species. A second aspect of the study addressed sample loss during cleaning. Lower yield after Cd-cleaning for G. ruber, G. sacculifer and N. dutertrei confirmed this to be the more aggressive method. Strongest correlations between yield and Delta[CO3^2-] in core-top samples were for Cd-cleaned G. ruber (r = 0.88, p = 0.020) and Cd-cleaned P. obliquiloculata (r = 0.68, p = 0.030). In a down-core record (WIND28K) correlation, r, between yield values 〉 30% and dissolution index, XDX, was -0.61 (p = 0.002). Where cleaning yield 〈 30% most Mg-cleaned Mg/Ca values were biased by dissolution.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 92
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    PANGAEA
    In:  Supplement to: Castañeda, Isla S; Schouten, Stefan; Pätzold, Jürgen; Lucassen, Friedrich; Kasemann, Simone A; Kuhlmann, Holger; Schefuß, Enno (2016): Hydroclimate variability in the Nile River Basin during the past 28,000 years. Earth and Planetary Science Letters, 438, 47-56, https://doi.org/10.1016/j.epsl.2015.12.014
    Publication Date: 2023-03-03
    Description: It has long been known that extreme changes in North African hydroclimate occurred during the late Pleistocene yet many discrepancies exist between sites regarding the timing, duration and abruptness of events such as Heinrich Stadial (HS) 1 and the African Humid Period (AHP). The hydroclimate history of the Nile River is of particular interest due to its lengthy human occupation history yet there are presently few continuous archives from the Nile River corridor, and pre-Holocene studies are rare. Here we present new organic and inorganic geochemical records of Nile Basin hydroclimate from an eastern Mediterranean (EM) Sea sediment core spanning the past 28 ka BP. Our multi-proxy records reflect the fluctuating inputs of Blue Nile versus White Nile material to the EM Sea in response to gradual changes in local insolation and also capture abrupt hydroclimate events driven by remote climate forcings, such as HS1. We find strong evidence for extreme aridity within the Nile Basin evolving in two distinct phases during HS1, from 17.5 to 16 ka BP and from 16 to 14.5 ka BP, whereas peak wet conditions during the AHP are observed from 9 to 7 ka BP. We find that zonal movements of the Congo Air Boundary (CAB), and associated shifts in the dominant moisture source (Atlantic versus Indian Ocean moisture) to the Nile Basin, likely contributed to abrupt hydroclimate variability in northern East Africa during HS1 and the AHP as well as to non-linear behavior of hydroclimate proxies. We note that different proxies show variable gradual and abrupt responses to individual hydroclimate events, and thus might have different inherent sensitivities, which may be a factor contributing to the controversy surrounding the abruptness of past events such as the AHP. During the Late Pleistocene the Nile Basin experienced extreme hydroclimate fluctuations, which presumably impacted Paleolithic cultures residing along the Nile corridor.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 93
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    PANGAEA
    In:  Supplement to: Vogts, Angela; Badewien, Tanja; Rullkötter, Jürgen; Schefuß, Enno (2016): Near-constant apparent hydrogen isotope fractionation between leaf wax n-alkanes and precipitation in tropical regions: Evidence from a marine sediment transect off SW Africa. Organic Geochemistry, 96, 18-27, https://doi.org/10.1016/j.orggeochem.2016.03.003
    Publication Date: 2023-03-03
    Description: A transect of marine surface sediment samples from 1° N to 28° S off southwest Africa was analysed to verify the application of hydrogen isotope compositions of terrestrial plant-wax n-alkanes preserved in ocean sediments as a proxy for continental hydrological conditions. Conditions on the adjacent continent range from humid evergreen forests to deciduous forests, wood- and shrub land and further to arid grasslands and deserts. The hydrogen isotope values for the dominant n-alkane homologues (C29, C31 and C33) vary from -123 per mil to -141 per mil VSMOW and correlate with the modelled hydrogen isotope composition of mean annual and growing season precipitation of postulated continental source areas (r up to 0.8, p 〈 0.01). The apparent hydrogen isotope fractionation between alkanes and mean annual precipitation is remarkably uniform (-109 per mil on average, Sigma 〈= 5 per mil, n = 27). Potentially, effects of aridity on the apparent hydrogen isotope fractionation are concealed by the contribution of different plants (C3 dicotyledons vs C4 grasses). Thus, isotope ratios of leaf wax n-alkanes preserved in ocean margin sediments in these and similar tropical regions may be directly converted to dD ratios of ancient precipitation by employing a constant hydrogen isotope fractionation.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 94
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    PANGAEA
    In:  Supplement to: Zhuang, Guang-Chao; Elling, Felix J; Nigro, Lisa M; Samarkin, Vladimir A; Joye, Samantha B; Teske, Andreas P; Hinrichs, Kai-Uwe (2016): Multiple evidence for methylotrophic methanogenesis as the dominant methanogenic pathway in hypersaline sediments from the Orca Basin, Gulf of Mexico. Geochimica et Cosmochimica Acta, 187, 1-20, https://doi.org/10.1016/j.gca.2016.05.005
    Publication Date: 2023-03-03
    Description: Among the most extreme habitats on Earth, dark, deep, anoxic brines host unique microbial ecosystems that remain largely unexplored. As the terminal step of anaerobic degradation of organic matter, methanogenesis is a potentially significant but poorly constrained process in deep-sea hypersaline environments. We combined biogeochemical and phylogenetic analyses as well as incubation experiments to unravel the origin of methane in hypersaline sediments of Orca Basin in the northern Gulf of Mexico. Substantial concentrations of methane (up to 3.4 mM) coexisted with high concentrations of sulfate (16-43 mM) in two sediment cores retrieved from the northern and southern parts of Orca Basin. The strong depletion of 13C in methane (-77 to -89 per mill) pointed towards a biological source. While low concentrations of competitive substrates limited the significance of hydrogenotrophic and acetoclastic methanogenesis, the presence of non-competitive methylated substrates (methanol, trimethylamine, dimethyl sulfide, dimethylsulfoniopropionate) supported the potential for methane generation through methylotrophic methanogenesis. Thermodynamic calculations demonstrated that hydrogenotrophic and acetoclastic methanogenesis were unlikely to occur under in situ conditions, while methylotrophic methanogenesis from a variety of substrates was highly favorable. Likewise, carbon isotope relationships between methylated substrates and methane supported methylotrophic methanogenesis as the major source of methane. Stable isotope tracer and radiotracer experiments with 13C bicarbonate, acetate and methanol as well as 14C-labeled methylamine indicated that methylotrophic methanogenesis was the predominant methanogenic pathway. Based on 16S rRNA gene sequences, halophilic methylotrophic methanogens related to the genus Methanohalophilus dominated the benthic archaeal community in the northern basin but also occurred in the southern basin. High abundances of methanogen lipid biomarkers such as intact polar and polyunsaturated hydroxyarchaeols were detected in sediments from the northern basin, with lower abundances in the southern basin. Strong 13C-depletion of saturated and monounsaturated hydroxyarchaeol were consistent with methylotrophic methanogenesis as the major methanogenic pathway. Collectively, the availability of methylated substrates, thermodynamic calculations, experimentally determined methanogenic activity as well as lipid and gene biomarkers strongly suggested methylotrophic methanogenesis as predominant pathway of methane formation in the presence of sulfate in Orca Basin sediments.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 95
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    PANGAEA
    In:  Supplement to: Bernhardt, Anne; Hebbeln, Dierk; Regenberg, Marcus; Lückge, Andreas; Strecker, Manfred R (2016): Shelfal sediment transport by an undercurrent forces turbidity-current activity during high sea level along the Chile continental margin. Geology, 44(4), 295-298, https://doi.org/10.1130/G37594.1
    Publication Date: 2023-03-03
    Description: Terrigenous sediment supply, marine transport, and depositional processes along tectonically active margins are key to decoding turbidite successions as potential archives of climatic and seismic forcings. Sequence stratigraphic models predict coarse-grained sediment delivery to deep-marine sites mainly during sea-level fall and lowstand. Marine siliciclastic deposition during transgressions and highstands has been attributed to sustained connectivity between terrigenous sources and marine sinks facilitated by narrow shelves. To decipher the controls on Holocene highstand turbidite deposition, we analyzed 12 sediment cores from spatially discrete, coeval turbidite systems along the Chile margin (29° - 40°S) with changing climatic and geomorphic characteristics but uniform changes in sea level. Sediment cores from intraslope basins in north-central Chile (29° - 33°S) offshore a narrow to absent shelf record a shut-off of turbidite deposition during the Holocene due to postglacial aridification. In contrast, core sites in south-central Chile (36° - 40°S) offshore a wide shelf record frequent turbidite deposition during highstand conditions. Two core sites are linked to the Biobío river-canyon system and receive sediment directly from the river mouth. However, intraslope basins are not connected via canyons to fluvial systems but yield even higher turbidite frequencies. High sediment supply combined with a wide shelf and an undercurrent moving sediment toward the shelf edge appear to control Holocene turbidite sedimentation and distribution. Shelf undercurrents may play an important role in lateral sediment transport and supply to the deep sea and need to be accounted for in sediment-mass balances.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 96
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    In:  Supplement to: Perez, Laura; García-Rodríguez, Felipe; Hanebuth, Till J J (2016): Variability in terrigenous sediment supply offshore of the Río de la Plata (Uruguay) recording the continental climatic history over the past 1200 years. Climate of the Past, 12(3), 623-634, https://doi.org/10.5194/cp-12-623-2016
    Publication Date: 2023-03-03
    Description: The continental shelf adjacent to the Río de la Plata (RdlP) exhibits extremely complex hydrographic and ecological characteristics which are of great socioeconomic importance. Since the long-term environmental variations related to the atmospheric (wind fields), hydrologic (freshwater plume), and oceanographic (currents and fronts) regimes are little known, the aim of this study is to reconstruct the changes in the terrigenous input into the inner continental shelf during the late Holocene period (associated with the RdlP sediment discharge) and to unravel the climatic forcing mechanisms behind them. To achieve this, we retrieved a 10 m long sediment core from the RdlP mud depocenter at 57 m water depth (GeoB 13813-4). The radiocarbon age control indicated an extremely high sedimentation rate of 0.8 cm per year, encompassing the past 1200 years (AD 750-2000). We used element ratios (Ti / Ca, Fe / Ca, Ti / Al, Fe / K) as regional proxies for the fluvial input signal and the variations in relative abundance of salinity-indicative diatom groups (freshwater versus marine-brackish) to assess the variability in terrigenous freshwater and sediment discharges. Ti / Ca, Fe / Ca, Ti / Al, Fe / K and the freshwater diatom group showed the lowest values between AD 850 and 1300, while the highest values occurred between AD 1300 and 1850. The variations in the sedimentary record can be attributed to the Medieval Climatic Anomaly (MCA) and the Little Ice Age (LIA), both of which had a significant impact on rainfall and wind patterns over the region. During the MCA, a weakening of the South American summer monsoon system (SAMS) and the South Atlantic Convergence Zone (SACZ), could explain the lowest element ratios (indicative of a lower terrigenous input) and a marine-dominated diatom record, both indicative of a reduced RdlP freshwater plume. In contrast, during the LIA, a strengthening of SAMS and SACZ may have led to an expansion of the RdlP river plume to the far north, as indicated by higher element ratios and a marked freshwater diatom signal. Furthermore, a possible multidecadal oscillation probably associated with Atlantic Multidecadal Oscillation (AMO) since AD 1300 reflects the variability in both the SAMS and SACZ systems.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 97
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    In:  Supplement to: Rachmayani, Rima; Prange, Matthias; Schulz, Michael (2016): Intra-interglacial climate variability: model simulations of Marine Isotope Stages 1, 5, 11, 13, and 15. Climate of the Past, 12(3), 677-695, https://doi.org/10.5194/cp-12-677-2016
    Publication Date: 2023-03-03
    Description: Using the Community Climate System Model version 3 (CCSM3) including a dynamic global vegetation model, a set of 13 time slice experiments was carried out to study global climate variability between and within the Quaternary interglacials of Marine Isotope Stages (MISs) 1, 5, 11, 13, and 15. The selection of interglacial time slices was based on different aspects of inter- and intra-interglacial variability and associated astronomical forcing. The different effects of obliquity, precession, and greenhouse gas (GHG) forcing on global surface temperature and precipitation fields are illuminated. In most regions seasonal surface temperature anomalies can largely be explained by local insolation anomalies induced by the astronomical forcing. Climate feedbacks, however, may modify the surface temperature response in specific regions, most pronounced in the monsoon domains and the polar oceans. GHG forcing may also play an important role for seasonal temperature anomalies, especially at high latitudes and early Brunhes interglacials (MIS 13 and 15) when GHG concentrations were much lower than during the later interglacials. High- versus low-obliquity climates are generally characterized by strong warming over the Northern Hemisphere extratropics and slight cooling in the tropics during boreal summer. During boreal winter, a moderate cooling over large portions of the Northern Hemisphere continents and a strong warming at high southern latitudes is found. Beside the well-known role of precession, a significant role of obliquity in forcing the West African monsoon is identified. Other regional monsoon systems are less sensitive or not sensitive at all to obliquity variations during interglacials. Moreover, based on two specific time slices (394 and 615 ka), it is explicitly shown that the West African and Indian monsoon systems do not always vary in concert, challenging the concept of a global monsoon system on astronomical timescales. High obliquity can also explain relatively warm Northern Hemisphere high-latitude summer temperatures despite maximum precession around 495 ka (MIS 13). It is hypothesized that this obliquity-induced high-latitude warming may have prevented a glacial inception at that time.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 98
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    In:  Supplement to: Kretschmer, Kerstin; Kucera, Michal; Schulz, Michael (2016): Modeling the distribution and seasonality of Neogloboquadrina pachyderma in the North Atlantic Ocean during Heinrich Stadial 1. Paleoceanography, 31(7), 986-1010, https://doi.org/10.1002/2015PA002819
    Publication Date: 2023-03-03
    Description: Fossil shells of planktonic foraminifera serve as the prime source of information on past changes in surface ocean conditions. Because the population size of planktonic foraminifera species changes throughout the year, the signal preserved in fossil shells is biased towards the conditions when species production was at its maximum. The amplitude of the potential seasonal bias is a function of the magnitude of the seasonal cycle in production. Here we use a planktonic foraminifera model coupled to an ecosystem model to investigate to what degree seasonal variations in production of the species Neogloboquadrina pachyderma may affect paleoceanographic reconstructions during Heinrich Stadial 1 (~18-15 cal. ka B.P.) in the North Atlantic Ocean. The model implies that during Heinrich Stadial 1 the maximum seasonal production occurred later in the year compared to the Last Glacial Maximum (~21-19 cal. ka B.P.) and the pre-industrial era north of 30 ºN. A diagnosis of the model output indicates that this change reflects the sensitivity of the species to the seasonal cycle of sea-ice cover and food supply, which collectively lead to shifts in the modeled maximum production from the Last Glacial Maximum to Heinrich Stadial 1 by up to six months. Assuming equilibrium oxygen isotopic incorporation in the shells of N. pachyderma, the modeled changes in seasonality would result in an underestimation of the actual magnitude of the meltwater isotopic signal recorded by fossil assemblages of N. pachyderma wherever calcification is likely to take place.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 99
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    In:  Supplement to: Kulgemeyer, Tobias; von Dobeneck, Tilo; Müller, Hendrik; Bryan, Karin R; de Lange, Willem P; Battershill, Christopher N (2016): Lithofacies distribution and sediment dynamics on a storm-dominated shelf from combined photographic, acoustic and sedimentological profiling methods (Bay of Plenty, New Zealand). Marine Geology, 376, 158-174, https://doi.org/10.1016/j.margeo.2016.03.005
    Publication Date: 2023-03-03
    Description: Sediment dynamics on a storm-dominated shelf (western Bay of Plenty, New Zealand) were mapped and analyzed using the newly developed multi-sensor benthic profiler MARUM NERIDIS III. An area of 60 km × 7 km between 2 and 35 m water depth was surveyed with this bottom-towed sled equipped with a high-resolution camera for continuous close-up seafloor photography and a CTD with connected turbidity sensor. Here we introduce our approach of using this multi-parameter dataset combined with sidescan sonography and sedimentological analyses to create detailed lithofacies and bedform distribution maps and to derive regional sediment transport patterns. For the assessment of sediment distribution, photographs were classified and their spatial distribution mapped out according to associated acoustic backscatter from a sidescan sonar. This provisional map was used to choose target locations for surficial sediment sampling and subsequent laboratory analysis of grain size distribution and mineralogical composition. Finally, photographic, granulometric and mineralogical facies were combined into a unified lithofacies map and corresponding stratigraphic model. Eight distinct types of lithofacies with seawards increasing grain size were discriminated and interpreted as reworked relict deposits overlain by post-transgressional fluvial sediments. The dominant transport processes in different water depths were identified based on type and orientation of bedforms, as well as bottom water turbidity and lithofacies distribution. Observed bedforms include subaquatic dunes, coarse sand ribbons and sorted bedforms of varying dimensions, which were interpreted as being initially formed by erosion. Under fair weather conditions, sediment is transported from the northwest towards the southeast by littoral drift. During storm events, a current from the southeast to the northweast is induced which is transporting sediment along the shore in up to 35 m water depth. Shorewards oriented cross-shore transport is taking place in up to 60 m water depth and is likewise initiated by storm events. Our study demonstrates how benthic photographic profiling delivers comprehensive compositional, structural and environmental information, which compares well with results obtained by traditional probing methods, but offers much higher spatial resolution while covering larger areas. Multi-sensor benthic profiling enhances the interpretability of acoustic seafloor mapping techniques and is a rapid and economic approach to seabed and habitat mapping especially in muddy to sandy facies.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 4 datasets
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    In:  Supplement to: Jorat, Ehsan M; Mörz, Tobias; Moon, Vicki G; Kreiter, Stefan; de Lange, Willem P (2015): Utilizing piezovibrocone in marine soils at Tauranga Harbor, New Zealand. Geomechanics and Engineering, 9(1), 1-14, https://doi.org/10.12989/gae.2015.9.1.001
    Publication Date: 2023-03-03
    Description: Piezovibrocones have been developed to evaluate the liquefaction potential of onshore soils, but have not yet been utilized to evaluate the in-situ liquefaction behavior of offshore marine and volcanoclastic sediments. Two static and vibratory CPTu (Cone Penetration Tests) were performed at Tauranga Harbor, New Zealand. The lithology is known from nearby drillholes and the influence of vibration on different types of marine soils is evaluated using the reduction ratio (RR) calculated from static and vibratory CPTu. A sediment layer with high potential for liquefaction and one with a slight reaction to cyclic loading are identified. In addition to the reduction ratio, the liquefaction potential of sediment is analyzed using classic correlations for static CPTu data, but no liquefaction potential was determined. This points to an underestimation of liquefaction potential with the classic static CPTu correlations in marine soil. Results show that piezovibrocone tests are a sensitive tool for liquefaction analysis in offshore marine and volcanoclastic soil.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 8 datasets
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