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  • 1
    Publication Date: 2024-06-26
    Description: A deciduous shrub previously included in Ficus talbotii for many years, is now regarded as a new species, Ficus pongumphaii. It is morphologically distinct from F. talbotii with as typical characters the densely brown pubescent to tomentose or villous on leafy twig; the elliptic, suborbicular to obovate leaf blades that are brown tomentellous on the upper surface and brown floccose tomentose to villous underneath; the pedunculate figs are obovate, brown floccose or villous outside and have internal hairs. The leaf anatomy shows a multiple epidermis on both surfaces; enlarged lithocysts on both sides of the lamina, which are more abundant adaxially and with very few abaxially. The species, endemic to Thailand, is named after the great Thai dendrologist, Associate Professor Somnuek Pongumphai.
    Keywords: Ficus ; leaf anatomy ; Moraceae ; new species
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 2
    Publication Date: 2024-06-26
    Description: When volcanic mountains slide into the sea, they trigger tsunamis. How big are these waves, and how far away can they do damage? Ritter Island provides some answers.
    Type: Article , PeerReviewed
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  • 3
    Publication Date: 2024-06-26
    Description: In this study we look beyond the previously studied effects of oceanic CO2 injections on atmospheric and oceanic reservoirs and also account for carbon cycle and climate feedbacks between the atmosphere and the terrestrial biosphere. Considering these additional feedbacks is important since backfluxes from the terrestrial biosphere to the atmosphere in response to reducing atmospheric CO2 can further offset the targeted reduction. To quantify these dynamics we use an Earth system model of intermediate complexity to simulate direct injection of CO2 into the deep ocean as a means of emissions mitigation during a high CO2 emission scenario. In three sets of experiments with different injection depths, we simulate a 100-year injection period of a total of 70 GtC and follow global carbon cycle dynamics over another 900 years. In additional parameter perturbation runs, we varied the default terrestrial photosynthesis CO2 fertilization parameterization by ±50 % in order to test the sensitivity of this uncertain carbon cycle feedback to the targeted atmospheric carbon reduction through direct CO2 injections. Simulated seawater chemistry changes and marine carbon storage effectiveness are similar to previous studies. As expected, by the end of the injection period avoided emissions fall short of the targeted 70 GtC by 16–30 % as a result of carbon cycle feedbacks and backfluxes in both land and ocean reservoirs. The target emissions reduction in the parameter perturbation simulations is about 0.2 and 2 % more at the end of the injection period and about 9 % less to 1 % more at the end of the simulations when compared to the unperturbed injection runs. An unexpected feature is the effect of the model's internal variability of deep-water formation in the Southern Ocean, which, in some model runs, causes additional oceanic carbon uptake after injection termination relative to a control run without injection and therefore with slightly different atmospheric CO2 and climate. These results of a model that has very low internal climate variability illustrate that the attribution of carbon fluxes and accounting for injected CO2 may be very challenging in the real climate system with its much larger internal variability.
    Type: Article , PeerReviewed
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  • 4
    Publication Date: 2024-06-26
    Type: Thesis , NonPeerReviewed
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  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-26
    Description: Two Polarstern expeditions were conducted in 1995 (ANT-XII/4) and 2001 (ANT-XVIII/5a) to the Bellingshausen Sea and Amundsen Sea and the suspected Eltanin meteorite impact in the SE-Pacific. A survey of the sediment distribution and its acoustic structure along the cruise track was performed. The seafloor topography was sampled using the multibeam sonar system Hydrosweep DS2 which operates on a frequency of 15.5 kHz. The resulting AWI Bathymetric Chart of the Eltanin Meteorite Impact Area is based on a Digital Terrain Model of this area. The mapping was performed using ArcGIS. The Eltanin impact area which covers the 4.100 m high Freden Seamount is visualized by one overview sheet of the scale 1:200,000 and four 1:100,000 subsheets.
    Keywords: ANT-XII/4; AWI_Paleo; Eltanin-impact-area; Eltanin Meteorite Impact Area, Freeden Seamount, SE-Pacific; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS35 06AQANTXII_4
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-26
    Description: During the fourth Antarctic voyage ANT-IV of the research icebreaker POLARSTERN standard meteorological measurements have been performed. The measurements include 3-hourly synoptic observations as well as daily upper air soundings. The measurements started on September 6 1985 at Bremerhaven and were terminated at April 28 1986 in Punta Arenas. The 3-hourly synoptic observations are performed following the instructions of the FM 13 ships code defined by the World Meteorological Organization (WMO). The datasets include automatic measurements such as mean ship's speed, wind velocity, wind direction, air temperature, water temperature as well as visual observations such as total cloud amount, present weather, clouds, height and period of swell waves, ice classification. The visual observation are not performed during night time. For the upper air soundings VAISALA RS80 radiosondes, carried by helium-filled balloons (TOTEX 350 - 1500) were used. Data reception and evaluation were carried out by a MicroCora System (VAISALA). The upper air soundings include profile measurements of pressure, temperature, relative humidity and wind vector. Usually the soundings started at the heliport (10 m above sea level) and terminated between 15 and 37 km. The height of the measurements was calculated by applying the barometric formula. The wind vector was determined with the aid of the OMEGA navigation system.
    Keywords: ANT-IV/1a; ANT-IV/1b; ANT-IV/1c; ANT-IV/2; ANT-IV/3; ANT-IV/4; AWI_Meteo; Canarias Sea; CT; Meteorological Long-Term Observations @ AWI; North Atlantic Ocean; North Sea; Polarstern; PS08; PS08/01331; PS08/01332; PS08/01333; PS08/01334; PS08/01335; PS08/01336; PS08/01337; PS08/01338; PS08/01339; PS08/01340; PS08/01341; PS08/01342; PS08/01343; PS08/01344; PS08/01345; PS08/01346; PS08/01347; PS08/01348; PS08/01349; PS08/01350; PS08/01351; PS08/01352; PS08/01353; PS08/01354; PS08/01355; PS08/01356; PS08/01357; PS08/01358; PS08/01359; PS08/01360; PS08/01361; PS08/01362; PS08/01363; PS08/01364; PS08/01365; PS08/01366; PS08/01367; PS08/01368; PS08/01369; PS08/01370; PS08/01371; PS08/01372; PS08/01373; PS08/01374; PS08/01375; PS08/01376; PS08/01377; PS08/01378; PS08/01379; PS08/01380; PS08/01381; PS08/01382; PS08/01383; PS08/01384; PS08/01385; PS08/01386; PS08/01387; PS08/01388; PS08/01389; PS08/01390; PS08/01391; PS08/01392; PS08/01393; PS08/01394; PS08/01395; PS08/01396; PS08/01397; PS08/01398; PS08/01399; PS08/01400; PS08/01401; PS08/01402; PS08/01403; PS08/01404; PS08/01405; PS08/01414; PS08/01415; PS08/01416; PS08/01417; PS08/01418; PS08/01419; PS08/01420; PS08/01421; PS08/01422; PS08/01423; PS08/01424; PS08/01425; PS08/01426; PS08/01427; PS08/01428; PS08/01429; PS08/01430; PS08/01431; PS08/01432; PS08/01433; PS08/01434; PS08/01435; PS08/01436; PS08/01437; PS08/01438; PS08/01439; PS08/01440; PS08/01441; PS08/01442; PS08/01443; PS08/01444; PS08/01445; PS08/01446; PS08/01447; PS08/01448; PS08/01449; PS08/01450; PS08/01451; PS08/01452; PS08/01453; PS08/01454; PS08/01455; PS08/01456; PS08/01457; PS08/01458; PS08/01459; PS08/01460; PS08/01461; PS08/01462; PS08/01463; PS08/01464; PS08/01465; PS08/01466; PS08/01467; PS08/01468; PS08/01469; PS08/01470; PS08/01471; PS08/01472; PS08/01473; PS08/01474; PS08/01475; PS08/01476; PS08/01477; PS08/01478; PS08/01479; PS08/01480; PS08/01481; PS08/01482; PS08/01483; PS08/01484; PS08/01485; PS08/01486; PS08/01487; PS08/01488; PS08/01489; PS08/01490; PS08/01491; PS08/01492; PS08/01493; PS08/01494; PS08/01495; PS08/01496; PS08/01497; PS08/01498; PS08/01499; PS08/01500; PS08/01501; PS08/01502; PS08/01503; PS08/01504; PS08/01505; PS08/01506; PS08/01507; PS08/01508; PS08/01509; PS08/01510; PS08/01511; PS08/01512; PS08/01513; PS08/01514; PS08/01515; PS08/01516; PS08/01517; PS08/01518; PS08/01519; PS08/01520; PS08/01521; PS08/01522; PS08/01523; PS08/1a-track; PS08/1b-track; PS08/1c-track; PS08/2-track; PS08/3-track; PS08/4-track; PS08 NOAMP; RADIO; Radiosonde; South Atlantic Ocean; Underway cruise track measurements
    Type: Dataset
    Format: application/zip, 191 datasets
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  • 7
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Berner, Heinrich (1991): Mechanismen der Sedimentbildung in der Framstrasse, im Arktischen Ozean und in der Norwegischen See. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 20, 167 pp, urn:nbn:de:gbv:46-ep000106655
    Publication Date: 2024-06-26
    Description: The grain size distribution and clay mineral composition of lithogenic particles of ice-rafted material, sinking matter, surface sediments, as well as from deep-sea cores are analysed. The samples were collected in the Fram Strait, the Arctic Ocean, and the Norwegian Sea during several expeditions with the research vessels "Polarstern", "Meteor" and "Poseidon", and Norwegian rearch vessels. Sinking matter was caught with sediment traps, fitted with timer-controlled sample changers, which had been deployde in the sea for usually one year.
    Keywords: 104-1; 109-1; 111-2; 114-1; 117-1; 120-1; 121-1; 122-2; 57-04; 57-06; 57-07; 57-08; 57-09; 57-11; 57-12; 57-13; 57-14; 57-20; 58-08; Arctic Ocean; ARK-I/3; ARK-II/4; ARK-II/5; ARK-III/3; ARK-IV/3; BC; BI-1_trap; Box corer; Fram Strait; FS-1_trap; FS-2_trap; FS-3_trap; GC; GeoB; Geosciences, University of Bremen; Giant box corer; GIK16103-1; GIK16104-1; GIK16105-1; GIK16109-1; GIK16122-1; GIK16129-1; GIK16131-1; GIK16132-1; GIK16133-1; GIK16135-1; GIK16136-1; GIK16138-1; GIK16139-1; GIK16143-1; GIK16144-1; GIK16145-1; GIK16146-1; GIK16147-1; GIK16149-1; GIK16150-1; GIK16152-1; GIK16156-1; GIK16157-1; GIK16158-1; GIK16161-1; GIK16162-1; GIK16163-1; GIK16167-1; GIK16168-1; GIK16169-1; GIK16170-1; GIK16172-1; GIK16175-1; GIK16176-1; GIK16180-1; GIK21289-1 PS07/578; GIK21290-3 PS07/579; GIK21291-3 PS07/581; GIK21292-3 PS07/582; GIK21293-3 PS07/583; GIK21294-3 PS07/584; GIK21295-3 PS07/586; GIK21295-5 PS07/586; GIK21296-3 PS07/587; GIK21297-3 PS07/588; GIK21298-3 PS07/590; GIK21300-3 PS07/592; GIK21301-2 PS07/593; GIK21302-2 PS07/594; GIK21303-2 PS07/595; GIK21305-1 PS07/597; GIK21306-2 PS07/598; GIK21307-2 PS07/599; GIK21308-3 PS07/601; GIK21309-3 PS07/602; GIK21310-4 PS07/603; GIK21311-3 PS07/605; GIK21312-3 PS07/606; GIK21314-3 PS07/608; GIK21316-5 PS07/612; GIK21318-4 PS07/615; GIK21319-2 PS07/617; GIK21322-3 PS07/626; GIK21323-3 PS07/627; GIK21513-8 PS11/276-8; GIK21514-5 PS11/278-5; GIK21515-10 PS11/280-10; GIK21516-5 PS11/282-5; GIK21518-13 PS11/287-13; GIK21519-10 PS11/296-10; GIK21520-10 PS11/310-10; GIK21521-13 PS11/340-13; GIK21522-18 PS11/358-18; GIK21523-14 PS11/362-14; GIK21524-1 PS11/364-1; GIK21525-2 PS11/365-2; GIK21528-7 PS11/372-7; GIK21529-7 PS11/376-7; GIK21530-3 PS11/382-3; GIK21532-1 PS11/396-1; GIK23055-1; GIK23056-2; GIK23057-1; GIK23058-1; GIK23059-1; GIK23060-1; GIK23061-3; GIK23062-2; GIK23063-1; GIK23064-2; GIK23065-1; GIK23066-1; GIK23067-2; GIK23068-1; GIK23069-1; GIK23070-2; GIK23071-1; GIK23072-1; GIK23073-2; GIK23074-2; GIK23126-1 PS03/126; GIK23138-1 PS03/138; GIK23150-1 PS03/150; GIK23189-1 PS03/189; GIK23206-1 PS03/206; GIK23207-1 PS03/207; GIK23210-1 PS03/210; GIK23211-1 PS03/211; GIK23216-1 PS03/216; GIK23217-1 PS03/217; GIK23220-1 PS03/220; GIK23221-1 PS03/221; GIK23222-1 PS03/222; GIK23229-1 PS05/414; GIK23230-1 PS05/416; GIK23231-2 PS05/417; GIK23232-1 PS05/418; GIK23233-1 PS05/420; GIK23235-1 PS05/422; GIK23240-1 PS05/428; GIK23241-1 PS05/429; GIK23243-2 PS05/431; GIK23244-1 PS05/449; GIK23247-2 PS05/452; GIK23248-1 PS05/453; GKG; Gravity corer; Gravity corer (Kiel type); Håkon Mosby; HM52; HM52-02; HM57; HM57-04; HM57-05; HM57-06; HM57-07; HM57-08; HM57-09; HM57-11; HM57-12; HM57-13; HM57-14; HM57-20; HM58; HM58-02; HM58-08; HM82/83; ICE; Iceland Sea; Ice station; LB-1_trap; Lofoten Basin; M107-1; M118-1; M2/2; Meteor (1986); Mooring (long time); MOORY; Na-1_trap; Nansen Basin; NB-1_trap; Norway Slope; Norwegian Sea; Polarstern; PS03; PS05; PS07; PS1050-1; PS1060-1; PS1071-1; PS11; PS11/269-1; PS1105-1; PS1120-2; PS1121-1; PS1124-1; PS1125-1; PS1127-1; PS1128-1; PS1130-1; PS1131-1; PS1132-1; PS1229-1; PS1230-1; PS1231-2; PS1232-1; PS1233-1; PS1235-1; PS1240-1; PS1241-1; PS1243-2; PS1244-1; PS1247-2; PS1248-1; PS1289-1; PS1290-3; PS1291-3; PS1292-3; PS1293-3; PS1294-3; PS1295-3; PS1295-5; PS1296-3; PS1297-3; PS1298-3; PS1300-3; PS1301-2; PS1302-2; PS1303-2; PS1305-1; PS1306-2; PS1307-2; PS1308-3; PS1309-3; PS1310-4; PS1311-3; PS1312-3; PS1314-3; PS1316-5; PS1318-4; PS1319-2; PS1322-3; PS1323-3; PS1511-1; PS1513-8; PS1514-5; PS1515-10; PS1516-5; PS1518-13; PS1519-10; PS1520-10; PS1521-13; PS1522-18; PS1523-14; PS1524-1; PS1525-2; PS1528-7; PS1529-7; PS1530-3; PS1532-1; Quaternary Environment of the Eurasian North; QUEEN; Sea_Ice_A; Sea_Ice_B; Sea_Ice_C; Sea_Ice_D; SL; SP-1; SP-1_trap; Svalbard; Trap, sediment; TRAPS; Voering Plateau; Voring Plateau; VP-2_trap; Western Djupet
    Type: Dataset
    Format: application/zip, 18 datasets
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  • 8
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Wollenburg, Jutta Erika; Mackensen, Andreas; Kuhnt, Wolfgang (2007): Benthic foraminiferal biodiversity response to a changing Arctic palaeoclimate in the last 24.000 years. Palaeogeography, Palaeoclimatology, Palaeoecology, 255(3-4), 195-222, https://doi.org/10.1016/j.palaeo.2007.05.007
    Publication Date: 2024-06-26
    Description: Four sediment cores recovered from 1000 to 2500 m water depth in the Arctic Ocean, tracing the inflowing Atlantic water from Fram Strait, Yermak Plateau, northern Barents Sea continental slope as far as the Laptev Sea, have been analyzed for species richness and diversity. Samples were wet sieved after freeze-drying using a 63-µm sieve. Where possible at least 300 specimens were counted from the size fraction 〉63 µm, however, samples from deglacial periods are often affected by carbonate dissolution. In such samples foraminiferal numbers are low. Samples containing less than 40 specimens were excluded from statistical analyses. Because we are aware that specimen numbers 〈100 specimen are still critical for H analyses, core sections containing less than 100 specimens are highlighted in the figures. Here, we will characterize biodiversity trends by the two most widely used biodiversity measurements, the information function H (Buzas and Gibson, 1969) with its decomposition equation ln(S) and ln(E) (Buzas and Hayek, 1996), and the Fisher Alpha Index (Fisher, Corbett, and Williams, 1943). For spectral analysis the Fisher alpha record of core PS2837-5 was resampled at equally spaced 100-year intervals. For the spectral analysis, two methodes were used within the ANALYSERIES software package (Paillard et al., 1996): 1. The Blackman-Tuckey (1958) for its high confidence of the results; 2. The maximum entropy method (e.g. Haykin, 1983) for its high resolution. The cores reveal well-correlated biodiversity maxima and minima. Distinct periodicities of species richness variability of 1.57 kyr and 0.76 kyr characterize the Late Weichselian, and of 1.16 kyr and 0.54 kyr even more pronounced the Holocene. The biodiversity maxima/minima coincide with terrestrial and marine warm and cool events at high northern latitude. We suggest that either the physiology of most rare species is temperature sensitive, or sustained food supply increased the taxonomic richness during warmer intervals.
    Keywords: ARK-III/3; ARK-IX/4; ARK-VIII/3; ARK-XIII/2; AWI_Paleo; Fram Strait; GIK21290-4 PS07/579; Gravity corer (Kiel type); KAL; Kasten corer; Laptev Sea; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Polarstern; PS07; PS1290-4; PS19/245; PS19 ARCTIC91; PS2212-3; PS2458-4; PS27; PS27/038; PS2837-5; PS44; PS44/065; SL; Yermak Plateau
    Type: Dataset
    Format: application/zip, 8 datasets
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  • 9
    Publication Date: 2024-06-26
    Description: Not filtered water samples were taken in 10 ml ampoules (sealed immediately after being acidified with phosphoric acid to pH〈2, sampling), or 40 ml screw-lid vials, and measured onboard at sampling or next days, or frozen (-20°C) until being acidified and measured in home labs. Carbon measurement was by high-temperature catalytic oxydation in a 10 cm column packed with 5% Pt on aluminum oxide beads at 900°C in a stream of oxygen, and CO2 detection by infrared extinction after the removal of moisture and SO2 by appropriate traps (cold trap, Mg-percarbonate, Na-pyrophosphate, tin, bronze or Sulfix). The apparatus was the dual channel Dimatek 2000 equipped with a Binos 200 detector. Nitrogen was measured by chemoluminescence detection of NO2 in the combustion gases after leaving the Binos detector in one of the two channels of the setup. Most measurements of samples containing high nitrate were discarded, when data were inconsistent. The nature of nitrate interference is not clear.
    Keywords: AL79A; AL79A_BY38; AL79A_F1; AL79A_F10; AL79A_F11; AL79A_F14; AL79A_F19; AL79A_F2; AL79A_F20; AL79A_F22; AL79A_F23; AL79A_F3; AL79A_F4; AL79A_F5; AL79A_F7; AL79A_F8; AL79A_F9; AL79A_S21; Alkor (1990); Baltic Sea; Bottle, Niskin 10-L; NIS_10L
    Type: Dataset
    Format: application/zip, 17 datasets
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  • 10
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Zühlsdorff, Christine; Hanebuth, Till J J; Henrich, Rüdiger (2008): Persistent quasi-periodic turbidite activity off Saharan Africa and its comparability to orbital and climate cyclicities. Geo-Marine Letters, 28(2), 87-95, https://doi.org/10.1007/s00367-007-0092-0
    Publication Date: 2024-06-26
    Description: Based on a high-resolution sediment record from a submarine meandering canyon system offshore the present-day hyperarid Saharan Africa, two phases of turbidity-current activity can be distinguished during the past 13,000 years. Frequent, siliciclastic turbidity currents can be related to deglacial sea-level history, whereas rhythmically recurring fine-grained and carbonate-rich turbidity currents with recurrence times of roughly 900 years are inferred for the Holocene. Various trigger mechanisms can be considered to initiate turbidity currents, but only a few can explain a periodic turbidite activity. A comparison of Holocene turbidite recurrence times and basic cycles of 900 and 1,800 years found in various Holocene paleoclimate studies suggests that a previously unrecognized climate-related coupling may be active.
    Keywords: Center for Marine Environmental Sciences; GeoB8509-2; Gravity corer (Kiel type); M58/1; MARUM; Meteor (1986); SL
    Type: Dataset
    Format: application/zip, 4 datasets
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