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  • 1
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    Elsevier
    In:  Signal Processing, Tokyo, Elsevier, vol. 8, no. 1, pp. 401-413, pp. L16603
    Publication Date: 1985
    Keywords: Spectrum ; Maximum likelihood
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  • 2
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    Elsevier
    In:  Amsterdam, Elsevier, vol. 12, pp. 225, (ISBN 3-7643-7011-4)
    Publication Date: 1985
    Keywords: Textbook of geophysics ; Seismics (controlled source seismology) ; seismic Migration ; Acoustics ; Wave propagation ; Waves
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  • 3
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    Springer
    In:  New York, Springer, vol. 7, no. Publ. No. 12, pp. 127, (ISBN 3-540-44363-0)
    Publication Date: 1985
    Keywords: Stress ; Borehole geophys. ; Seismicity ; Tectonics ; FROTH, ; RUB ; GMG
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  • 4
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    Springer
    In:  Professional Paper, Observation of the Continental Crust Through Drilling I., Berlin, Springer, vol. 1, no. 231, pp. 324-342, (ISBN: 3-540-23712-7)
    Publication Date: 1985
    Keywords: Stress ; Borehole geophys. ; Seismicity ; Tectonics
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  • 5
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    Springer
    In:  Heidelberg, Springer, vol. V/2, no. Subvol. b, pp. 220, (ISBN: 0-08-037951-6)
    Publication Date: 1985
    Keywords: Review article ; Seismology ; (The Earth's free) oscillations ; Waves ; Gravimetry, Gravitation ; Geomagnetics ; Planetology ; solar ; system ; Bosum ; Busse ; Chapman ; Gierloff-Emden ; Haak ; Hagedorn ; Jacoby ; Lubinova ; Rucher ; Roeser ; Schmucker ; Soffel ; Stacey ; Voppel
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  • 6
    Publication Date: 2017-07-10
    Description: A total of 131 current meter records of between 6 and 24 month duration are analysed to describe the deep flow field of the eastern North Atlantic from 19° to 54°N and from the Continental Slope to the Mid Atlantic Ridge. Mean flows are weak and may be statistically indeterminate in some records and locations, but appear to indicate cyclonic circulations around the Iberia and Porcupine abyssal plains with a generally southward flow along the Mid Atlantic ridge and a deep northward slope current (where measurements exist) along the eastern boundary. The deepest inflow to the north-eastern basin that has been identified to date takes place through the Discovery Gap of 〉4,700 m sill-depth at 37° 25′N 15° 45′W in the Azores-Portugal ridge. South of that ridge, observations are sparse and no systematic circulation is yet evident. These observations are discussed in relation to recent geostrophic estimates of the deep circulation.
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  • 7
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    Springer
    In:  In: Submarine Fans and Related Turbidite Systems. Springer, New York, pp. 71-78. ISBN 978-1-4612-9570-9
    Publication Date: 2018-01-19
    Description: The Magdalena Fan can be divided into: upper fan—1:60–1:110 gradients, channels with well-developed levees, generally several subbottom reflectors on 3.5-kHz records, and fine-grained sediments; middle fan—1:110–1:200 gradients, channels with very subdued levees, several to few sub- bottom reflectors on 3.5-kHz records, and chaotic and discontinuous reflections on multichannel seismic (MCS) records; lower fan—1:250 gradients, small channels and relatively smooth seafloor, generally coarsegrained sediments, few or no subbottom reflectors on 3.5-kHz records, and flat continuous reflections on MCS records. In addition to the turbidity currents, slumping along the continental slope and elsewhere also influenced sedimentation in the fan.
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  • 8
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    Elsevier
    In:  Quaternary Science Reviews, 4 (4). pp. 215-278.
    Publication Date: 2020-06-04
    Description: Molluscan fossils collected from shallow water marine sediment across NW Europe and nearby Arctic regions have been analysed for the extent of isoleucine epimerization (DL ratio) in indigenous protein residues. The DL ratios confirm that essentially all ‘classical’ Eemian sites from NW Europe are of the same age, and are correlative with the type locality near Amersfoort in the Netherlands; shells from interglacial marine sediment beneath the type Weichselian till in Poland also correlate with the type Eemian site. DL ratios in Holsteinian marine shells (0.29) are substantially higher than in their Eemian counterparts (0.17); ‘Late Cromerian’ shells yield even higher ratios (0.46). DL ratios in late glacial shells (0.06) and Middle Weichselian shells (0.09) permit differentiation from modern (0.01) and last interglacial material. Based on the position of the Matuyama-Brunhes boundary and the differences in DL ratios, the Eemian must correlate with isotope substage 5e, whereas the Holsteinian is most likely substage 7c, possibly stage 9 but certainly younger than stage 11. Intra-Saalian warm periods may be terrestrial equivalents of the younger substages of stage 7. Extensive pre-Eemian marine sediments along the SW coast of Denmark previously correlated with the Holsteinian are shown to be of ‘Late Cromerian’ age. The underlying till there is the first widespread evidence of a pre-Elsterian till in NW Europe. DL ratios in molluscs from last interglacial sites along the Arctic coast of the USSR, the Arctic Islands and eastern Greenland are substantially lower than in their European counterparts due to their low thermal histories. The combined mid- and high-latitude data are used to develop a predictive model for the expected DL ratio in any of several moderate epimerization-rate taxa for last interglacial sites with mean temperatures between −20 and +15°C. Not all sites could be unambiguously assigned to an established interglacial. The Fjøsanger (Norway) and Margareteberg (Sweden) sites previously thought to be Eemian, yield DL ratios higher than in secure nearby Eemian material. It is yet unresolved whether these are aberrant sites or if they predate the last interglacial. In situ shoreline deposits encountered in borings in SW Belgium and in exposures on the Belgium coastal plain contain molluscs that yield DL ratios intermediate between secure Eemian and Late Weichselian ratios, raising the possibility that a late stage 5 high-sea-level event attained near-modern levels in the southern North Sea basin. Resolution of these uncertainties is the focus of future work.
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  • 9
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    Elsevier
    In:  Elsevier, Amsterdam, 294 pp. ISBN 0-444-42471-7
    Publication Date: 2019-08-28
    Type: Book , NonPeerReviewed
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  • 10
    Publication Date: 2016-01-22
    Description: The lipopolysaccharides of Rhodobacter sulfidophilus and the two budding species Rhodopseudomonas acidophila and Rhodopseudomonas blastica were isolated and chemically analyzed. The all have a lipid A backbone structure with glucosamine as the only amino sugar. The lipid A's of Rb. sulfidophilus and Rps. blastica contain phosphate, their fatty acids are characterized by ester-linked, unsubstituted 3-OH-10:0 and amide-linked 3-OH-14:0 (Rb. sulfidophilus) or 3-oxo-14:0 (Rps. blastica). Lipid A of Rps. acidophila is free of phosphate and contains the rare 3-OH-16:0 fatty acid in amide linkage. The lipopolysaccharides of all three species contain 2-keto-3-deoxy-octonate (KDO) but are devoid of heptoses. Neutral sugars with the exception of glucose are lacking in the lipopolysaccharide of Rb. sulfidophilus. This shows a high galacturonic acid content. The lipopolysaccharides of Rps. acidophila and Rps. blastica have neutral sugar spectra indicative for typical O-chains (rhamnose, mannose, galactose, glucose in both species, and in Rps. blastica additionally 2-O-methyl-6-deoxy-hexose). The taxonomic value of the data is discussed.
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  • 11
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    Springer
    In:  Paläontologische Zeitschrift, 59 (1-2). pp. 15-33.
    Publication Date: 2018-01-25
    Description: A concept explaining biocalcification as a form of calcium detoxification is advanced using geochemical and paleontological criteria. The first appearence of calcareous skeletons at the turn of the Precambrian/Cambrian is interpreted as a biotic response to a gradual rise of Ca2+ in world ocean resulting in Ca2+ stress environments in shelf areas. Periodic appearance in the Phanerozoic record of heavily calcified marine biota, absent or relic in modern seas, suggests considerable temporal fluctuations of calcium concentrations in the ancient ocean. Temporal changes in Ca2+ and mineral nutrient contents in the environment can thus be seen as overriding factors in the evolution of organisms.
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  • 12
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    Springer
    In:  In: Observation of the Continental Crust Through Drilling I : proceedings of the international symposium held in Tarrytown, May 20-25, 1984. , ed. by Raleigh, C. B. Exploration of the deep continental crust . Springer, Berlin (u.a.), pp. 6-15. ISBN 3-540-15873-1 ; 0-387-15873-1
    Publication Date: 2015-03-02
    Description: For most earth scientists outside the USSR, plans for deep continental crustal drilling seem unrealistic. It will be even harder to convince money-spending organizations or personalities of their feasability. Therefore, we ourselves should continually have in mind an introduction to lectures that Patrick Winston from MIT uses to sell Artificial Intelligence: "If you are a skeptic, I want to make you a believer - and if you are a believer, I want to make you a skeptic."
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  • 13
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    Elsevier
    In:  Journal of Volcanology and Geothermal Research, 25 . pp. 193-224.
    Publication Date: 2017-07-19
    Description: Small-volume (ca. 0.6 km3) pyroclastic flow deposits at Laacher See contain lithic breccias and two types of ground layers that differ significantly in their structure and composition from the main body of flow units. Lithic breccia bodies, up to 3.5 m thick, containing up to 85 weight% lithic blocks, occur locally at various distances from the vent. The deposition of these breccias was apparently governed by the strong influence of paleomorphology on the dynamics of the pyroclastic flows. The breccias were deposited at three main changes in bottom gradient along the path of the pyroclastic flows. The accumulation of large lithics is explained: (a) by compression of flows on the rising bottom close to the vent; (b) by thinning of flows accelerating over a steep incline; (c) by deceleration of the pre-concentrated lower part of flows in hydraulic jumps; and (d) possibly by a stationary vortex at the inner bend of a valley curvature. Poorly sorted lithic-rich ground layers, laterally highly variable in internal structure and composition, are restricted to marginal regions of the pyroclastic flow deposits within deep and narrow valleys. They are interpreted as having formed due to the extreme roughness of the valley walls, enforcing irregular turbulent flow and intense fluidization of the flow head, in which density-dominated segregation of lithics occurred. Wellsorted lapilli-rich ground layers of constant lateral thickness were probably generated by a more regularly moving, less intensely fluidized head of pyroclastic flows in which size-dominated segregation was effective but density-segregation was minor. A model of the temporal and longitudinal evolution of a flow head is proposed. Close to the vent, the head is exclusively erosive. With increasing distance, erosive power declines and erosion is paralleled by ground layer formation under strong fluidization. Further from the vent, the head ceases to erode while fluidization is still sufficient for ground layer formation. When fluidization declines to a level ineffective for segregation, ground layers terminate while the head advances and only terminates when plug-flow dominates.
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  • 14
    Publication Date: 2020-03-20
    Description: A multi-pond saltern that creates a gradient of salt concentrations has been studied with respect to some characteristics of the resulting environments and their microbial populations. The increase in salt concentration was correlated with increase in diurnal temperature and biomass present and with decrease in oxygen concentrations. Many types of organisms below 15% (w/v) total salts, were found, many of them normal inhabitants of seawater and even freshwater. Most organisms over 15% salts were halophilic. The salt concentrations comprised two ranges, each characterized by different microbial populations. First, between 15 and 30% salts, the populations ofDunaliella increased, reaching large numbers; moderately halophilic eubacteria and some fast-growing halobacteria predominated as heterotrophic microorganisms and, among the first, thePseudomonas-Alteromonas-Alcaligenes group andVibrio were the more abundant taxonomic groups; and gram-positive cocci appeared mainly over 25% salts. Phototrophic bacteria, both oxygenic and anoxygenic, were also found in this range, and among the anoxygenic type,Chromatium species andRodospirillum salexigens were probably predominant. Second, over 30% salts the diversity decreased greatly, all organisms found at the lower salt concentrations disappeared, and instead large populations of halobacteria developed. Over 50% salts, only three species of halobacteria were found.
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  • 15
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    Springer
    In:  In: Antarctic Nutrient Cycles and Food Webs. , ed. by Siegfried, W. R., Condy, P. R. and Laws, R. M. Springer, Berlin, Germany, pp. 551-554. ISBN 978-3-642-82277-3
    Publication Date: 2020-06-11
    Description: The Sub-Antarctic Fur Seal, Arctocephalus tropicalis, at Gough Island preys predominantly on cephalopods, but includes relatively small quantities of fish in its diet. Stomachs of Fur Seals (n = 220) culled on land were either empty (32%), contained only stones (8%) or contained almost exclusively prey remains resistant to digestion, such as cephalopod pens, ‘beaks’, eye balls, fish bones and otoliths. The pooled cephalopod lower beaks (n = 424) that could be identified (n = 337), showed that Ommastrephidae (52.5%), Histioteuthidae (25.2%), Onychoteuthidae (19.9%), Cranchiidae (2.1%) and Octopoteuthidae (0.3%) constituted the main prey items based on frequency of occurrence. Cephalopod mass estimates, from regression of lower rostral lengths against mass, approximated this relative arrangement of cephalopod families.
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  • 16
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    Springer
    In:  Deutsche Hydrographische Zeitschrift, 38 (1). pp. 7-22.
    Publication Date: 2016-11-02
    Description: Current data obtained from 7 moorings in the Northeast Atlantic in the course of many years are analysed with respect to semi-diurnal barotropic and baroclinic tides and diurnal barotropic tides. For semi-diurnal tides M2 and S2 the energy distribution is usually dominated by the barotropic mode; only in a few cases does the first-order baroclinic mode contain higher energy. Barotropic tidal ellipse orientations are found to be consistent with results from earlier tide gauge observations in this area. Significant deviations occur, however, in amplitudes. Results for the diurnal component K1 are also presented. With few exceptions, tides are found to be progressive waves in this area. The current ellipse pattern is similar to results obtained indirectly by Cartwright, Edden, Spencer et al. [1980] from tide gauge observations.
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  • 17
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    Elsevier
    In:  Tectonophysics, 115 (1-2). pp. 101-129.
    Publication Date: 2018-01-17
    Description: Plastically deformed quartzites from the Betic Movement Zone (Betic Cordilleras, Spain) exhibit microstructures indicative of crystal plasticity on a mineral grain scale. Quartzites with dynamically recrystallized grain sizes larger than 10 μm have strong crystallographic preferred orientations, narrow grain boundaries, little creep damage, and an inverse proportionality of dislocation density and grain size. Mylonites with grain sizes smaller than 10 μm have low crystallographic preferred orientations, wide grain boundaries (up to 1000 Å), abundant creep damage, and decreasing dislocation density with diminishing grain size. This is thought to reflect a clear-cut shift in deformational regimes from dislocation creep to superplastic flow at 10 μm grain size. Superplasticity can be acquired by quartzites which suffer dynamic recrystallization to grain sizes smaller than 10 μm during an initial dislocation creep stage. Dislocation motion is the major accomodating mechanism for strain incompatibilities that arise during grain-boundary sliding in the mylonites.It seems reasonable to estimate flow stresses from unbound dislocation densities and dynamically recrystallized grain sizes in the tectonite specimens. In the mylonites, dynamically recrystallized grain size probably reflects the stress magnitude before the shift in deformational mechanisms, and an estimate for late stage stresses is provided by unbound dislocation densities. In both deformational regimes the flow strength appears to depend on the extent of dynamic recrystallization.
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  • 18
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    Springer
    In:  Marine Biology, 85 (3). pp. 313-322.
    Publication Date: 2019-02-27
    Description: Fishes and zooplankton were obtained (March-April 1979 and partly in August 1974) from 45 hauls taken during the day and at night in the central equatorial Atlantic between Latitude 3 ~ and 2 ~ from the surface to 1250-m depth, using the RMT 1+8, a combined opening-closing plankton and micronekton trawl. The vertical distribution of 30 myctophid species is described. All species migrate in a diel pattern, Ceratoscopelus warmingii and Lampanyctus photonotus down to at least 1250 m. During daytime most species aggregated at 400- to 700-m depth, therefore only partly occupying the depth of the Deep Scattering Layer (400 to 500 m at 15 kHz). The feeding patterns of seven of the most abundant species were compared, with a total of 1 905 stomach contents being analysed. All seven species are regarded as opportunistic predators, which feed predominantly during the night on calanoid copepods. A total of 66 species of calanoid copepods were identified among the prey items, with smaller species definitely being in the minority. Stomachs of C. warmingii (700 to 1 250 m depth) and Lepidophanes guentheri (500 to 900 m depth) from daytime samples contained copepod species restricted to the upper 150 m of the water column, including Undinula vulgaris, Nannocalanus minor, and Euchaeta marina, thereby confirming an extended vertical migration of predators. Differences in diet and preferences between species in their total food spectrum are described.
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  • 19
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    Elsevier
    In:  Progress in Oceanography, 14 . pp. 231-257.
    Publication Date: 2016-05-10
    Description: Hydrographic data from two cruises in the Canary Basin (Meteor 57, July 1981; Poseidon 86, April 1982) are analysed with respect to current distribution and lateral heat flux in the Azores-Madeira region. The first part of the data base consists of long transects of XBT and G.E.K. measurements between Cape Finisterre (North West Spain) and the northern Canary Basin, where several year-long current meter records exist. Further information is obtained by thermosalinograph surface data and by expendable current profilers (XCP). Geostrophic currents are derived from XBT profiles, using the tight temperature-salinity relationship in the depth range of the Warmwassersphäre. The results compare well with the G.E.K. and XCP current observations. The second part consists of CTD data from an eddy resolving, box-shaped CTD survey (500 × 500 km2) centered at the mooring location (33°N, 22°W), The observations are supplemented by satellite-buoy trajectories. Horizontal parameter distribution is shown in terms of objectively contoured maps. Bands of spatially enhanced energetic structures, seen in the long transects are further resolved by the box survey as a deep jet-like current system cross the Canary Basin in a west-east direction. Associated with this Azores Current is a frontal zone with near-surface temperature and salinity steps of order 2 K and 0.3 practical salinity units. The dynamic topography field can be decomposed into a linear background field, a Rossby wave and a mesoscale eddy field. We find that major contributions to the meridional eddy heat flux are confined to the vicinity of the Azores current frontal zone. It is shown that the principal balance in the temperature equation is between heating by the mean horizontal advection terms and cooling by the eddy flux divergence.
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  • 20
    Publication Date: 2020-07-14
    Description: Adult Sepia officinalis L. were caught in June 1984, in the coastal waters of Wimereux (France). Deposition of the eggs took place in the seawater aquaria of the “Station Marine”. The oxygen consumption of S. officinalis was measured during embryonic and juvenile development. Aerobic metabolism occurs as soon as the early embryonic Stage 21. Oxygen diffuses through the initially thick egg shell; the oxygen level in the perivitelline liquid reaches a maximal value just before hatching (116.7±6.9 mm Hg). Hatchings display only a slight increase in oxygen consumption compared to embryos in the last stage of development. Respiration experiments with 40 d old juveniles showed that oxygen consumption increases with temperature, but is not affected by photoperiod. Experiments under increasing hypoxia revealed that S. officinalis juveniles are good regulators and maintain a constant oxygen consumption in the range of 4 to 7 mg O2l-1. Juveniles successfully recover from an hypoxic stress of 2 mg O2l-1 maintained for 1 h. This suggests that the respiratory pigments (pre-hemocyanins) of 40 d-old juveniles have a high oxygen affinity and/or that these juveniles have the ability to adapt to anaerobic conditions.
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  • 21
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    Springer
    In:  Marine Biology, 86 (2). pp. 199-202.
    Publication Date: 2020-07-14
    Description: Cephalopod remains were collected from all of 12 dead Emperor penguin chicks [Aptenodytes forsteri (Gray)], from 76% of 29 living adult Emperor penguins, and from 18% of 105 living adult Adelie penguins [Pygoscelis adeliae (Hombron & Jacquinot)] from Adelie Land, Antarctica, in 1982. Of the seven species of squids represented by lower beaks, Psychroteuthis glacialis comprised 88% of the number in both Emperor chicks and Emperor adults and 100% in Adelie adults. From estimates of the weight of squids represented by lower beaks, Gonatus antarcticus and Kondakovia longimana contributed 18 and 14%, respectively, of the weight of squids in the diet of Emperor chicks and 27 and 21%, respectively, in the diet of Emperor adults. The data suggest that Psychroteuthis glacialis probably hatch in July-September and grow steadily for one year, and then spawn and die.
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  • 22
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    Elsevier
    In:  In: Coupled Ocean-Atmosphere Models. , ed. by Nihoul, J. C. Elsevier Oceanography Series, 40 . Elsevier, Amsterdam, pp. 63-81.
    Publication Date: 2019-08-08
    Description: A primitive equation equatorial model has been developed to study climate variability due to wind and thermodynamic forcing in an equatorial region. The model basin extends from 30° S to 30° N and zonally over 140°, has a variable horizontal resolution (50–800 km) and 13 vertical levels. Experiments are performed with observed annual cycle as well as 32 years of observed bimonthly wind data. A preliminary analysis of these experiments shows that the model is capable of simulating the basic pattern of annual as well as interannual variability of the Pacific Ocean. In particular, the model response shows evidence of the major El Niños which occurred between 1947 and 1978.
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  • 23
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    Springer
    In:  Estuaries, 8 (2A). pp. 145-157.
    Publication Date: 2019-02-27
    Description: Over the past decade, the annual cycle of the major pelagic processes in relation to environmental factors and species composition of the plankton has been studied intensively at a fixed station in Kiel Bight. A series of sequential phases, differentiated according to characteristic properties, succeed each other in a recurring pattern each year. The following phases have been differentiated: the spring diatom bloom, the late spring copepod maximum, the summer stratification, the fall blooms and the winter dormancy. Each phase represents a particular pattern of biogenous element cycling, both within the pelagic system and between the pelagic and benthic systems. Each phase is also characterized by a spectrum of dominant species, many of which do not recur each year. Greatest variation is found amongst bloom diatoms, whereas large, slow-growing species such as the Ceratia and most metazooplankton are highly recurrent. Variation in species composition is not related to long-term trends since the past century, in spite of the considerable increase in anthropogenic nutrient input to the Bight. Short-term events appear to determine occurrence of fast-growing species, many of which have benthic resting stages in their life histories. It is concluded that more attention should be paid to life history strategies of species if the mechanisms of seasonal succession are to be elucidated. Long-term observations on appearance or absence of the various species in relation to environmental properties can provide clues as to the nature of these life history strategies.
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  • 24
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    Springer
    In:  Oecologia, 67 (2). pp. 255-259.
    Publication Date: 2020-06-16
    Description: Every summer the deepest parts of the inner Flensburg fjord are subject to O2-deficiency lasting from a few weeks to several months. In spring, however, populations of Metridium senile can be found in these areas, in spite of the fact that frequently the local anoxic period of the previous summer has been 2–3 times longer than their anoxia LD50-value (3 wks). Responsible for this phenomenon is an intensive recolonization by adult Metridium during autumn and winter. This process has been investigated in an 8 months monitoring from May to December 1981. Results on the recolonization mechanism, the population structure of immigrating anemones and recolonization rate as a function of available hard substratum are presented.
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  • 25
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    Elsevier
    In:  In: Coupled ocean-atmosphere models. Elsevier Oceanography Series, 40 . Elsevier, Amsterdam, The Netherlands, pp. 543-590. ISBN 0-444-42486-5
    Publication Date: 2020-08-03
    Description: The potential vorticity profile in the seasonal pycnocline can be predicted from the surface buoyancy and momentum fluxes by means of the Lagrangian correlation of seasonally varying mixed-layer depth and density. Water flows geostrophically from the seasonal pycnocline into the permanent pycnocline, through the sloping surface of depth D defined by the annual maximum depth of the mixed layer. Potential vorticity flows into the permanent pycnocline where U(D)· ∇D ≤W(D) and vice versa. A theory is given for the regional variation of D, and methods of determining D from hydrographic data are reviewed. This physical understanding of potential vorticity sources and sinks makes it possible to reformulate ventilated thermocline models in terms of flux rather than density boundary conditions, and guides the design of coupled models of ocean—atmosphere circulation. It leads to formulae for water-mass formation and the nutrient balance in the seasonal boundary layer.
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  • 26
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    Springer
    In:  In: The Great American Biotic Interchange. , ed. by Stehli, F. G. S. and Webb, D. Springer, Boston, MA, pp. 3-16.
    Publication Date: 2019-07-03
    Description: Complex problems seem to have a way of becoming increasingly complex as we learn more, recognize new variables, and appreciate the labyrinthine nature of interactions. When we learn to deal with them as large-scale systems, however, models can be posited and tested, and it becomes possible to move from an observational-analytical approach to one allowing a certain degree of experimentation.
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  • 27
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    Springer
    In:  In: The Great American Biotic Interchange. , ed. by Stehli, F. G. and Webb, D. Springer, Boston, MA, pp. 17-48.
    Publication Date: 2019-07-03
    Description: Any reconstruction of the geological history of the Central America land bridge is dependent on conjectural motions of several lithospheric plates. The most important aspect of a timing sequence for a link between the North and South America land masses is apparently the creation of the Caribbean Plate. The geological record, however, which details a tectonic evolution of the Caribbean Plate and its margins is so enigmatic that many critical questions remain unresolved, and every developed model is couched in some incompatibilities.
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  • 28
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    Springer
    In:  In: The Great American Biotic Interchange. , ed. by Stehli, F. G. and Webb, S. D. Springer, Boston, MA, pp. 89-121.
    Publication Date: 2019-07-02
    Description: The reconstruction of Caribbean plate history is an uncertain task, but a task that has intrigued generations of geologists. Each worker has turned to the task of historical interpretation influenced by a particular set of experiences or a special approach, and the results have been accordingly varied. A complete history of interpretations would form the subject of a fascinating chapter in the history of geological philosophy, but such is not the purpose of this chapter. Instead, I will dwell on a set of data that call for what I believe to be a relatively conservative view of Cretaceous and Tertiary plate history. My own interpretation is based heavily on my own or my students’ field experiences in the northeastern West Indies, Guatemala, Belize, and Venezuela, as well as extensive field excursions in Hispaniola, Jamaica, the Lesser Antilles, Central America, and the Dutch Antilles. I am further heavily influenced by the results of the Deep Sea Drilling Project (DSDP), Leg 15, which produced information of fundamental interest in the Venezuelan and Colombian Basins, and by several dissertations of the Princeton University group in northern Venezuela.
    Type: Book chapter , NonPeerReviewed
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  • 29
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    Elsevier
    In:  Marine Geology, 64 (1-2). pp. 157-177.
    Publication Date: 2019-04-16
    Description: Water samples and suspended matter taken in the Atlantis-II Deep area (Red Sea) during the expedition SO-2 (with RV “Sonne”) in November 1977 were investigated for chemical composition. Only slight changes have been found for most components since 1966. A strong decrease of the Cu content (from 100–500 μg kg−1 according to Brooks et al., 1969, to values below 1 μg kg−1) has, however, become evident. Comparison between theoretical concentrations in the intermediate brine layers (resulting when using the lower or the upper homothermal layers, respectively, as end members of mixing processes with Red Sea deep water) and the concentrations measured prove that precipitation and resolution processes have considerable influence on the concentrations found in solution. Components strongly involved in such processes are: iron, manganese, copper, oxygen, sulfate, and silica, as could be shown from comparison of theoretical and measured concentration profiles along the water column. Investigations of the metals suspended in the brine confirm these processes. Compared to 1971/1972, the Cu and Zn values in suspension (preferring the southwestern basin at that time) are clearly reduced — thus being in agreement with the recently lowered hydrothermal activity. Remarks on the hypothetical composition of the unknown hydrothermal brine discharging into the deepest basin are also included.
    Type: Article , PeerReviewed
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  • 30
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    Springer
    In:  Geologische Rundschau, 74 (3). pp. 585-597.
    Publication Date: 2021-02-18
    Description: The Pantelleria Rift system is a wide zone of post-Miocene northwest-trending grabens and horsts beneath the Sicily Strait. The central grabens host volcanics of predominantly alkalic composition which are exposed on the islands of Pantelleria and Linosa. On the Maltese Islands, along the northeastern shoulder of the rift, an Oligocene-Miocene carbonate succession exposed above sea level allows structural analysis and determination of shallow crustal stresses within the otherwise largely submarine rift system. An older northeast-trending set of normal faults is probably the expression of an Oligocene-Miocene crustal extension event which produced continental rifts in western Europe and led to passive margin formation in the western Mediterranean. Younger northwest-trending grabens of the Pantelleria Rift system cut the older faults almost at right angles and define a zone of lithospheric stretching between Tunisia and Sicily. The northwest-trending grabens which subsided dramatically since the beginning of Pliocene time appear to be connected by east-trending dextral and, more rarely, north-trending sinistral transforms. Displacement along the transforms is probably in the order of a few kilometres. In-situ stress measurements carried out on the Maltese Islands show maximum horizontal compression (SH) parallel to the rift. This suggests that in general σ1 (vertical) and σ2 (horizontal and parallel to the rift) are of about the same magnitude; both exceed σ3 (Sh) which trends northeasterly. Slight intraplate convergence in a NW-SE direction seems to be more than balanced by extension in a NE-SW direction. Neotectonics of the region possibly reflects an asthenospheric flow pattern which became established during the Messinian salinity crisis. The mechanism of recent intraplate deformation of the Pelagian shelf has relevance for the understanding of more anciently subsided platforms of the Apulian Plate.
    Type: Article , PeerReviewed
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  • 31
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    Springer
    In:  Marine Biology, 86 (2). pp. 199-202.
    Publication Date: 2021-08-31
    Description: Cephalopod remains were collected from all of 12 dead Emperor penguin chicks [Aptenodytes forsteri (Gray)], from 76% of 29 living adult Emperor penguins, and from 18% of 105 living adult Adelie penguins [Pygoscelis adeliae (Hombron & Jacquinot)] from Adelie Land, Antarctica, in 1982. Of the seven species of squids represented by lower beaks, Psychroteuthis glacialis comprised 88% of the number in both Emperor chicks and Emperor adults and 100% in Adelie adults. From estimates of the weight of squids represented by lower beaks, Gonatus antarcticus and Kondakovia longimana contributed 18 and 14%, respectively, of the weight of squids in the diet of Emperor chicks and 27 and 21%, respectively, in the diet of Emperor adults. The data suggest that Psychroteuthis glacialis probably hatch in July–September and grow steadily for one year, and then spawn and die.
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  • 32
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    Elsevier
    In:  Earth and Planetary Science Letters, 73 (2-4). pp. 285-298.
    Publication Date: 2020-04-08
    Description: The concentrations of nine rare earth elements (REE) La, Ce, Nd, Sm, Eu, Gd, Dy, Er and Yb, have been determined in mixed species assemblages of foraminifera tests taken from Atlantic Ocean sediment core tops. Reductive cleaning techniques have revealed that REE are present in three phases in foraminifera tests collected from sea floor sediments; REE included in the foraminiferal calcite matrix (termed lattice REE), REE associated with an authigenic FeMn-rich phase adsorbed onto the surface of the test following the death of the organism (termed coating REE) and REE associated with alumino-silicate detritus (termed detrital REE) which commonly infills the test chambers after burial in the sediment. The concentrations of REE in the nondetrital (lattice plus coating) and lattice phases have been measured in this study. Approximately 90% of the REE measured in the non-detrital phase reside in the coating phase, the remainder being present in the lattice phase. These data have been used to investigate the relationship between the distribution of dissolved REE in the ocean and in the coating and lattice phases. In addition to the REE the concentrations of Mn, Fe, Cu, Al and PO4 have been measured as an aid to characterisation of the various phases.
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