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  • 1
    Book
    Book
    Late quaternary sea-level correlation and applications : Walter S. Newman memorial vol., [proceedings of the NATO Advanced Study Inst. on Late Quaternary Sea-Level Correlation and Applications, Halifax, Canada, 19 - 30 July 1987] (1989)
    Dordrecht [u.a.] : Kluwer
    Details Availability
    Keywords: Sea level Congresses ; Geology, Stratigraphic Congresses Quaternary ; stratigraphic - quaternary ; Konferenzschrift ; Konferenzschrift 1987 ; Festschrift ; Eustatische Meeresspiegelschwankung ; Holozän ; Pleistozän
    Type of Medium: Book
    Pages: X, 229 S. , graph. Darst., Kt.
    ISBN: 0792300165
    Series Statement: NATO ASI series 256
    DDC: 551.7/9
    RVK:
    UT 3100
    Language: English
    Note: Festschrift Walter S. Newman
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    GEOMAR CATALOGUE
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  • 2
    Online Resource
    Online Resource
    Monitoring in Coastal Environments Using Foraminifera and Thecamoebian Indicators. (2007)
    Cambridge :Cambridge University Press,
    Details
    Keywords: Environmental monitoring. ; Electronic books.
    Description / Table of Contents: Emphasizes the methodological approaches being used for environmental applications of foraminifera and thecamoebians. Its main audience will include researchers and consultants, but it will also serve as a supplementary text for graduate students in courses that deal with environmental monitoring and assessment.
    Type of Medium: Online Resource
    Pages: 1 online resource (193 pages)
    Edition: 1st ed.
    ISBN: 9780511153921
    URL: https://ebookcentral.proquest.com/lib/geomar/detail.action?docID=202064
    DDC: 577.510287
    Language: English
    Note: Cover -- Half-title -- Title -- Copyright -- Contents -- Preface -- Scope of This Book -- Who Should Read This Book -- 1 Some Perspective on Testate Rhizopods -- TESTATE RHIZOPODS AS RELIABLE, COST-EFFECTIVE INDICATORS -- UTILITY OF TESTATE RHIZOPODS AS ENVIRONMENTAL INDICATORS -- SOME LIFESTYLE ASPECTS OF TESTATE RHIZOPODS -- Habitat Preferences -- Foraminifera and Thecamoebian Tests -- Sensitivity to Environmental Change -- Reproduction Mode in Relation to Environment -- The Species Identification Problem -- Trophic Position of Foraminifera and Thecamoebians -- BASIC ECOLOGIC DISTRIBUTIONS -- Lakes and Other Freshwater Environments -- Marshes -- Lagoons and Estuaries -- Shelf Areas -- SPATIAL VARIABILITY AND PATTERNS -- SUMMARY OF KEY POINTS -- 2 Methodological Considerations -- COLLECTION OF SAMPLES -- Surface Samples -- Cores -- PROCESSING OF SAMPLES -- Separation of Fossils from Sediment -- Staining Methods -- HANDLING WASHED RESIDUES -- SAMPLING PRECAUTIONS -- Nearshore Subtidal Settings -- Estuarine Environments -- Continental Shelf Settings -- SPATIAL VARIABILITY OF FORAMINIFERA IN CORES -- SOME DATA PRESENTATION OPTIONS -- TAPHONOMIC CONSIDERATIONS -- Bioturbation -- Living to Fossil Assemblage Transitions -- The Dissolved Oxygen Factor -- CaCO3 Dissolution -- SUMMARY OF KEY POINTS -- 3 Applications -- SEA-LEVEL CHANGES -- Definitive Assemblages -- Applications -- RECONSTRUCTION OF COASTAL MARINE PALEOENVIRONMENTS -- Classification of Estuaries and Embayments -- Salinity/Temperature Indicators -- Turbidity Maxima -- Organic Matter Deposition -- Hurricane Detection in Estuarine Sediments -- FORAMINIFERA AND POLLUTION -- Species Sensitivity -- Benthic Foraminifera and Oxygen -- Foraminifera/Organic Matter Interactions -- Foraminifera and Trace Metal Contamination -- Combined Pollution Effects -- Water Temperature Impacts. , Deformed Foraminifera Tests as Pollution Indicators -- Combined Use of Foraminifera and Other Organisms -- FORAMINIFERA AS TRACERS AND TRANSPORT INDICATORS -- Foraminifera as Sediment and Transport Tracers -- MARINE-FRESHWATER TRANSITIONS -- Bedford Basin, Nova Scotia (Canada) -- Raised Basins in New Brunswick (Canada) -- Porter's Lake, Nova Scotia (Canada) -- PALEOCEANOGRAPHIC ANALYSIS -- SUMMARY OF KEY POINTS -- 4 Research on New Applications -- PALEOPRODUCTIVITY -- FORAMINIFERA POPULATIONS AS INDICATORS OF CORAL REEF HEALTH -- CHEMICAL ECOLOGY IN BENTHIC FORAMINIFERA -- CHEMICAL TRACERS IN FORAMINIFERAL TESTS -- SUMMARY OF KEY POINTS -- 5 Freshwater Systems Applications -- THECAMOEBIANS -- General Considerations -- Biology of Thecamoebians -- THE FOSSIL RECORD -- EVOLUTION -- THECAMOEBIAN METHODOLOGY -- PALEOECOLOGICAL RELATIONSHIPS -- Wet Niches -- Lacustrine Niches -- Brackish Water -- Estuaries -- ECOLOGICAL INDICATORS -- APPLICATIONS IN VARIOUS FIELDS -- Relocation of Paleo-sealevels -- Forensic Studies -- Freshwater Influence Detection -- PALEOECOLOGICAL STUDIES OF LACUSTRINE DEPOSITS -- Lakes in North America -- Lakes in Europe -- OTHER POTENTIAL APPLICATIONS -- SUMMARY OF KEY POINTS -- 6 Conclusions and Final Remarks -- Appendix -- GLOSSARY -- TAXONOMIC LIST OF SPECIES -- Benthic foraminifera -- Miliolids -- Tintinnids -- Thecamoebians -- Bibliography -- Name Index -- Subject Index.
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  • 3
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    Foraminiferal assemblages of the Mackenzie-Beaufort Sea Slope and Amundsen Gulf
    PANGAEA
    In:  Supplement to: Scott, David B; Schell, Trecia M; St-Onge, Guillaume; Rochon, André; Blasco, Steve (2009): Foraminiferal assemblage changes over the last 15,000 years on the Mackenzie-Beaufort Sea Slope and Amundsen Gulf, Canada: Implications for past sea ice conditions. Paleoceanography, 24(2), PA2219, https://doi.org/10.1029/2007PA001575
    Details
    Publication Date: 2023-05-12
    Description: Two cores, one from the Beaufort Sea Slope at 1000 m water depth (core 750) and one from the Amundsen Gulf at 426 m (core 124), were collected to help determine paleo-ice cover in the Holocene and late glacial of this area. Site 750 is particularly sensitive to changes in paleo-ice cover because it rests beneath the present ice margin of the permanent Arctic ice pack. Core 124 was sampled just in front of the former glacier that moved out into the Amundsen Gulf and started to recede about 13 ka B.P. Both cores have a strong occurrence of calcareous foraminifera in the upper few centimeters, but these disappear throughout most of the Holocene, suggesting more open water in that time period than present. In the sediments representing the end of the last glacial period (dated at ~11,500-14,000 calibrated years B.P. (cal B.P.)) a calcareous fauna with an abundant planktic foraminiferal fauna suggests a return to almost permanent ice cover, much like the central Arctic today. Together with the foraminifera there was also abundant ice-rafted debris (IRD) in both cores between 12,000 cal B.P. and ~14,000 cal B.P., but those units are of different ages between cores, suggesting different events. The IRD in both cores appears to have the same magnetic and chemical signals, but their origins cannot be determined exactly until clay mineralogy is completed. There is abundant organic debris in both cores below the IRD units: the organics in core 750 are very diffuse and not visually identifiable, but the organic material in core 124 is clearly identifiable with terrestrial root fragments; these are 14C dated at over 37,000 years B.P. This is a marine unit as it also has glacial front foraminifera in the sediment with the organic debris that must have been originating from subglacial streams. The seismic and multibeam data both indicate glaciers did not cross the core 124 site.
    Type: Dataset
    Format: application/zip, 4 datasets
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    DATA PANGAEA
  • 4
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    Tab. 1: Radiocarbon ages of samples from the Canadian archipelago (2011)
    PANGAEA
    In:  Supplement to: Mudie, Peta J; Rochon, André; Prins, Maarten Arnoud; Soenarjo, Donny; Troelstra, Simon; Levac, Elisabeth; Scott, David B; Roncaglia, Lucia; Kuijpers, Antoon (2006): Late Pleistocene-Holocene marine geology of nares strait Region: palaeoceanography from foraminifera and dinoflagellate cysts, sedimentology and stable isotopes. Polarforschung, 74(1-3), 169-183, hdl:10013/epic.29931.d001
    Details
    Publication Date: 2023-02-12
    Description: A sediment-sampling program was carried out in the Nares Strait region during the Nares 2001 Expedition to obtain cores for high-resolution palaeoceanographic studies of late Pleistocene-Holocene climate change. Long cores (〉4 m) were obtained from basins near Coburg Island, Jones Sound, John Richardson Fiord off Kane Basin, and in northeastern Hall Basin. Short cores and grab samples were taken on shelves east and west of northern Smith Sound and in Kennedy Channel. Detailed studies of sediment texture, stable isotopes, microfossils and palynomorphs were made on the longest cores from Jones Sound and Hall Basin at the southern and northern ends of the Nares Strait region.
    Keywords: Age, cultural; Age, dated; Age, dated material; Age, dated standard deviation; Age, radiocarbon; Calendar age; Coburg Island, Jones Sound, Canada; DEPTH, sediment/rock; Event label; GC; Gravity corer; LSSL2001-006PC; LSSL2001-79PC; Mass; northeastern Hall Basin, Canada; Sample, optional label/labor no; δ13C
    Type: Dataset
    Format: text/tab-separated-values, 61 data points
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    DATA PANGAEA
  • 5
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    (Table 1) Paleomagnetic and biological stratigraphic events from Sale borehole, Morocco
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: Age model; Ageprofile Datum Description; CDRILL; Core drilling; DEPTH, sediment/rock; Sale_Briqueterie; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 45 data points
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    DATA PANGAEA
  • 6
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    Benthic foraminifera of the Labrador Sea and Buffin Bay
    PANGAEA
    In:  Supplement to: Scott, David B; Mudie, Peta J; de Vernal, Anne; Hillaire-Marcel, Claude; Baki, V; Mackinnon, K D; Medioli, F S; Mayer, Larry A (1989): Lithostratigraphy, biostratigraphy, and stable-isotope stratigraphy of cores from ODP Leg 105 Site surveys, Labrador Sea and Bffin Bay. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 561-582, https://doi.org/10.2973/odp.proc.sr.105.169.1989
    Details
    Publication Date: 2023-05-12
    Description: Trigger weight (TWC) and piston (PC) cores obtained from surveys of the three sites drilled during Ocean Drilling Program (ODP) Leg 105 were studied in detail for benthic foraminiferal assemblages, total carbonate (all sites), planktonic foraminiferal abundances (Sites 645 and 647), and stable isotopes (Sites 646 and 647). These high-resolution data provide the link between modern environmental conditions represented by the sediment in the TWC and the uppermost cores of the ODP holes. This link provides essential control data for interpretating late Pleistocene paleoceanographic records from these core holes. At Site 645 in Baffin Bay, local correlation is difficult because the area is dominated by ice-rafted deposits and by debris flows and/or turbidite sedimentation. At the two Labrador Sea sites (646 and 647), the survey cores and uppermost ODP cores can be correlated. High-resolution data from the site survey cores also provide biostratigraphic data that refine the interpretations compiled from core-catcher samples at each ODP site.
    Keywords: HUD84-030-04; HUD84-030-04TC; HUD85-027-16; HUD85-027-16TC; Labrador Sea; PC; Piston corer; TC; Trigger corer
    Type: Dataset
    Format: application/zip, 3 datasets
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    DATA PANGAEA
  • 7
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    (Table 2) Paleomagnetic and biological stratigraphic events of DSDP Hole 81-552A from the North Atlantic Ocean
    PANGAEA
    Details
    Publication Date: 2023-06-27
    Keywords: 81-552A; Age model; Ageprofile Datum Description; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg81; North Atlantic/PLATEAU; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 46 data points
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    DATA PANGAEA
  • 8
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    (Table 3) Paleomagnetic and biological stratigraphic events of DSDP Hole 94-608 from the North Atlantic Ocean
    PANGAEA
    Details
    Publication Date: 2023-06-27
    Keywords: 94-608; Age model; Ageprofile Datum Description; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg94; North Atlantic/FLANK; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 45 data points
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    DATA PANGAEA
  • 9
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    Quaternary benthic foraminifers from DSDP Sites 95-612 and 95-613
    PANGAEA
    In:  Supplement to: Scott, David B (1987): Quaternary benthic foraminifers from Deep Sea Drilling Project Sites 612 and 613, Leg 95, New Jersey Transect. In: Poag, CW; Watts, AB; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 95, 313-337, https://doi.org/10.2973/dsdp.proc.95.109.1987
    Details
    Publication Date: 2023-05-12
    Description: The Quaternary benthic foraminifers from Leg 95 Sites 612 and 613 were examined with respect to paleoceanographic trends. Data from the two sites indicate the presence of markedly different bottom-water masses, during both glacial and interglacial periods. The dominant interglacial species at Site 612 is Uvigerinct peregrina, which is barely present in corresponding intervals at Site 613. Dominant glacial species are Elphidium excavatum and Cassidulina reniforme at Site 612 and Epistominella takayanagii at Site 613.
    Keywords: Deep Sea Drilling Project; DSDP
    Type: Dataset
    Format: application/zip, 2 datasets
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    DATA PANGAEA
  • 10
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    (Table 1) Relative abundance of benthic foraminifera in sediment core HUD85-027-16 (1989)
    PANGAEA
    Details
    Publication Date: 2023-11-09
    Keywords: Adercotryma glomeratum; Ammobaculites foliaceoum; Astrammina rara; Astrononion gallowayi; Bolivina arctica; Bolivina spathulata; Brizalina pseudopunctata; Buccella frigida; Bulimina marginata; Buliminella hensoni; Cassidulina laevigata; Cassidulina reniforme; Cassidulina subglobosa; Cibicides lobatulus; Counting 〉63 µm fraction; Cribrostomoides subglobosum; Dendrophyra arborescens; Dentalina spp.; DEPTH, sediment/rock; Eggerella advena; Elphidium bartletti; Elphidium excavatum forma clavata; Elphidium subarcticum; Eoeponides pulchella; Epistominella takayanagii; Event label; Fissurina spp.; Foraminifera, benthic agglutinated indeterminata; Foraminifera, benthic specimens; Foraminifera, planktic; Fursenkoina fusiformis; Fursenkoina pauciloculata; Globobulimina auriculata; Haynesina orbicularis; HUD85-027-16; HUD85-027-16TC; Hyperammina elongata; Islandiella islandica; Islandiella teretis; Labrador Sea; Lagena spp.; Laryngosigma hyalascidia; Lenticulina spp.; Miliolina subrotundra; Nonion barleeanum; Nonionella labradorica; Number of species; Nuttallides umbonifera; Oolina hexagona; Oridorsalis umbonatus; Patellina corrugata; PC; Piston corer; Planulina wuellerstorfi; Psammosphaera fusca; Pseudopolymorphina novangliae; Pullenia subcarinata; Pyrgo williamsoni; Quinqueloculina arctica; Quinqueloculina culturata; Quinqueloculina seminulum; Quinqueloculina stalkeri; Recurvoides scitulum; Reophax arcticus; Reophax scotti; Rhabdammina agglutissima; Rhizammina algaeformis; Saccammina difflugiformis; Stetsonia horvathi; TC; Textularia wiesneri; Trigger corer; Triloculina trihedra; Trochammina globigeriniformis; Uvigerina peregrina; Valvulineria arctica; Valvulineria laevigata
    Type: Dataset
    Format: text/tab-separated-values, 6901 data points
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    DATA PANGAEA
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