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  • 1
    Publication Date: 2023-07-10
    Keywords: 20-198A; Adercotryma sp.; Ammodiscus cretaceus; Bolivinopsis parvissimus; Counting 〉63 µm fraction; Deep Sea Drilling Project; DRILL; Drilling/drill rig; Dry mass; DSDP; DSDP/ODP/IODP sample designation; Foraminifera, benthic agglutinated; Glomar Challenger; Glomospira charoides; Glomospira gordialis; Glomospira irregularis; Glomospira serpens; Haplophragmoides biumbilicalis; Haplophragmoides ex gr. H. herbichi; Haplophragmoides ex gr. H. perexplicatus-constrictus; Haplophragmoides fraudulentus; Haplophragmoides incredibilis; Haplophragmoides multicamerus; Hormosina crassa; Hormosina ovulum; Hyperammina spp.; Kalamopsis grzybowskii; Leg20; North Pacific/BASIN; Number of species; Paratrochamminoides corpulentus; Paratrochamminoides dubius; Paratrochamminoides intricatus; Paratrochamminoides semipellucidus; Paratrochamminoides sp.; Plectorecurvoides parvus; Praecystammina globigerinaeformis; Recurvoides sp.; Rhizammina sp.; Sample code/label; Subreophax scalaris; Trochamminoides ex. gr. H. proteus; Trochamminoides olszewskii; Volume
    Type: Dataset
    Format: text/tab-separated-values, 840 data points
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  • 2
    Publication Date: 2023-07-10
    Keywords: 20-196; Adercotryma sp.; Ammodiscus tenuissimus; Bolivinopsis parvissimus; Buzasina pacifica; Counting 〉63 µm fraction; Deep Sea Drilling Project; Dendrophrya excelsa; DRILL; Drilling/drill rig; Dry mass; DSDP; DSDP/ODP/IODP sample designation; Foraminifera, benthic agglutinated; Foraminifera, benthic agglutinated indeterminata; Glomar Challenger; Glomospira charoides; Glomospira gordialis; Glomospira irregularis; Haplophragmoides biumbilicalis; Haplophragmoides ex gr. H. perexplicatus-constrictus; Haplophragmoides fraudulentus; Haplophragmoides krasheninnikovi; Haplophragmoides molestus; Hormosina crassa; Hormosina ovulum; Hyperammina sp.; Leg20; North Pacific/ABYSSAL FLOOR; Number of species; Paratrochamminoides corpulentus; Paratrochamminoides dubius; Paratrochamminoides intricatus; Paratrochamminoides semipellucidus; Paratrochamminoides sp.; Plectorecurvoides parvus; Plectorecurvoides rotundus; Praecystammina globigerinaeformis; Pseudobolivina munda; Rhizammina sp.; Sample code/label; Subreophax scalaris; Volume
    Type: Dataset
    Format: text/tab-separated-values, 442 data points
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Wightman, Winton G; Kuhnt, Wolfgang (1992): Biostratigraphy and paleoecology of Late Cretaceous abyssal agglutinated foraminifers from the western Pacific Ocean (Deep Sea Drilling Project Holes 196A and 198A and Ocean Drilling Program Holes 800A and 801A). In: Larson, RL; Lancelot, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 129, 247-264, https://doi.org/10.2973/odp.proc.sr.129.148.1992
    Publication Date: 2024-01-09
    Description: Abyssal agglutinated foraminifers allow biostratigraphic correlation of Upper Cretaceous brown zeolitic claystones in Deep Sea Drilling Project Holes 196A and 198A and Ocean Drilling Program Holes 800A and 801 A. Three agglutinated foraminiferal zones subdivide the strata overlying the Campanian to Cenomanian cherts. The lower zone is characterized by Hormosina gigantea, which is a Campanian zonal marker in the North Atlantic Ocean and western Tethys. A major correlation level, which was observed in all holes studied, is based on the acme of evolute Haplophragmoides spp. This acme zone was observed in Sample 129-801A-6R-CC, about 9 m above the first occurrence of H. gigantea in Sample 129-801A-7R-1, 62-67 cm (approximately middle Campanian). The uppermost zone is characterized by dominant Paratrochamminoides spp. and in some instances common Bolivinopsis parvissimus (late Campanian to Maestrichtian). The available biostratigraphic data for the Upper Cretaceous of Sites 196, 198, 800, and 801 are correlated with the biochronologic framework of the North Atlantic, western Mediterranean, and Carpathians. Additionally, we use quantitative estimates of the diversity and abundance of agglutinated foraminiferal species to monitor general faunal trends with time in the western Pacific.
    Keywords: 129-800A; 129-801A; 20-196; 20-198A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Joides Resolution; Leg129; Leg20; North Pacific/ABYSSAL FLOOR; North Pacific/BASIN; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 4
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Wightman, Winton G (1992): Reworked benthic foraminifers from Site 802, East Mariana Basin, western Equatorial Pacific. In: Larson, RL; Lancelot, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 129, 229-245, https://doi.org/10.2973/odp.proc.sr.129.123.1992
    Publication Date: 2024-01-09
    Description: Reworked shallow-water larger and deep-water calcareous benthic foraminifers were recovered from foraminiferal packstones and nannofossil chalks in Hole 802A. The autochthonous zeolitic pelagic claystone is characterized by late Campanian abyssal agglutinated foraminifers that allow correlation with the North Atlantic and the adjacent Pigafetta Basin. Assemblages of DendrophryalRhizammina in graded beds within the zeolitic claystone indicate reworking through entrainment in the flocculent E layer of turbidites, rather than recolonization following a biosiliceous event. Background sedimentation of the claystone took place below the carbonate compensation depth. The nannofossil chalk contains reworked lower bathyal to abyssal calcareous foraminifers of late Paleocene to early Miocene age. The topmost bed of the nannofossil chalk unit commences with an algal foraminiferal packstone containing Lepidocyclina sumatrensis, Heterostegina borneensis, Amphistegina hauerina, Asterigerina marshallana, and A. tentoria, which indicate that the source area was a shallow-water reef and allow the bed to be dated as early Miocene. The absence of obviously younger planktonic microfossils in the graded bed indicates that the resedimentation event was generally contemporaneous with original deposition and took place during an early Miocene global sea-level highstand. An early Miocene shallow-water assemblage is also seen in the graded beds at the base of a volcaniclastic turbidite sequence overlying the nannofossil chalks. Resedimentation of this unit was associated with volcanic activity some distance away.
    Keywords: 129-802A; Amphistegina hauerina; Angulogerina angulosa; Aragonia ouezzanensis; Aragonia velascoensis; Asterigerina marshallana; Asterigerina tentoria; Bolivina sp.; Bolivina spp.; Bulimina tuxpamensis; Cassidulina subtumida; Cibicides ribbingi; Cibicides spp.; Cibicidoides voltzianus; Counting 〉63 µm fraction; Dendrophyra latissima; Dentalina spp.; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Epistomina caracolla; Gaudryina pyramidata; Globorotalites michelinianus; Glomospira charoides; Gyroidinoides beisseli; Gyroidinoides cf. praeglobosus; Haplophragmoides biumbilicalis; Haplophragmoides herbichi; Haplophragmoides spp.; Heterostegina borneensis; Hormosina crassa; Hormosina ovulum; Hyperammina dilatata; Joides Resolution; Leg129; Lenticulina sp.; Lenticulina spp.; Lepidocyclina sumatrensis; Loxostomum eleyi; North Pacific Ocean; Number of species; Ocean Drilling Program; ODP; Oridorsalis umbonatus; Orthomorphina aff. antillea; Orthomorphina cf. columnaris; Pararotalia armata; Paratrochamminoides corpulentus; Paratrochamminoides intricatus; Planulina cf. wuellerstorfi; Plectorecurvoides rotundus; Pleurostomella cf. alternans; Praebulimina cushmani; Praecystammina globigerinaeformis; Pullenia minuta; Reussella cf. pseudospinulosa; Rhizammina sp.; Rotalia tectoria; Saccammina sphaerica; Sample code/label; Siphonina cf. tenuicarinata; Stilostomella lepidula; Stilostomella pseudoscripta; Stilostomella sp.; Subreophax scalaris; Trochammina depressa
    Type: Dataset
    Format: text/tab-separated-values, 2352 data points
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  • 5
    Publication Date: 2024-01-09
    Keywords: 129-801A; Adercotryma sp.; Aschemocella spp.; Bolivinopsis parvissimus; Counting 〉63 µm fraction; Dendrophrya excelsa; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Dry mass; DSDP/ODP/IODP sample designation; Foraminifera, benthic agglutinated; Foraminifera, benthic agglutinated indeterminata; Glomospira charoides; Glomospira gordialis; Glomospira irregularis; Glomospira serpens; Haplophragmoides cf. concavus; Haplophragmoides cf. decussatus; Haplophragmoides ex gr. H. perexplicatus-constrictus; Haplophragmoides fraudulentus; Haplophragmoides krasheninnikovi; Haplophragmoides multicamerus; Haplophragmoides sp.; Haplophragmoides spp.; Hormosina crassa; Hormosina ovuloides; Hormosina ovulum gigantea; Hormosina ovulum ovulum; Hyperammina dilatata; Hyperammina elongata; Hyperammina spp.; Joides Resolution; Kalamopsis spp.; Leg129; Lituotuba lituiformis; North Pacific Ocean; Number of species; Nuttallides sp.; Ocean Drilling Program; ODP; Paratrochamminoides corpulentus; Paratrochamminoides dubius; Paratrochamminoides intricatus; Paratrochamminoides semipellucidus; Paratrochamminoides spp.; Plectorecurvoides rotundus; Praecystammina globigerinaeformis; Psammosphaera sp.; Pseudobolivina munda; Recurvoides sp.; Sample code/label; Trochammina sp.; Trochamminoides septatus; Turritellella shoneana; Volume
    Type: Dataset
    Format: text/tab-separated-values, 1824 data points
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  • 6
    Publication Date: 2024-01-09
    Keywords: 129-800A; Ammodiscus cretaceus; Aschemocella spp.; Bolivinopsis parvissimus; Buzasina pacifica; Counting 〉63 µm fraction; Dendrophrya excelsa; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Dry mass; DSDP/ODP/IODP sample designation; Foraminifera, benthic agglutinated; Foraminifera, benthic agglutinated indeterminata; Glomospira charoides; Glomospira gordialis; Glomospira irregularis; Glomospira serpens; Haplophragmoides biumbilicalis; Haplophragmoides decussatus; Haplophragmoides ex gr. H. perexplicatus-constrictus; Haplophragmoides fraudulentus; Haplophragmoides multicamerus; Haplophragmoides sp.; Haplophragmoides spp.; Hormosina crassa; Hormosina ovuloides; Hormosina ovulum gigantea; Hormosina ovulum ovulum; Hyperammina spp.; Joides Resolution; Kalamopsis grzybowskii; Karrerulina cf. conversa; Leg129; North Pacific Ocean; Number of species; Ocean Drilling Program; ODP; Paratrochamminoides corpulentus; Paratrochamminoides dubius; Paratrochamminoides intricatus; Paratrochamminoides semipellucidus; Paratrochamminoides spp.; Plectorecurvoides parvus; Praecystammina globigerinaeformis; Pseudobolivina munda; Sample code/label; Subreophax scalaris; Trochamminoides cf. proteus; Volume
    Type: Dataset
    Format: text/tab-separated-values, 672 data points
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Sedimentology 41 (1994), S. 0 
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The early Stephanian Bonar Cyclothem of the Sydney Basin, Nova Scotia, contains an erosional surface cut through coastal plain strata with economic coals and distributary channel bodies. The erosion surface is interpreted as a palaeovalley 20 m deep and at least 7 km wide that marks a sequence boundary formed during relative fall in sea level. The palaeovalley is filled with stacked alluvial channel bodies which become more isolated as the valley fill passes upward into red, alluvial plain deposits, probably laid down in an anastomosed river system. In an adjacent, interfluve area, calcretes and red, vertic palaeosols cap coastal strata. Assemblage analysis of agglutinated foraminifera and thecamoebians indicates that the palaeovalley was filled with freshwater sediments before an initial marine transgression flooded the alluvial surface and adjacent interfluve.Valley incision probably reflects glacioeustatic sea level fall. However, the alluvial nature of the valley deposits suggests that valley filling reflects an abundant sediment supply during lowstand and/or transgressive stages and was not a direct consequence of sea level rise. During the subsequent transgression phase, aggradation was rapid as sediment supply apparently kept pace with rising sea level. Features of both channel and extra-channel facies suggest that seasonality intensified during the transition from coastal plain to palaeovalley and alluvial plain deposition.
    Type of Medium: Electronic Resource
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  • 8
  • 9
    Publication Date: 1994-08-01
    Print ISSN: 0037-0746
    Electronic ISSN: 1365-3091
    Topics: Geosciences
    Published by Wiley
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  • 10
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