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  • 1
    In: Netherlands Journal of Geosciences - Geologie en Mijnbouw, Cambridge University Press (CUP), Vol. 92, No. 1 ( 2013-04), p. 69-86
    Abstract: We investigated the Quaternary lithological succession and faunas in a borehole near Moriaanshoofd (Province of Zeeland, SW Netherlands), in order to improve our understanding of the depositional context of classical Gelasian mammal faunas from the region. The fossils mostly derive from the base of a fossil-rich interval between 31 m and 36.5 m below the surface, that was initially interpreted as a Middle or Late Pleistocene interglacial marine unit, but turned out to be a Late Quaternary fluvial unit with large amounts of reworked fossils and sediments. Eocene mollusc taxa pinpoint Flanders (Belgium) as the source region for this river. Within the base of this paleo-Schelde River fossil material of various stratigraphic provenance became incorporated.
    Type of Medium: Online Resource
    ISSN: 0016-7746 , 1573-9708
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2013
    detail.hit.zdb_id: 2012361-9
    detail.hit.zdb_id: 160629-3
    SSG: 13
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  • 2
    Online Resource
    Online Resource
    The Bulletin of Zoological Nomenclature ; 2009
    In:  The Bulletin of Zoological Nomenclature Vol. 66, No. 2 ( 2009-06), p. 159-163
    In: The Bulletin of Zoological Nomenclature, The Bulletin of Zoological Nomenclature, Vol. 66, No. 2 ( 2009-06), p. 159-163
    Type of Medium: Online Resource
    ISSN: 0007-5167
    Language: English
    Publisher: The Bulletin of Zoological Nomenclature
    Publication Date: 2009
    detail.hit.zdb_id: 2882993-1
    SSG: 12
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  • 3
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 2014
    In:  Netherlands Journal of Geosciences - Geologie en Mijnbouw Vol. 93, No. 3 ( 2014-09), p. 119-134
    In: Netherlands Journal of Geosciences - Geologie en Mijnbouw, Cambridge University Press (CUP), Vol. 93, No. 3 ( 2014-09), p. 119-134
    Abstract: We investigated fossil small mammals from a borehole near Moriaanshoofd (Zeeland, southwest Netherlands) in order to get better insights in the fossil mammal faunas that are found in the subsurface in the southwestern Netherlands, and to investigate the age and provenance of the mammal fauna that is being dredged from the deep tidal gullies in the nearby Oosterschelde estuary. The record in the borehole covers Gelasian (Early Pleistocene) to Holocene deposits, represented by six formations. Thirty-nine specimens of small mammals were obtained from the borehole. These fossils derived from the Early Pleistocene marine Maassluis Formation and from directly overlying deposits of a Late Pleistocene age. During Weichselian times (33–24 ka), a proto-Schelde River shaped the northern Oosterschelde area. The river reworked substantial amounts of Early and Middle Pleistocene deposits. At the base of the Schelde-derived fluvial sequence (regionally described as the Koewacht Formation), Gelasian vertebrate faunas were concentrated in the channel lag. The Late Pleistocene channel lag is almost certainly the main source for the rich Early Pleistocene vertebrate faunas with larger mammals dredged from the Oosterschelde.
    Type of Medium: Online Resource
    ISSN: 0016-7746 , 1573-9708
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2014
    detail.hit.zdb_id: 2012361-9
    detail.hit.zdb_id: 160629-3
    SSG: 13
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  • 4
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 2008
    In:  Netherlands Journal of Geosciences - Geologie en Mijnbouw Vol. 87, No. 2 ( 2008-08), p. 181-188
    In: Netherlands Journal of Geosciences - Geologie en Mijnbouw, Cambridge University Press (CUP), Vol. 87, No. 2 ( 2008-08), p. 181-188
    Abstract: We describe the occurrence in the Netherlands of three teeth of Mimomys hajnackensis (Arvicolidae, Rodentia) from three separate boreholes extending into matine deposits of the Maassluis Formation. These marine Pliocene/Early Pleistocene deposits at depth are overlain by, and interdigitate eastwards with, the freshwater deposits of the Waalre and Peize Formations (formerly known in part as the Tegelen Formation). Teeth identified as M. hajnackensis have not previously been described from the Netherlands although similar material has been reported from Pliocene deposits in Germany at Frechen and Hambach close to the Dutch border. The material described here comes from boreholes at the Polder de Biesbosch near Dordrecht, Diepenveen and Deventer. To our knowledge, these finds represent the oldest described rodent fossils from the Netherlands, corresponding to an absolute age of 2.9 to 3.3 Ma on the basis of comparison with other European localities, implying that the remains are reworked from older deposits.
    Type of Medium: Online Resource
    ISSN: 0016-7746 , 1573-9708
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2008
    detail.hit.zdb_id: 2012361-9
    detail.hit.zdb_id: 160629-3
    SSG: 13
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  • 5
    Online Resource
    Online Resource
    IOP Publishing ; 2023
    In:  Journal of Instrumentation Vol. 18, No. 04 ( 2023-04-01), p. P04014-
    In: Journal of Instrumentation, IOP Publishing, Vol. 18, No. 04 ( 2023-04-01), p. P04014-
    Abstract: The D-Egg, an acronym for “Dual optical sensors in an Ellipsoid Glass for Gen2,” is one of the optical modules designed for future extensions of the IceCube experiment at the South Pole. The D-Egg has an elongated-sphere shape to maximize the photon-sensitive effective area while maintaining a narrow diameter to reduce the cost and the time needed for drilling of the deployment holes in the glacial ice for the optical modules at depths up to 2700 m. The D-Egg design is utilized for the IceCube Upgrade, the next stage of the IceCube project also known as IceCube-Gen2 Phase 1, where nearly half of the optical sensors to be deployed are D-Eggs. With two 8-inch high-quantum efficiency photomultiplier tubes (PMTs) per module, D-Eggs offer an increased effective area while retaining the successful design of the IceCube digital optical module (DOM). The convolution of the wavelength-dependent effective area and the Cherenkov emission spectrum provides an effective photodetection sensitivity that is 2.8 times larger than that of IceCube DOMs. The signal of each of the two PMTs is digitized using ultra-low-power 14-bit analog-to-digital converters with a sampling frequency of 240 MSPS, enabling a flexible event triggering, as well as seamless and lossless event recording of single-photon signals to multi-photons exceeding 200 photoelectrons within 10 ns. Mass production of D-Eggs has been completed, with 277 out of the 310 D-Eggs produced to be used in the IceCube Upgrade. In this paper, we report the design of the D-Eggs, as well as the sensitivity and the single to multi-photon detection performance of mass-produced D-Eggs measured in a laboratory using the built-in data acquisition system in each D-Egg optical sensor module.
    Type of Medium: Online Resource
    ISSN: 1748-0221
    Language: Unknown
    Publisher: IOP Publishing
    Publication Date: 2023
    detail.hit.zdb_id: 2235672-1
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  • 6
    In: Newsletters on Stratigraphy, Schweizerbart, Vol. 26, No. 2-3 ( 1992-04-22), p. 65-118
    Type of Medium: Online Resource
    ISSN: 0078-0421
    Uniform Title: Report of the RCMNS working group on fossil mammals, Reisensburg 1990
    Language: English , English
    Publisher: Schweizerbart
    Publication Date: 1992
    detail.hit.zdb_id: 129382-5
    detail.hit.zdb_id: 2158078-9
    SSG: 13
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  • 7
    Online Resource
    Online Resource
    Wiley ; 2015
    In:  Geological Journal Vol. 50, No. 3 ( 2015-05), p. 246-256
    In: Geological Journal, Wiley, Vol. 50, No. 3 ( 2015-05), p. 246-256
    Abstract: This paper reviews the Early Pleistocene arvicolids from the UK, including new material, and updating the taxonomy and the stratigraphic interpretations. The biostratigraphic system for the Pliocene and Early Pleistocene proposed by Tesakov for southeast Europe is applied to the UK assemblages. Previous work which recognized three faunal groups is confirmed. The latest assemblages, from the ‘Weybourne Crag’ deposits (currently included in the Wroxham Crag Formation), fall within arvicolid biozone MNR1. The earlier arvicolids, from the Norwich Crag, fall within biozone MNR2, in two distinct levels. The later level, dating from the second half of biozone MNR2, includes the arvicolids from deposits exposed on the Suffolk coast near Southwold, including Easton Bavents. These underlie deposits previously assigned to the Baventian Stage. The earlier arvicolid assemblages date from the first part of biozone MNR2 (or just possibly the end of biozone MNR3) and come from Norwich Crag Formation deposits including the type Bramertonian (Bramerton, Norfolk), as well as deposits at and near the surface in the area of Sizewell (Suffolk). On the basis of palaeomagnetic calibration in southeast Europe, the three levels of the UK sequence are interpreted as corresponding to approximate absolute age limits of 2.1–2.25 Ma (‘Weybourne Crag’), 2.25–2.35 Ma (the later Norwich Crag Formation) and 2.35–2.45 Ma (the earlier Norwich Crag Formation). The revised arvicolid biostratigraphy is considered to be valid for the North Sea Basin area, allowing correlation with deposits in the Netherlands, and a link to be made between continental and marine biostratigraphic schemes. Copyright © 2014 John Wiley & Sons, Ltd.
    Type of Medium: Online Resource
    ISSN: 0072-1050 , 1099-1034
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2015
    detail.hit.zdb_id: 1479201-1
    SSG: 13
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  • 8
    Online Resource
    Online Resource
    Elsevier BV ; 2013
    In:  Quaternary International Vol. 284 ( 2013-1), p. 62-73
    In: Quaternary International, Elsevier BV, Vol. 284 ( 2013-1), p. 62-73
    Type of Medium: Online Resource
    ISSN: 1040-6182
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2013
    detail.hit.zdb_id: 2002133-1
    detail.hit.zdb_id: 1077692-8
    SSG: 13
    SSG: 14
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