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  • 1
    Monograph available for loan
    Monograph available for loan
    London : Geological Society
    Call number: AWI G5-02-0078
    Type of Medium: Monograph available for loan
    Pages: VI, 218 S. : Abb. ; 24 cm
    ISBN: 1862390754
    Series Statement: Geological Society Special Publication 181
    Branch Library: AWI Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 9/M 01.0159
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: 200 S.
    ISBN: 1862390754
    Series Statement: Geological Society special publication 181
    Classification:
    Meteorology and Climatology
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Unknown
    London : The Geological Society
    Description / Table of Contents: The climate of the early Earth was probably very warm and has, in general, reduced since the Archean. However, it now seems that the world is about 0.6°C warmer than it was 100 years ago and estimates of the rate of global warming over the next century range from 0.16°C to 0.35°C per decade. Concurrently, global sea-level is predicted to rise from 2.4 to 10 cm per decade. These rates of change are much faster than those normally associated with the geological record, causing geologists and palaeontologists to reassess their data and their forecasts on rates of future change. With the current interest in global climatic change and, more specifically, with global warming, it is clear that palaeontologists have valuable information to provide on the impacts of past climatic change. This volume contains papers from an international array of such geologists and palaeontologists, showing how studies of micro- and macrofossils, plant and vertebrate fossils from a range of geological ages have contributed to our understanding of how climate affects both local and more widespread areas. The contributions are arranged in geological order, ranging from the Permo-Carboniferous to the post-glacial recovery of the last 18,000 years, with an emphasis on climate change during the last two million years, particularly in NW Europe. Climates: Past and Present will be of interest to palaeontologists, geologists and palaeoclimatologists who specialize in climatic reconstructions and any professionals enagaged in research into the geological aspects of climate change.
    Pages: Online-Ressource (218 Seiten)
    ISBN: 1862390754
    Language: English
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  • 4
    Unknown
    London : The Geological Society
    Keywords: Massenaussterben ; Paläontologie ; Regeneration ; Paläobiologie ; Paläoökologie ; Biotischer Faktor ; Extinction (Biology) ; Paleoecology
    Description / Table of Contents: General --- David J. Bottjer, Jennifer K. Schubert, and Mary L. Droser: Comparative evolutionary palaeoecology: assessing the changing ecology of the past / Geological Society, London, Special Publications, 102:1-13, doi:10.1144/GSL.SP.1996.001.01.01 --- Erle G. Kauffman and Peter J. Harries: The importance of crisis progenitors in recovery from mass extinction / Geological Society, London, Special Publications, 102:15-39, doi:10.1144/GSL.SP.1996.001.01.02 --- Peter J. Harries, Erle G. Kauffman, and Thor A. Hansen: Models for biotic survival following mass extinction / Geological Society, London, Special Publications, 102:41-60, doi:10.1144/GSL.SP.1996.001.01.03 --- Valentin A. Krassilov: Recovery as a function of community structure / Geological Society, London, Special Publications, 102:61-63, doi:10.1144/GSL.SP.1996.001.01.04 --- E. A. Jarzembowski and A. J. Ross: Insect origination and extinction in the Phanerozoic / Geological Society, London, Special Publications, 102:65-78, doi:10.1144/GSL.SP.1996.001.01.05 --- Palaeozoic --- Andrey Yu. Zhuravlev: Reef ecosytem recovery after the Early Cambrian extinction / Geological Society, London, Special Publications, 102:79-96, doi:10.1144/GSL.SP.1996.001.01.06 --- F. M. Swain: Ostracode speciation following Middle Ordovician extinction events, north central United States / Geological Society, London, Special Publications, 102:97-104, doi:10.1144/GSL.SP.1996.001.01.07 --- H. A. Armstrong: Biotic recovery after mass extinction: the role of climate and ocean-state in the post-glacial (Late Ordovician-Early Silurian) recovery of the conodonts / Geological Society, London, Special Publications, 102:105-117, doi:10.1144/GSL.SP.1996.001.01.08 --- William B. N. Berry: Recovery of post—Late Ordovician extinction graptolites: a western North American perspective / Geological Society, London, Special Publications, 102:119-126, doi:10.1144/GSL.SP.1996.001.01.09 --- Dimitri Kaljo: Diachronous recovery patterns in Early Silurian corals, graptolites and acritarchs / Geological Society, London, Special Publications, 102:127-133, doi:10.1144/GSL.SP.1996.001.01.10 --- Petr Čejchan and Jindřich Hladil: Searching for extinction/recovery gradients: the Frasnian-Famennian interval, Mokrá Section, Moravia, central Europe / Geological Society, London, Special Publications, 102:135-161, doi:10.1144/GSL.SP.1996.001.01.11 --- Michael R. House: Juvenile goniatite survival strategies following Devonian extinction events / Geological Society, London, Special Publications, 102:163-185, doi:10.1144/GSL.SP.1996.001.01.12 --- O. L. Kossovaya: The mid-Carboniferous rugose coral recovery / Geological Society, London, Special Publications, 102:187-199, doi:10.1144/GSL.SP.1996.001.01.13 --- William A. DiMichele and Tom L. Phillips: Climate change, plant extinctions and vegetational recovery during the Middle-Late Pennsylvanian Transition: the Case of tropical peat-forming environments in North America / Geological Society, London, Special Publications, 102:201-221, doi:10.1144/GSL.SP.1996.001.01.14 --- Mesozoic --- Douglas H. Erwin and P. Hua-Zhang: Recoveries and Radiations: Gastropods After the Permo-Triassic Mass Extinction / Geological Society, London, Special Publications, 102:223-229, doi:10.1144/GSL.SP.1996.001.01.15 --- A. Hallam: Recovery of the marine fauna in Europe after the end-Triassic and Early Toarcian mass Extinctions / Geological Society, London, Special Publications, 102:231-236, doi:10.1144/GSL.SP.1996.001.01.16 --- A. Tewari, M. B. Hart, and M. P. Watkinson: Foraminiferal recovery after the mid-Cretaceous oceanic anoxic events (OAEs) in the Cauvery Basin, southeast India / Geological Society, London, Special Publications, 102:237-244, doi:10.1144/GSL.SP.1996.001.01.17 --- Danuta Peryt and Marcos Lamolda: Benthonic foraminiferal mass extinction and survival assemblages from the Cenomanian-Turonian Boundary Event in the Menoyo Section, northern Spain / Geological Society, London, Special Publications, 102:245-258, doi:10.1144/GSL.SP.1996.001.01.18 --- Nataliya A. Tur: Planktonic foraminifera recovery from the Cenomanian-Turonian mass extinction event, northeastern Caucasus / Geological Society, London, Special Publications, 102:259-264, doi:10.1144/GSL.SP.1996.001.01.19 --- M. B. Hart: Recovery of the food chain after the Late Cenomanian extinction event / Geological Society, London, Special Publications, 102:265-277, doi:10.1144/GSL.SP.1996.001.01.20 --- M. E. J. Fitzpatrick: Recovery of Turonian dinoflagellate cyst assemblages from the effects of the oceanic anoxic event at the end of the Cenomanian in southern England / Geological Society, London, Special Publications, 102:279-297, doi:10.1144/GSL.SP.1996.001.01.21 --- Elena A. Yazykova: Post-crisis recovery of Campanian desmoceratacean ammonites from Sakhalin, far east Russia / Geological Society, London, Special Publications, 102:299-307, doi:10.1144/GSL.SP.1996.001.01.22 --- Carl F. Koch: Latest Cretaceous mollusc species ‘fabric’ of the US Atlantic and Gulf Coastal Plain: a baseline for measuring biotic recovery / Geological Society, London, Special Publications, 102:309-317, doi:10.1144/GSL.SP.1996.001.01.23 --- Cenozoic --- Eduardo A. M. Koutsoukos: Phenotypic experiments into new pelagic niches in early Danian planktonic foraminifera: aftermath of the K/T boundary event / Geological Society, London, Special Publications, 102:319-335, doi:10.1144/GSL.SP.1996.001.01.24 --- E. M. Bugrova: Recovery of North Caucasus foraminiferal assemblages after the pre-Danian extinctions / Geological Society, London, Special Publications, 102:337-342, doi:10.1144/GSL.SP.1996.001.01.25 --- R. P. Speijer and G. J. Van Der Zwaan: Extinction and survivorship of southern Tethyan Benthic foraminifera across the Cretaceous/Palaeogene boundary / Geological Society, London, Special Publications, 102:343-371, doi:10.1144/GSL.SP.1996.001.01.26 --- Patricia H. Kelley and Thor A. Hansen: Recovery of the naticid gastropod predator-prey system from the Cretaceous-Tertiary and Eocene-Oligocene extinctions / Geological Society, London, Special Publications, 102:373-386, doi:10.1144/GSL.SP.1996.001.01.27
    Pages: Online-Ressource (VI, 394 Seiten) , Illustrationen, Diagramme
    ISBN: 1897799454
    Language: English
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Terra nova 3 (1991), S. 0 
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The various extinctions of marine taxa in the Late Cenomanian can be shown as conforming to the ‘step-wise extinction’ model. The order of such extinctions is, however, compatible with the presence of an expanded oxygen minimum zone in the world ocean. The occurrence of iridium anomalies at this level in the succession may, however, indicate a volcanogenic control on the global environment. Detailed time-analysis of the Late Cenomanian event has been used to produce a correlation of some key successions.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Unequivocal planktonic foraminifera have been discovered in Oxfordian strata from Dorset and Scotland. These assemblages are, in part, coeval with previously reported occurrences of planktonic taxa in the Oxfordian of Normandy and Seine Maritime (France). Three species are now reported from the United Kingdom for the first time: Globuligerina oxfordiana (Grigelis, 1958), Haeuslerina helvetojurassica (Haeusler, 1881) and Compactogerina sp. cf. C. stellapolaris (Grigelis, 1977). There appears to be a close relationship between the distribution of these planktonic taxa in the UK and a marked sea-level highstand.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 329 (1987), S. 364-364 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Paleoceanography. Editor James P. Ken-nett. American Geophysical Union, Washington, DC. 6/yr. $100 (institutional), $34 (individual AGUmembers). THE subject area covered by Paleoceanography is a highly competitive one, which is already served by journals such as Marine Geology, Marine ...
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 286 (1980), S. 252-254 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] In the planktonic environment, and especially in the surface waters where the planktonic Foraminiferida are most abundant, faunas avoid competition by adjusting their regional distributions to the different surface water and temperature regimes and by sometimes seeking different levels in the water ...
    Type of Medium: Electronic Resource
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  • 9
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    Unknown
    In:  Geological Society Special Publication 230: 187-206.
    Publication Date: 2007-10-08
    Description: The mid-Cenomanian non-sequence is described in terms of its stratigraphical position, regional impact and importance in Cenomanian stratigraphy. After its discovery in the site investigation for the Channel Tunnel and its location within the chalk succession of the Dover-Sangatte area, it has been traced throughout the United Kingdom and northern France. In stratigraphically complete successions it is coincident with the base of the Rotalipora cushmani Taxon Range Zone, although in many areas there is a major hiatus (= sequence boundary?) at this level. In more marginal successions, the non-sequence is characterized by the presence of reworked, phosphatized macrofossil assemblages in which the actual date of deposition can only be determined by the non-phosphatized macrofaunal elements or the microfossils extracted from the enclosing sediments. In Dorset/Devon and northern France the Cenomanian successions are condensed, and horizons with reworked macrofaunas have been investigated using a variety of micropalaeontological techniques (thin-sections, processed residues, acid reductions, etc.). In these areas the mid-Cenomanian non-sequence becomes one of the most important features of the succession and marks a major hiatus in many localities.
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  • 10
    facet.materialart.
    Unknown
    In:  Geological Society Special Publication 194: 115-125.
    Publication Date: 2002-01-01
    Description: The planktonic foraminifera almost certainly evolved from benthonic ancestors in the early Jurassic. The meroplanktonic genus Conoglobigerina, known from south-central and eastern Europe, appears in the Bajocian and is probably derived from the even more geographically restricted Praegubkinella. This genus was represented by a single taxon in the earliest Toarcian but diversified after the Toarcian anoxic event. At the same level Oberhauserella quadrilobata Fuchs, 1967 became more inflated and there is some evidence to suggest that the anoxic event' was the environmental perturbation that began the transition to a planktonic mode of life. In the Callovian-Oxfordian interval, the planktonic foraminifera are still restricted to a relatively limited area bounded by the North Atlantic Ocean, NW Europe and Eastern Europe and this remained the case even in the earliest Cretaceous. It was only in the Aptian-Albian that the palaeogeographical distribution changed dramatically, probably as a response to the elevated sea levels caused by the increased rate of ocean crust production which began in the Early Aptian. The principal diversification events in the Jurassic (Toarcian, Bajocian, Callovian-Oxfordian) also appear to be related to sea level highstands.
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