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            Export Date: 25 March 2024            
            CODEN: PPPYA            
            Correspondence Address: Vörös, A.; MTA-MTM-ELTE Research Group for Paleontology, Hungarian Academy of Sciences, Hungarian Natural History Museum, Eötvös Loránd University, P.O.B. 137, H-1431 Budapest, Hungary; email: voros@nhmus.hu</comment>
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	&lt;pre class=&quot;comment&quot; style=&quot;margin-top: 0; margin-bottom: 0;&quot;&gt;&lt;u&gt;Megjegyzés&lt;/u&gt;: Cited By :6            
            Export Date: 25 March 2024            
            CODEN: PPPYA            
            Correspondence Address: Vörös, A.; MTA-MTM-ELTE Research Group for Paleontology, Hungarian Academy of Sciences, Hungarian Natural History Museum, Eötvös Loránd University, P.O.B. 137, H-1431 Budapest, Hungary; email: voros@nhmus.hu&lt;/pre&gt;

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      <comment>Cited By :35            
            Export Date: 25 March 2024            
            CODEN: PPPYA            
            Correspondence Address: Vörös, A.; Research Group for Palaeontology, P.O.B. 137, H-1431 Budapest, Hungary; email: voros@nhmus.hu</comment>
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	&lt;pre class=&quot;comment&quot; style=&quot;margin-top: 0; margin-bottom: 0;&quot;&gt;&lt;u&gt;Megjegyzés&lt;/u&gt;: Cited By :35            
            Export Date: 25 March 2024            
            CODEN: PPPYA            
            Correspondence Address: Vörös, A.; Research Group for Palaeontology, P.O.B. 137, H-1431 Budapest, Hungary; email: voros@nhmus.hu&lt;/pre&gt;

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      <comment>Cited By :52            
            Export Date: 25 March 2024            
            CODEN: PPPYA            
            Correspondence Address: Vörös, A.; Geological and Palaeontological Department, , Budapest, Hungary; email: voros@nhmus.hu</comment>
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      <abstractText>The Jurassic brachiopod fauna of the Alpine-Mediterranean region is dominated by smooth rhynchonellids and spirifermids and sulcate or perforate terebratulids, in contrast to the typical coarsely ribbed brachiopods of the contemporaneous European and African epicontinental areas. The best studied example of the Mediterranean brachiopod province is the Pliensbachian fauna of the Bakony Mountains (Hungary).
There the five most abundant genera are all smooth (Linguithyris, Securithyris, Apringia, Bakonyithyris, Pisirhynchia). These smooth genera represent different morphological types (sulcate, axiniform, uniplicate). Phylogenetically related forms are known from several
evolutionary lineages of discontinuous record ranging from the Triassic to the Recent. The Triassic-Jurassic and the Neogene-Recent parts of these evolutionary lineages are represented by several genera, while in the Late Cretaceous-Paleogene interval they seemingly disappear, at least they have no record. The Recent relatives of the above Pliensbachian genera live mostly in the deep sea: three are shallow bathyal (200-400 m), three deep bathyal (800-1200 m) and three abyssal (2000-4500 m). The abyssal genera occur mainly in the East Pacific. The geographical distdbution of the bathyal genera shows peculiar features: they are more or less confined to the western sides of the great ocean basins (West Pacific, West Indian Ocean, Caribbean region) and they are "thalassobathyal", i.e., they are living on submarine plateaus, seamounts or island aprons and not on the continental slopes. This pattern, extrapolated to the past, shows good analogy with the Jurassic palaeogeographical model developed for the western part of the Tethys Ocean. It is hypothesized that smooth, mainly sulcate, articulate brachiopods flourished in the bathyal or even abyssal zones during the Palaeozoic; they were not refugees but formed well-adapted communities. This stable, conservative fauna may have survived the crises manifested
in the shelf seas and, in cases of appropriate palaeogeographical situations, may have implanted its descendants to the shallow bathyal or even sublittoral regions of the western margins of the ocean basins. The Mediterranean microcontinent system at the western part of the Jurassic Tethys might have been such an invaded region. Correlation
between plate tectonic changes of ocean/continent configurations, the presence of ocean basins closed on the west, and the occurrence of smooth articulate brachiopod groups in shallow bathyal to sublittoral settings collectively suggest that the deep-water forms invaded the shallow environments of the western Tethys in Early Mesozoic times and the W Pacific and W Indian Oceans in the Neogene. They stayed in the
deep-sea reservoir when a circum-equatorial ocean existed in the Late Mesozoic. (c) 2005 Elsevier B.V. All rights reserved.</abstractText>
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	&lt;pre class=&quot;comment&quot; style=&quot;margin-top: 0; margin-bottom: 0;&quot;&gt;&lt;u&gt;Megjegyzés&lt;/u&gt;: Cited By :52            
            Export Date: 25 March 2024            
            CODEN: PPPYA            
            Correspondence Address: Vörös, A.; Geological and Palaeontological Department, , Budapest, Hungary; email: voros@nhmus.hu&lt;/pre&gt;

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            Export Date: 23 February 2023            
            Correspondence Address: Vörös, A.; Geol./Paleontological Dept., Hungarian Nat. Hist. Museum, Múzeum krt. 14-16, Budapest HU-1088, Hungary; email: voros@paleo.nhmus.hu</comment>
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the Alpine region to the whole Mediterranean and the NW-European
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	&lt;pre class=&quot;comment&quot; style=&quot;margin-top: 0; margin-bottom: 0;&quot;&gt;&lt;u&gt;Megjegyzés&lt;/u&gt;: Cited By :81            
            Export Date: 23 February 2023            
            Correspondence Address: Vörös, A.; Geol./Paleontological Dept., Hungarian Nat. Hist. Museum, Múzeum krt. 14-16, Budapest HU-1088, Hungary; email: voros@paleo.nhmus.hu&lt;/pre&gt;

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	&lt;pre class=&quot;comment&quot; style=&quot;margin-top: 0; margin-bottom: 0;&quot;&gt;&lt;u&gt;Megjegyzés&lt;/u&gt;: GECZY JUBILEE VOLUME, ISBN: 963-463-020-0&lt;/pre&gt;
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      <comment>Cited By :81            
            Export Date: 11 November 2022            
            CODEN: PPPYA            
            Correspondence Address: Vörös, A.; Department of Geology and Paleontology, Hungarian Natural History Museum, Muzeum Körút 14-16, H-1370 Budapest, Hungary            
            Funding details: Hungarian Scientific Research Fund, OTKA, 356/88            
            Funding text 1: The author is indebted to the organizerso f this special volume for inviting his paper. Special thanks are due to Dr. Miguel Mancefiido (La Plata) and to an anonymous reviewer for their valuable comments,a nd \\['ori mprovingthe English text. M. Mancefiido gave very important complementary data to the distributiono f Middle Jurassic nucleatids: Dr. M. Kfizm6r (Budapest) provided the author with a version of the tectonic base map used in Figs. 2 6. Their help is acknowledged herein. The present work was partly supported by the Hungarian Scientific Research Foundation (OTKA) Grant No. 356/88.</comment>
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      <abstractText>The paleobiogeography of the Jurassic brachiopods of the Alpine-Carpathian region and adjacent areas is discussed on the basis of the distribution of ''distinctive taxa''. The Jurassic microplates of the western part of Tethys and the present-day ''terranes'' of the Alpine-Carpathian region are outlined and their relationships are discussed. The migration possibilities of the brachiopods in the Jurassic Tethys were controlled mainly by plate/microplate movements and by changes in the oceanic current system.

The Mediterranean microcontinent, isolated from the European and African shelves by oceanic/deep-sea belts, was the homeland of the Mediterranean brachiopod province. In the course of the Jurassic, the Mediterranean microcontinent moved, as part of the African plate, away from Europe, the widening Alboran-Ligurian-Penninic oceanic belt became a barrier preventing migration of brachiopods. By the end of the Middle Jurassic the Tisza microplate detached from Europe and formed a ''stepping stone'' for brachiopod dispersal. At about the same time, the ''Hesperian Strait'' opened between the basins of the Tethys and the Central Atlantic. The opening of this strait resulted in a reorganization of the Tethyan current system. The westward flowing equatorial currents which made a turn in the western corner of Tethys in the first half of the Mesozoic, now ran to the west through the Hesperian Strait via the Central Atlantic to the Pacific. This change produced a new pattern in brachiopod distribution: the Mediterranean fauna successfully invaded the European shelf, at the same time the Mediterranean province became impoverished.</abstractText>
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	&lt;pre class=&quot;comment&quot; style=&quot;margin-top: 0; margin-bottom: 0;&quot;&gt;&lt;u&gt;Megjegyzés&lt;/u&gt;: Cited By :81            
            Export Date: 11 November 2022            
            CODEN: PPPYA            
            Correspondence Address: Vörös, A.; Department of Geology and Paleontology, Hungarian Natural History Museum, Muzeum Körút 14-16, H-1370 Budapest, Hungary            
            Funding details: Hungarian Scientific Research Fund, OTKA, 356/88            
            F...&lt;/pre&gt;
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