Ericek, a new Pliocene vertebrate locality in the Çameli Basin (southwestern Anatolia, Turkey)

Abstract The Çameli Basin in southwestern Anatolia preserves a sequence of fossiliferous sediments that record the Pliocene and early Pleistocene faunal development in the area. Here, we present the fauna of Ericek, a locality near the bottom of the sequence. The locality is rich in fish remains, pa...
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Autor*in:	van den Hoek Ostende, Lars W. [verfasserIn] Gardner, James D. van Bennekom, Lysanne Alçiçek, M. Cihat Murray, Alison Wesselingh, Frank P. Alçiçek, Hülya Tesakov, Alexey

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2015

Schlagwörter:	Turkey Palaeobiogeography Palaeobatrachidae Palaeolake Palaeoenvironment

Anmerkung:	© Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg 2015

Übergeordnetes Werk:	Enthalten in: Palaeobiodiversity and Palaeoenvironments - Berlin : Springer, 2009, 95(2015), 3 vom: 09. Juli, Seite 305-320
Übergeordnetes Werk:	volume:95 ; year:2015 ; number:3 ; day:09 ; month:07 ; pages:305-320

Links:	Volltext

DOI / URN:	10.1007/s12549-015-0202-3

Katalog-ID:	SPR026192861

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100	1		\|a van den Hoek Ostende, Lars W. \|e verfasserin \|4 aut
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520			\|a Abstract The Çameli Basin in southwestern Anatolia preserves a sequence of fossiliferous sediments that record the Pliocene and early Pleistocene faunal development in the area. Here, we present the fauna of Ericek, a locality near the bottom of the sequence. The locality is rich in fish remains, particularly pharyngeal teeth of the cyprinids Barbus, Carassius and Capoeta, but also includes rare tooth-bearing bones of a possible cobitid and gobiid. The abundant fish remains agree with the geological interpretation that the Ericek sediments were deposited in a palaeolake. That interpretation is further supported by the abundance of mollusc fossils. The gastropod fauna is dominated by Pseudamnicola, Valvata and other freshwater prosobranch taxa. The dominance of prosobranch taxa over freshwater pulmonate species indicates a well-oxygenated lake environment. A range of aquatic, swamp and terrestrial tetrapod taxa are also represented. The amphibian fauna, documented mainly by anuran skull and postcranial bones and by a single salamander jaw, is consistent with a lacustrine setting for Ericek. Notable among the amphibian fossils are two jaws that may document the second record of palaeobatrachid frogs from Anatolia. Reptiles are represented by a few, incomplete vertebrae of colubroid and indeterminate snakes. Micromammal molars suggest the presence of a forested environment surrounding the palaeolake. Muridae are represented by three species, of which Apodemus cf. dominans is the most abundant. The shrew Asoriculus is the second most abundant species, which argues for a humid palaeoenvironment. The co-occurrences of the vole Mimomys occitanus and of the murids Orientalomys cf. similis and Rhagapodemus cf. primaevus indicate a late MN 15 age for the fauna, at an estimated age of 3.4 Ma.
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700	1		\|a Gardner, James D. \|4 aut
700	1		\|a van Bennekom, Lysanne \|4 aut
700	1		\|a Alçiçek, M. Cihat \|4 aut
700	1		\|a Murray, Alison \|4 aut
700	1		\|a Wesselingh, Frank P. \|4 aut
700	1		\|a Alçiçek, Hülya \|4 aut
700	1		\|a Tesakov, Alexey \|4 aut
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author_variant	d h o l w v dholw dholwv j d g jd jdg b l v bl blv m c a mc mca a m am f p w fp fpw h a ha a t at
matchkey_str	article:18671608:2015----::rcknwloeeetbaeoaiynhaeiaisuh
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publishDate	2015
allfields	10.1007/s12549-015-0202-3 doi (DE-627)SPR026192861 (SPR)s12549-015-0202-3-e DE-627 ger DE-627 rakwb eng van den Hoek Ostende, Lars W. verfasserin aut Ericek, a new Pliocene vertebrate locality in the Çameli Basin (southwestern Anatolia, Turkey) 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg 2015 Abstract The Çameli Basin in southwestern Anatolia preserves a sequence of fossiliferous sediments that record the Pliocene and early Pleistocene faunal development in the area. Here, we present the fauna of Ericek, a locality near the bottom of the sequence. The locality is rich in fish remains, particularly pharyngeal teeth of the cyprinids Barbus, Carassius and Capoeta, but also includes rare tooth-bearing bones of a possible cobitid and gobiid. The abundant fish remains agree with the geological interpretation that the Ericek sediments were deposited in a palaeolake. That interpretation is further supported by the abundance of mollusc fossils. The gastropod fauna is dominated by Pseudamnicola, Valvata and other freshwater prosobranch taxa. The dominance of prosobranch taxa over freshwater pulmonate species indicates a well-oxygenated lake environment. A range of aquatic, swamp and terrestrial tetrapod taxa are also represented. The amphibian fauna, documented mainly by anuran skull and postcranial bones and by a single salamander jaw, is consistent with a lacustrine setting for Ericek. Notable among the amphibian fossils are two jaws that may document the second record of palaeobatrachid frogs from Anatolia. Reptiles are represented by a few, incomplete vertebrae of colubroid and indeterminate snakes. Micromammal molars suggest the presence of a forested environment surrounding the palaeolake. Muridae are represented by three species, of which Apodemus cf. dominans is the most abundant. The shrew Asoriculus is the second most abundant species, which argues for a humid palaeoenvironment. The co-occurrences of the vole Mimomys occitanus and of the murids Orientalomys cf. similis and Rhagapodemus cf. primaevus indicate a late MN 15 age for the fauna, at an estimated age of 3.4 Ma. Turkey (dpeaa)DE-He213 Palaeobiogeography (dpeaa)DE-He213 Palaeobatrachidae (dpeaa)DE-He213 Palaeolake (dpeaa)DE-He213 Palaeoenvironment (dpeaa)DE-He213 Gardner, James D. aut van Bennekom, Lysanne aut Alçiçek, M. Cihat aut Murray, Alison aut Wesselingh, Frank P. aut Alçiçek, Hülya aut Tesakov, Alexey aut Enthalten in Palaeobiodiversity and Palaeoenvironments Berlin : Springer, 2009 95(2015), 3 vom: 09. Juli, Seite 305-320 (DE-627)618328130 (DE-600)2537788-7 1867-1608 nnns volume:95 year:2015 number:3 day:09 month:07 pages:305-320 https://dx.doi.org/10.1007/s12549-015-0202-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 95 2015 3 09 07 305-320
spelling	10.1007/s12549-015-0202-3 doi (DE-627)SPR026192861 (SPR)s12549-015-0202-3-e DE-627 ger DE-627 rakwb eng van den Hoek Ostende, Lars W. verfasserin aut Ericek, a new Pliocene vertebrate locality in the Çameli Basin (southwestern Anatolia, Turkey) 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg 2015 Abstract The Çameli Basin in southwestern Anatolia preserves a sequence of fossiliferous sediments that record the Pliocene and early Pleistocene faunal development in the area. Here, we present the fauna of Ericek, a locality near the bottom of the sequence. The locality is rich in fish remains, particularly pharyngeal teeth of the cyprinids Barbus, Carassius and Capoeta, but also includes rare tooth-bearing bones of a possible cobitid and gobiid. The abundant fish remains agree with the geological interpretation that the Ericek sediments were deposited in a palaeolake. That interpretation is further supported by the abundance of mollusc fossils. The gastropod fauna is dominated by Pseudamnicola, Valvata and other freshwater prosobranch taxa. The dominance of prosobranch taxa over freshwater pulmonate species indicates a well-oxygenated lake environment. A range of aquatic, swamp and terrestrial tetrapod taxa are also represented. The amphibian fauna, documented mainly by anuran skull and postcranial bones and by a single salamander jaw, is consistent with a lacustrine setting for Ericek. Notable among the amphibian fossils are two jaws that may document the second record of palaeobatrachid frogs from Anatolia. Reptiles are represented by a few, incomplete vertebrae of colubroid and indeterminate snakes. Micromammal molars suggest the presence of a forested environment surrounding the palaeolake. Muridae are represented by three species, of which Apodemus cf. dominans is the most abundant. The shrew Asoriculus is the second most abundant species, which argues for a humid palaeoenvironment. The co-occurrences of the vole Mimomys occitanus and of the murids Orientalomys cf. similis and Rhagapodemus cf. primaevus indicate a late MN 15 age for the fauna, at an estimated age of 3.4 Ma. Turkey (dpeaa)DE-He213 Palaeobiogeography (dpeaa)DE-He213 Palaeobatrachidae (dpeaa)DE-He213 Palaeolake (dpeaa)DE-He213 Palaeoenvironment (dpeaa)DE-He213 Gardner, James D. aut van Bennekom, Lysanne aut Alçiçek, M. Cihat aut Murray, Alison aut Wesselingh, Frank P. aut Alçiçek, Hülya aut Tesakov, Alexey aut Enthalten in Palaeobiodiversity and Palaeoenvironments Berlin : Springer, 2009 95(2015), 3 vom: 09. Juli, Seite 305-320 (DE-627)618328130 (DE-600)2537788-7 1867-1608 nnns volume:95 year:2015 number:3 day:09 month:07 pages:305-320 https://dx.doi.org/10.1007/s12549-015-0202-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 95 2015 3 09 07 305-320
allfields_unstemmed	10.1007/s12549-015-0202-3 doi (DE-627)SPR026192861 (SPR)s12549-015-0202-3-e DE-627 ger DE-627 rakwb eng van den Hoek Ostende, Lars W. verfasserin aut Ericek, a new Pliocene vertebrate locality in the Çameli Basin (southwestern Anatolia, Turkey) 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg 2015 Abstract The Çameli Basin in southwestern Anatolia preserves a sequence of fossiliferous sediments that record the Pliocene and early Pleistocene faunal development in the area. Here, we present the fauna of Ericek, a locality near the bottom of the sequence. The locality is rich in fish remains, particularly pharyngeal teeth of the cyprinids Barbus, Carassius and Capoeta, but also includes rare tooth-bearing bones of a possible cobitid and gobiid. The abundant fish remains agree with the geological interpretation that the Ericek sediments were deposited in a palaeolake. That interpretation is further supported by the abundance of mollusc fossils. The gastropod fauna is dominated by Pseudamnicola, Valvata and other freshwater prosobranch taxa. The dominance of prosobranch taxa over freshwater pulmonate species indicates a well-oxygenated lake environment. A range of aquatic, swamp and terrestrial tetrapod taxa are also represented. The amphibian fauna, documented mainly by anuran skull and postcranial bones and by a single salamander jaw, is consistent with a lacustrine setting for Ericek. Notable among the amphibian fossils are two jaws that may document the second record of palaeobatrachid frogs from Anatolia. Reptiles are represented by a few, incomplete vertebrae of colubroid and indeterminate snakes. Micromammal molars suggest the presence of a forested environment surrounding the palaeolake. Muridae are represented by three species, of which Apodemus cf. dominans is the most abundant. The shrew Asoriculus is the second most abundant species, which argues for a humid palaeoenvironment. The co-occurrences of the vole Mimomys occitanus and of the murids Orientalomys cf. similis and Rhagapodemus cf. primaevus indicate a late MN 15 age for the fauna, at an estimated age of 3.4 Ma. Turkey (dpeaa)DE-He213 Palaeobiogeography (dpeaa)DE-He213 Palaeobatrachidae (dpeaa)DE-He213 Palaeolake (dpeaa)DE-He213 Palaeoenvironment (dpeaa)DE-He213 Gardner, James D. aut van Bennekom, Lysanne aut Alçiçek, M. Cihat aut Murray, Alison aut Wesselingh, Frank P. aut Alçiçek, Hülya aut Tesakov, Alexey aut Enthalten in Palaeobiodiversity and Palaeoenvironments Berlin : Springer, 2009 95(2015), 3 vom: 09. Juli, Seite 305-320 (DE-627)618328130 (DE-600)2537788-7 1867-1608 nnns volume:95 year:2015 number:3 day:09 month:07 pages:305-320 https://dx.doi.org/10.1007/s12549-015-0202-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 95 2015 3 09 07 305-320
allfieldsGer	10.1007/s12549-015-0202-3 doi (DE-627)SPR026192861 (SPR)s12549-015-0202-3-e DE-627 ger DE-627 rakwb eng van den Hoek Ostende, Lars W. verfasserin aut Ericek, a new Pliocene vertebrate locality in the Çameli Basin (southwestern Anatolia, Turkey) 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg 2015 Abstract The Çameli Basin in southwestern Anatolia preserves a sequence of fossiliferous sediments that record the Pliocene and early Pleistocene faunal development in the area. Here, we present the fauna of Ericek, a locality near the bottom of the sequence. The locality is rich in fish remains, particularly pharyngeal teeth of the cyprinids Barbus, Carassius and Capoeta, but also includes rare tooth-bearing bones of a possible cobitid and gobiid. The abundant fish remains agree with the geological interpretation that the Ericek sediments were deposited in a palaeolake. That interpretation is further supported by the abundance of mollusc fossils. The gastropod fauna is dominated by Pseudamnicola, Valvata and other freshwater prosobranch taxa. The dominance of prosobranch taxa over freshwater pulmonate species indicates a well-oxygenated lake environment. A range of aquatic, swamp and terrestrial tetrapod taxa are also represented. The amphibian fauna, documented mainly by anuran skull and postcranial bones and by a single salamander jaw, is consistent with a lacustrine setting for Ericek. Notable among the amphibian fossils are two jaws that may document the second record of palaeobatrachid frogs from Anatolia. Reptiles are represented by a few, incomplete vertebrae of colubroid and indeterminate snakes. Micromammal molars suggest the presence of a forested environment surrounding the palaeolake. Muridae are represented by three species, of which Apodemus cf. dominans is the most abundant. The shrew Asoriculus is the second most abundant species, which argues for a humid palaeoenvironment. The co-occurrences of the vole Mimomys occitanus and of the murids Orientalomys cf. similis and Rhagapodemus cf. primaevus indicate a late MN 15 age for the fauna, at an estimated age of 3.4 Ma. Turkey (dpeaa)DE-He213 Palaeobiogeography (dpeaa)DE-He213 Palaeobatrachidae (dpeaa)DE-He213 Palaeolake (dpeaa)DE-He213 Palaeoenvironment (dpeaa)DE-He213 Gardner, James D. aut van Bennekom, Lysanne aut Alçiçek, M. Cihat aut Murray, Alison aut Wesselingh, Frank P. aut Alçiçek, Hülya aut Tesakov, Alexey aut Enthalten in Palaeobiodiversity and Palaeoenvironments Berlin : Springer, 2009 95(2015), 3 vom: 09. Juli, Seite 305-320 (DE-627)618328130 (DE-600)2537788-7 1867-1608 nnns volume:95 year:2015 number:3 day:09 month:07 pages:305-320 https://dx.doi.org/10.1007/s12549-015-0202-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 95 2015 3 09 07 305-320
allfieldsSound	10.1007/s12549-015-0202-3 doi (DE-627)SPR026192861 (SPR)s12549-015-0202-3-e DE-627 ger DE-627 rakwb eng van den Hoek Ostende, Lars W. verfasserin aut Ericek, a new Pliocene vertebrate locality in the Çameli Basin (southwestern Anatolia, Turkey) 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg 2015 Abstract The Çameli Basin in southwestern Anatolia preserves a sequence of fossiliferous sediments that record the Pliocene and early Pleistocene faunal development in the area. Here, we present the fauna of Ericek, a locality near the bottom of the sequence. The locality is rich in fish remains, particularly pharyngeal teeth of the cyprinids Barbus, Carassius and Capoeta, but also includes rare tooth-bearing bones of a possible cobitid and gobiid. The abundant fish remains agree with the geological interpretation that the Ericek sediments were deposited in a palaeolake. That interpretation is further supported by the abundance of mollusc fossils. The gastropod fauna is dominated by Pseudamnicola, Valvata and other freshwater prosobranch taxa. The dominance of prosobranch taxa over freshwater pulmonate species indicates a well-oxygenated lake environment. A range of aquatic, swamp and terrestrial tetrapod taxa are also represented. The amphibian fauna, documented mainly by anuran skull and postcranial bones and by a single salamander jaw, is consistent with a lacustrine setting for Ericek. Notable among the amphibian fossils are two jaws that may document the second record of palaeobatrachid frogs from Anatolia. Reptiles are represented by a few, incomplete vertebrae of colubroid and indeterminate snakes. Micromammal molars suggest the presence of a forested environment surrounding the palaeolake. Muridae are represented by three species, of which Apodemus cf. dominans is the most abundant. The shrew Asoriculus is the second most abundant species, which argues for a humid palaeoenvironment. The co-occurrences of the vole Mimomys occitanus and of the murids Orientalomys cf. similis and Rhagapodemus cf. primaevus indicate a late MN 15 age for the fauna, at an estimated age of 3.4 Ma. Turkey (dpeaa)DE-He213 Palaeobiogeography (dpeaa)DE-He213 Palaeobatrachidae (dpeaa)DE-He213 Palaeolake (dpeaa)DE-He213 Palaeoenvironment (dpeaa)DE-He213 Gardner, James D. aut van Bennekom, Lysanne aut Alçiçek, M. Cihat aut Murray, Alison aut Wesselingh, Frank P. aut Alçiçek, Hülya aut Tesakov, Alexey aut Enthalten in Palaeobiodiversity and Palaeoenvironments Berlin : Springer, 2009 95(2015), 3 vom: 09. Juli, Seite 305-320 (DE-627)618328130 (DE-600)2537788-7 1867-1608 nnns volume:95 year:2015 number:3 day:09 month:07 pages:305-320 https://dx.doi.org/10.1007/s12549-015-0202-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 95 2015 3 09 07 305-320
language	English
source	Enthalten in Palaeobiodiversity and Palaeoenvironments 95(2015), 3 vom: 09. Juli, Seite 305-320 volume:95 year:2015 number:3 day:09 month:07 pages:305-320
sourceStr	Enthalten in Palaeobiodiversity and Palaeoenvironments 95(2015), 3 vom: 09. Juli, Seite 305-320 volume:95 year:2015 number:3 day:09 month:07 pages:305-320
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Turkey Palaeobiogeography Palaeobatrachidae Palaeolake Palaeoenvironment
isfreeaccess_bool	false
container_title	Palaeobiodiversity and Palaeoenvironments
authorswithroles_txt_mv	van den Hoek Ostende, Lars W. @@aut@@ Gardner, James D. @@aut@@ van Bennekom, Lysanne @@aut@@ Alçiçek, M. Cihat @@aut@@ Murray, Alison @@aut@@ Wesselingh, Frank P. @@aut@@ Alçiçek, Hülya @@aut@@ Tesakov, Alexey @@aut@@
publishDateDaySort_date	2015-07-09T00:00:00Z
hierarchy_top_id	618328130
id	SPR026192861
language_de	englisch
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author	van den Hoek Ostende, Lars W.
spellingShingle	van den Hoek Ostende, Lars W. misc Turkey misc Palaeobiogeography misc Palaeobatrachidae misc Palaeolake misc Palaeoenvironment Ericek, a new Pliocene vertebrate locality in the Çameli Basin (southwestern Anatolia, Turkey)
authorStr	van den Hoek Ostende, Lars W.
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topic_title	Ericek, a new Pliocene vertebrate locality in the Çameli Basin (southwestern Anatolia, Turkey) Turkey (dpeaa)DE-He213 Palaeobiogeography (dpeaa)DE-He213 Palaeobatrachidae (dpeaa)DE-He213 Palaeolake (dpeaa)DE-He213 Palaeoenvironment (dpeaa)DE-He213
topic	misc Turkey misc Palaeobiogeography misc Palaeobatrachidae misc Palaeolake misc Palaeoenvironment
topic_unstemmed	misc Turkey misc Palaeobiogeography misc Palaeobatrachidae misc Palaeolake misc Palaeoenvironment
topic_browse	misc Turkey misc Palaeobiogeography misc Palaeobatrachidae misc Palaeolake misc Palaeoenvironment
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title	Ericek, a new Pliocene vertebrate locality in the Çameli Basin (southwestern Anatolia, Turkey)
ctrlnum	(DE-627)SPR026192861 (SPR)s12549-015-0202-3-e
title_full	Ericek, a new Pliocene vertebrate locality in the Çameli Basin (southwestern Anatolia, Turkey)
author_sort	van den Hoek Ostende, Lars W.
journal	Palaeobiodiversity and Palaeoenvironments
journalStr	Palaeobiodiversity and Palaeoenvironments
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author_browse	van den Hoek Ostende, Lars W. Gardner, James D. van Bennekom, Lysanne Alçiçek, M. Cihat Murray, Alison Wesselingh, Frank P. Alçiçek, Hülya Tesakov, Alexey
container_volume	95
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author-letter	van den Hoek Ostende, Lars W.
doi_str_mv	10.1007/s12549-015-0202-3
title_sort	ericek, a new pliocene vertebrate locality in the çameli basin (southwestern anatolia, turkey)
title_auth	Ericek, a new Pliocene vertebrate locality in the Çameli Basin (southwestern Anatolia, Turkey)
abstract	Abstract The Çameli Basin in southwestern Anatolia preserves a sequence of fossiliferous sediments that record the Pliocene and early Pleistocene faunal development in the area. Here, we present the fauna of Ericek, a locality near the bottom of the sequence. The locality is rich in fish remains, particularly pharyngeal teeth of the cyprinids Barbus, Carassius and Capoeta, but also includes rare tooth-bearing bones of a possible cobitid and gobiid. The abundant fish remains agree with the geological interpretation that the Ericek sediments were deposited in a palaeolake. That interpretation is further supported by the abundance of mollusc fossils. The gastropod fauna is dominated by Pseudamnicola, Valvata and other freshwater prosobranch taxa. The dominance of prosobranch taxa over freshwater pulmonate species indicates a well-oxygenated lake environment. A range of aquatic, swamp and terrestrial tetrapod taxa are also represented. The amphibian fauna, documented mainly by anuran skull and postcranial bones and by a single salamander jaw, is consistent with a lacustrine setting for Ericek. Notable among the amphibian fossils are two jaws that may document the second record of palaeobatrachid frogs from Anatolia. Reptiles are represented by a few, incomplete vertebrae of colubroid and indeterminate snakes. Micromammal molars suggest the presence of a forested environment surrounding the palaeolake. Muridae are represented by three species, of which Apodemus cf. dominans is the most abundant. The shrew Asoriculus is the second most abundant species, which argues for a humid palaeoenvironment. The co-occurrences of the vole Mimomys occitanus and of the murids Orientalomys cf. similis and Rhagapodemus cf. primaevus indicate a late MN 15 age for the fauna, at an estimated age of 3.4 Ma. © Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg 2015
abstractGer	Abstract The Çameli Basin in southwestern Anatolia preserves a sequence of fossiliferous sediments that record the Pliocene and early Pleistocene faunal development in the area. Here, we present the fauna of Ericek, a locality near the bottom of the sequence. The locality is rich in fish remains, particularly pharyngeal teeth of the cyprinids Barbus, Carassius and Capoeta, but also includes rare tooth-bearing bones of a possible cobitid and gobiid. The abundant fish remains agree with the geological interpretation that the Ericek sediments were deposited in a palaeolake. That interpretation is further supported by the abundance of mollusc fossils. The gastropod fauna is dominated by Pseudamnicola, Valvata and other freshwater prosobranch taxa. The dominance of prosobranch taxa over freshwater pulmonate species indicates a well-oxygenated lake environment. A range of aquatic, swamp and terrestrial tetrapod taxa are also represented. The amphibian fauna, documented mainly by anuran skull and postcranial bones and by a single salamander jaw, is consistent with a lacustrine setting for Ericek. Notable among the amphibian fossils are two jaws that may document the second record of palaeobatrachid frogs from Anatolia. Reptiles are represented by a few, incomplete vertebrae of colubroid and indeterminate snakes. Micromammal molars suggest the presence of a forested environment surrounding the palaeolake. Muridae are represented by three species, of which Apodemus cf. dominans is the most abundant. The shrew Asoriculus is the second most abundant species, which argues for a humid palaeoenvironment. The co-occurrences of the vole Mimomys occitanus and of the murids Orientalomys cf. similis and Rhagapodemus cf. primaevus indicate a late MN 15 age for the fauna, at an estimated age of 3.4 Ma. © Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg 2015
abstract_unstemmed	Abstract The Çameli Basin in southwestern Anatolia preserves a sequence of fossiliferous sediments that record the Pliocene and early Pleistocene faunal development in the area. Here, we present the fauna of Ericek, a locality near the bottom of the sequence. The locality is rich in fish remains, particularly pharyngeal teeth of the cyprinids Barbus, Carassius and Capoeta, but also includes rare tooth-bearing bones of a possible cobitid and gobiid. The abundant fish remains agree with the geological interpretation that the Ericek sediments were deposited in a palaeolake. That interpretation is further supported by the abundance of mollusc fossils. The gastropod fauna is dominated by Pseudamnicola, Valvata and other freshwater prosobranch taxa. The dominance of prosobranch taxa over freshwater pulmonate species indicates a well-oxygenated lake environment. A range of aquatic, swamp and terrestrial tetrapod taxa are also represented. The amphibian fauna, documented mainly by anuran skull and postcranial bones and by a single salamander jaw, is consistent with a lacustrine setting for Ericek. Notable among the amphibian fossils are two jaws that may document the second record of palaeobatrachid frogs from Anatolia. Reptiles are represented by a few, incomplete vertebrae of colubroid and indeterminate snakes. Micromammal molars suggest the presence of a forested environment surrounding the palaeolake. Muridae are represented by three species, of which Apodemus cf. dominans is the most abundant. The shrew Asoriculus is the second most abundant species, which argues for a humid palaeoenvironment. The co-occurrences of the vole Mimomys occitanus and of the murids Orientalomys cf. similis and Rhagapodemus cf. primaevus indicate a late MN 15 age for the fauna, at an estimated age of 3.4 Ma. © Senckenberg Gesellschaft für Naturforschung and Springer-Verlag Berlin Heidelberg 2015
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container_issue	3
title_short	Ericek, a new Pliocene vertebrate locality in the Çameli Basin (southwestern Anatolia, Turkey)
url	https://dx.doi.org/10.1007/s12549-015-0202-3
remote_bool	true
author2	Gardner, James D. van Bennekom, Lysanne Alçiçek, M. Cihat Murray, Alison Wesselingh, Frank P. Alçiçek, Hülya Tesakov, Alexey
author2Str	Gardner, James D. van Bennekom, Lysanne Alçiçek, M. Cihat Murray, Alison Wesselingh, Frank P. Alçiçek, Hülya Tesakov, Alexey
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doi_str	10.1007/s12549-015-0202-3
up_date	2024-07-03T19:26:12.539Z
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Ericek, a new Pliocene vertebrate locality in the Çameli Basin (southwestern Anatolia, Turkey)

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Vorhandene Bände

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