Broennimannia persica n. ichnogen., n. ichnosp., a new crustacean microcoprolite from the Paleocene of eastern Iran
The new crustacean microcoprolite Broennimannia persica n. ichnogen., n. ichnosp., is described from the Paleocene (Danian-Selandian) of eastern Iran. The new microcoprolite is characterized by a bilateral symmetrical system of longitudinal “canals” that in transverse sections display an irregular (...
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| description | The new crustacean microcoprolite
Broennimannia persica
n. ichnogen., n. ichnosp., is described from the Paleocene (Danian-Selandian) of eastern Iran. The new microcoprolite is characterized by a bilateral symmetrical system of longitudinal “canals” that in transverse sections display an irregular (labyrinthine) outline with concave infoldings and rounded protuberances. The crescentic outline of parts of the canal system recalls the long-ranging ichnogenus
Palaxius
Brönnimann & Norton (Carboniferous to Pleistocene). In the latter ichnogenus, however, the canals are isolated. A general determination key for microcoprolites in transverse section is provided. The new microcoprolite occurs in poorly sorted foram-algal grainstones/packstones with a fine-grained siliciclastic content. The associated microfauna and –flora includes common miliolids, among the agglutinating
Haymanella
,
Stomatorbina
sp., serpulids, and dasycladalean algae (
Cymopolia
sp.,
Trinocladus atacis
Segonzac). From Iran, fossil microcoprolites have been described so far only from the Upper Jurassic, Lower Cretaceous, and Miocene.
Broennimannia persica
represents the first Paleocene record from this area. |
| doi_str_mv | 10.1007/s10347-020-00599-5 |
| format | Article |
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Broennimannia persica
n. ichnogen., n. ichnosp., is described from the Paleocene (Danian-Selandian) of eastern Iran. The new microcoprolite is characterized by a bilateral symmetrical system of longitudinal “canals” that in transverse sections display an irregular (labyrinthine) outline with concave infoldings and rounded protuberances. The crescentic outline of parts of the canal system recalls the long-ranging ichnogenus
Palaxius
Brönnimann & Norton (Carboniferous to Pleistocene). In the latter ichnogenus, however, the canals are isolated. A general determination key for microcoprolites in transverse section is provided. The new microcoprolite occurs in poorly sorted foram-algal grainstones/packstones with a fine-grained siliciclastic content. The associated microfauna and –flora includes common miliolids, among the agglutinating
Haymanella
,
Stomatorbina
sp., serpulids, and dasycladalean algae (
Cymopolia
sp.,
Trinocladus atacis
Segonzac). From Iran, fossil microcoprolites have been described so far only from the Upper Jurassic, Lower Cretaceous, and Miocene.
Broennimannia persica
represents the first Paleocene record from this area.</description><identifier>ISSN: 0172-9179</identifier><identifier>EISSN: 1612-4820</identifier><identifier>DOI: 10.1007/s10347-020-00599-5</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Algae ; Aquatic crustaceans ; Biogeosciences ; Canals ; Carboniferous ; Cretaceous ; Crustaceans ; Earth and Environmental Science ; Earth Sciences ; Ecology ; Flora ; Fossils ; Geochemistry ; Jurassic ; Miocene ; Original Article ; Palaeocene ; Paleocene ; Paleontology ; Plants ; Pleistocene ; Protuberances ; Sedimentology</subject><ispartof>Facies, 2020-07, Vol.66 (3), Article 15</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020</rights><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2020.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c319t-b9355ff07578c694f0f000315dfb07b01fbd81d6e28a9f2ce6ad67550a59389c3</citedby><cites>FETCH-LOGICAL-c319t-b9355ff07578c694f0f000315dfb07b01fbd81d6e28a9f2ce6ad67550a59389c3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10347-020-00599-5$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10347-020-00599-5$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,41487,42556,51318</link.rule.ids></links><search><creatorcontrib>Schlagintweit, Felix</creatorcontrib><creatorcontrib>Rashidi, Koorosh</creatorcontrib><creatorcontrib>Raisossadat, Seyed Naser</creatorcontrib><title>Broennimannia persica n. ichnogen., n. ichnosp., a new crustacean microcoprolite from the Paleocene of eastern Iran</title><title>Facies</title><addtitle>Facies</addtitle><description>The new crustacean microcoprolite
Broennimannia persica
n. ichnogen., n. ichnosp., is described from the Paleocene (Danian-Selandian) of eastern Iran. The new microcoprolite is characterized by a bilateral symmetrical system of longitudinal “canals” that in transverse sections display an irregular (labyrinthine) outline with concave infoldings and rounded protuberances. The crescentic outline of parts of the canal system recalls the long-ranging ichnogenus
Palaxius
Brönnimann & Norton (Carboniferous to Pleistocene). In the latter ichnogenus, however, the canals are isolated. A general determination key for microcoprolites in transverse section is provided. The new microcoprolite occurs in poorly sorted foram-algal grainstones/packstones with a fine-grained siliciclastic content. The associated microfauna and –flora includes common miliolids, among the agglutinating
Haymanella
,
Stomatorbina
sp., serpulids, and dasycladalean algae (
Cymopolia
sp.,
Trinocladus atacis
Segonzac). From Iran, fossil microcoprolites have been described so far only from the Upper Jurassic, Lower Cretaceous, and Miocene.
Broennimannia persica
represents the first Paleocene record from this area.</description><subject>Algae</subject><subject>Aquatic crustaceans</subject><subject>Biogeosciences</subject><subject>Canals</subject><subject>Carboniferous</subject><subject>Cretaceous</subject><subject>Crustaceans</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ecology</subject><subject>Flora</subject><subject>Fossils</subject><subject>Geochemistry</subject><subject>Jurassic</subject><subject>Miocene</subject><subject>Original Article</subject><subject>Palaeocene</subject><subject>Paleocene</subject><subject>Paleontology</subject><subject>Plants</subject><subject>Pleistocene</subject><subject>Protuberances</subject><subject>Sedimentology</subject><issn>0172-9179</issn><issn>1612-4820</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp9kE1LAzEQhoMoWKt_wFPAq1snSbPZHLX4USjoQc8hm07aLW1Sky3ivze1ojcvMwzzvvPxEHLJYMQA1E1mIMaqAg4VgNS6kkdkwGrGq3HD4ZgMgCleaab0KTnLeQXAFQgYkHyXIobQbWwJlm4x5c5ZGka0c8sQFxhG179V3paiNPGDurTLvXVoA910LkUXtymuux6pT3FD-yXSF7vG6DAgjZ6izT2mQKfJhnNy4u0648VPHpK3h_vXyVM1e36cTm5nlRNM91WrhZTeg5KqcbUee_AAIJic-xZUC8y384bNa-SN1Z47rO28VlKClVo02okhuTrMLae97zD3ZhV3KZSVhgvdcF4AyaLiB1X5IueE3mxTwZE-DQOzh2sOcE2Ba77hmr1JHEy5iMMC09_of1xf4YV8pA</recordid><startdate>20200701</startdate><enddate>20200701</enddate><creator>Schlagintweit, Felix</creator><creator>Rashidi, Koorosh</creator><creator>Raisossadat, Seyed Naser</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope></search><sort><creationdate>20200701</creationdate><title>Broennimannia persica n. ichnogen., n. ichnosp., a new crustacean microcoprolite from the Paleocene of eastern Iran</title><author>Schlagintweit, Felix ; Rashidi, Koorosh ; Raisossadat, Seyed Naser</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c319t-b9355ff07578c694f0f000315dfb07b01fbd81d6e28a9f2ce6ad67550a59389c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Algae</topic><topic>Aquatic crustaceans</topic><topic>Biogeosciences</topic><topic>Canals</topic><topic>Carboniferous</topic><topic>Cretaceous</topic><topic>Crustaceans</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Ecology</topic><topic>Flora</topic><topic>Fossils</topic><topic>Geochemistry</topic><topic>Jurassic</topic><topic>Miocene</topic><topic>Original Article</topic><topic>Palaeocene</topic><topic>Paleocene</topic><topic>Paleontology</topic><topic>Plants</topic><topic>Pleistocene</topic><topic>Protuberances</topic><topic>Sedimentology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Schlagintweit, Felix</creatorcontrib><creatorcontrib>Rashidi, Koorosh</creatorcontrib><creatorcontrib>Raisossadat, Seyed Naser</creatorcontrib><collection>CrossRef</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Facies</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Schlagintweit, Felix</au><au>Rashidi, Koorosh</au><au>Raisossadat, Seyed Naser</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Broennimannia persica n. ichnogen., n. ichnosp., a new crustacean microcoprolite from the Paleocene of eastern Iran</atitle><jtitle>Facies</jtitle><stitle>Facies</stitle><date>2020-07-01</date><risdate>2020</risdate><volume>66</volume><issue>3</issue><artnum>15</artnum><issn>0172-9179</issn><eissn>1612-4820</eissn><abstract>The new crustacean microcoprolite
Broennimannia persica
n. ichnogen., n. ichnosp., is described from the Paleocene (Danian-Selandian) of eastern Iran. The new microcoprolite is characterized by a bilateral symmetrical system of longitudinal “canals” that in transverse sections display an irregular (labyrinthine) outline with concave infoldings and rounded protuberances. The crescentic outline of parts of the canal system recalls the long-ranging ichnogenus
Palaxius
Brönnimann & Norton (Carboniferous to Pleistocene). In the latter ichnogenus, however, the canals are isolated. A general determination key for microcoprolites in transverse section is provided. The new microcoprolite occurs in poorly sorted foram-algal grainstones/packstones with a fine-grained siliciclastic content. The associated microfauna and –flora includes common miliolids, among the agglutinating
Haymanella
,
Stomatorbina
sp., serpulids, and dasycladalean algae (
Cymopolia
sp.,
Trinocladus atacis
Segonzac). From Iran, fossil microcoprolites have been described so far only from the Upper Jurassic, Lower Cretaceous, and Miocene.
Broennimannia persica
represents the first Paleocene record from this area.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s10347-020-00599-5</doi></addata></record> |
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| subjects | Algae Aquatic crustaceans Biogeosciences Canals Carboniferous Cretaceous Crustaceans Earth and Environmental Science Earth Sciences Ecology Flora Fossils Geochemistry Jurassic Miocene Original Article Palaeocene Paleocene Paleontology Plants Pleistocene Protuberances Sedimentology |
| title | Broennimannia persica n. ichnogen., n. ichnosp., a new crustacean microcoprolite from the Paleocene of eastern Iran |
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