{"id":37135,"date":"2026-06-16T14:13:29","date_gmt":"2026-06-16T17:13:29","guid":{"rendered":"http:\/\/localhost:8012\/GabrielPaladino.com\/2026\/06\/16\/cleoniceras-species-2\/"},"modified":"2026-06-16T16:31:15","modified_gmt":"2026-06-16T19:31:15","slug":"ammonoidea-cleoniceras","status":"publish","type":"post","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2026\/06\/16\/ammonoidea-cleoniceras\/","title":{"rendered":"Cleoniceras species"},"content":{"rendered":"<div>\n  <img decoding=\"async\" src=\"https:\/\/live.staticflickr.com\/65535\/55337710097_3a118b4e42_k.jpg\"><\/p>\n<p><b><i>Cleoniceras<\/i><\/b> is a genus of ammonites from the Lower Cretaceous, flourishing during the Albian Stage, approximately 113 to 100 million years ago. Although known from several regions of the former Tethyan realm, Madagascar \u2014 particularly the marine limestones and marls of the Mahajanga Basin, in the island&#8217;s northwest \u2014 has yielded abundant and well-preserved material, making it a key Albian locality for this group. These cephalopods are recognized by their characteristic shells: rather involute, high-whorled, with a small umbilicus and a venter ranging from arched to acute.<\/p>\n<p>When a specimen is cut and polished, it exposes a striking internal architecture. The phragmocone \u2014 the chambered portion of the shell used in buoyancy regulation during the animal&#8217;s life \u2014 is divided into a series of camerae separated by septa, growing progressively from a minute protoconch, barely the size of a grain of rice, to several centimeters across in the outer whorls. Following burial, some chambers became infilled with fine sediment, while others were left as hollow voids later lined with secondary minerals, most commonly calcite and, in some cases, quartz, producing the marked contrasts of color and texture typical of these polished sections; the degree of mineralization depends primarily on local burial and diagenetic conditions rather than on the size of the shell itself. The junction between each septum and the shell wall forms the suture line: a complex, winding, branch-like pattern that runs along every whorl and is one of the diagnostic features used to distinguish ammonite taxa. Externally, when left unpolished, the shell typically preserves its original ribbing \u2014 fine falcoid to sigmoidal ribs arising in pairs from umbilical tubercles and fading on the outermost whorls. While most fossilized shells from the Mahajanga Basin show their original aragonite replaced by stable calcite, a notable number of specimens retain patches of the original iridescent nacreous (mother-of-pearl) layer, a preservation style for which Madagascar&#8217;s Cleoniceras is well known among collectors and paleontologists alike.<\/p>\n<p><b>Scientific Classification:<\/b><br \/>Kingdom: Animalia<br \/>Phylum: Mollusca<br \/>Class: Cephalopoda<br \/>Subclass: Ammonoidea<br \/>Order: Ammonitida<br \/>Superfamily: Hoplitoidea (formerly Hoplitaceae)<br \/>Family: Hoplitidae<br \/>Subfamily: Cleoniceratinae<br \/>Genus: <i>Cleoniceras<\/i><br \/>Species: <i>Cleoniceras<\/i> sp.<\/p>\n<p><b>Era:<\/b> Mesozoic<br \/><b>Period:<\/b> Cretaceous (Albian, ~113\u2013100 Ma)<br \/><b>Origin:<\/b> Type locality, Mahajanga Basin, Madagascar (exact locality not determined for this specimen)<br \/><b>Dimensions:<\/b> 130 x 100 mm<\/p>\n<p><b>Geological Significance:<\/b><br \/>Species of <i>Cleoniceras<\/i> are important biostratigraphic markers for the Albian Stage: their relatively rapid evolutionary turnover and restricted stratigraphic ranges allow geologists to correlate marine sedimentary sequences across the ancient Tethys Ocean. Because successive growth stages \u2014 from protoconch to final body chamber \u2014 are preserved within a single shell, the genus has also been a useful subject for studies of ammonoid ontogeny and morphological adaptation. The genus&#8217;s diversity in Madagascar, including the subgenus <i>Paracleoniceras<\/i> \u2014 under which species such as <i>besairiei<\/i> (now widely reassigned to the genus <i>Aioloceras<\/i>) and <i>tenuicostulatum<\/i> were originally described \u2014 has been extensively documented by the French paleontologist Maurice Collignon in his <i>Atlas des Fossiles Caract\u00e9ristiques de Madagascar<\/i>, which remains a primary reference for identifying Albian ammonites from the region. Precise species-level identification of any given specimen, however, requires expert analysis of venter shape and suture detail together with knowledge of the exact locality and stratigraphic horizon it came from.<\/p>\n<p>Photo Taken: June 04, 2026<br \/>\n     <a href=\"https:\/\/flic.kr\/p\/2sj1egX\">High resolution<\/a><br \/>\n     <a href=\"https:\/\/www.flickr.com\/photos\/93293461@N03\/\">Flickr Gallery<\/a>\n  <\/p>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>Cleoniceras is a genus of ammonites from the Lower Cretaceous, flourishing during the Albian Stage, approximately 113 to 100 million years ago. Although known from several regions of the former Tethyan realm, Madagascar \u2014 particularly the marine limestones and marls of the Mahajanga Basin, in the island&#8217;s northwest \u2014 has yielded abundant and well-preserved material, [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"advanced_seo_description":"","jetpack_seo_html_title":"","jetpack_seo_noindex":false,"jetpack_seo_schema_type":"","_jetpack_newsletter_access":"","_jetpack_dont_email_post_to_subs":false,"_jetpack_newsletter_tier_id":0,"_jetpack_memberships_contains_paywalled_content":false,"_jetpack_feature_clip_id":0,"_jetpack_memberships_contains_paid_content":false,"footnotes":"","jetpack_post_was_ever_published":false},"categories":[2],"tags":[388,521,524,526,640,793,16911,1568,1584,17215,2743,2744,3156,17212,17213,17204,17205,3275,3276,3374,3375,16915,3660,17208,4731,4741,4838,5202,5204,5206,5352,5354,16904,17206,17207,16900,6694,16906,6717,7703,17210,17209,16902,7846,17211,7910,16901,8053,16909,16910,8274,8451,8452,17214,8803,8907,9308,9366,9559,9564,17217,16905,10693,17216,11211,11814,11926,12280,12330,12506,17218,13549,16907,14331,14333],"class_list":["post-37135","post","type-post","status-publish","format-standard","hentry","category-related-posts","tag-albian","tag-ammonite","tag-ammonitida","tag-ammonoidea","tag-animalia","tag-aragonite","tag-atlas-des-fossiles-caracteristiques-de-madagascar","tag-bilateria","tag-biostratigraphy","tag-calcite","tag-cephalopod","tag-cephalopoda","tag-cleoniceras","tag-cleoniceras-paracleoniceras-besairiei","tag-cleoniceras-paracleoniceras-tenuicostulatum","tag-cleoniceras-sp","tag-cleoniceratinae","tag-collectable","tag-collection","tag-conchologia","tag-conchology","tag-conquiliology","tag-cretaceous","tag-early-cretaceous","tag-eubilateria","tag-eukaryota","tag-extinct","tag-fosil","tag-fossil","tag-fossilised","tag-gabriel-paladino-ibanez","tag-gabrielpaladino-com","tag-geochronology","tag-hoplitidae","tag-hoplitoidea","tag-indian-ocean","tag-invertebrate","tag-involute","tag-iridescent","tag-lophotrochozoa","tag-lower-albian","tag-lower-cretaceous","tag-madagascan-ammonite","tag-madagascar","tag-mahajanga-basin","tag-malacology","tag-malagasy-ammonite","tag-marine","tag-marine-limestone","tag-maurice-collignon","tag-mesozoic","tag-mollusc","tag-mollusca","tag-mother-of-pearl","tag-nacre","tag-nektonic","tag-opisthokonta","tag-ornamentation","tag-paleoenvironment","tag-paleontology","tag-phragmocone","tag-planispiral","tag-protostomia","tag-quartz","tag-ribbing","tag-seashell","tag-shell","tag-species","tag-spiralia","tag-stratigraphy","tag-suture-line","tag-umbilicus","tag-whorl-section","tag-zoologia","tag-zoology","has-post-thumbnail"],"tags_input":"albian,ammonite,ammonitida,ammonoidea,animalia,aragonite,Atlas des Fossiles Caract\u00e9ristiques de Madagascar,bilateria,biostratigraphy,calcite,cephalopod,cephalopoda,cleoniceras,Cleoniceras (Paracleoniceras) besairiei,Cleoniceras (Paracleoniceras) tenuicostulatum,Cleoniceras sp.,Cleoniceratinae,collectable,collection,conchologia,conchology,conquiliology,cretaceous,Early Cretaceous,eubilateria,eukaryota,extinct,fosil,fossil,fossilised,Gabriel Paladino Iba\u00f1ez,gabrielpaladino.com,geochronology,Hoplitidae,Hoplitoidea,Indian Ocean,invertebrate,involute,iridescent,lophotrochozoa,Lower Albian,Lower Cretaceous,Madagascan ammonite,madagascar,Mahajanga Basin,malacology,Malagasy ammonite,marine,marine limestone,Maurice Collignon,mesozoic,mollusc,mollusca,mother-of-pearl,nacre,nektonic,opisthokonta,ornamentation,paleoenvironment,paleontology,phragmocone,planispiral,protostomia,quartz,ribbing,seashell,shell,species,spiralia,stratigraphy,suture line,umbilicus,whorl section,zoologia,zoology","jetpack_shortlink":"https:\/\/wp.me\/phjlBv-9EX","jetpack_sharing_enabled":true,"jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":22800,"url":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2024\/05\/19\/douvilleiceras-species\/","url_meta":{"origin":37135,"position":0},"title":"Douvilleiceras species","author":"Gabriel Paladino Ib\u00e1\u00f1ez","date":"May 19, 2024","format":false,"excerpt":"Douvilleiceras is a genus of ammonites from the Middle to Late Cretaceous. Its fossils have been found worldwide, in Africa, Asia, Europe, and North and South America.Fossils of Douvilleiceras are found in the Cretaceous of Angola, Brazil, Canada, Colombia (Capotes Formation, Cundinamarca), the Dominican Republic, Egypt, France, Iran, Japan, Madagascar,\u2026","rel":"","context":"In &quot;Related posts&quot;","block_context":{"text":"Related posts","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/category\/related-posts\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":22717,"url":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2024\/05\/09\/cleoniceras-species\/","url_meta":{"origin":37135,"position":1},"title":"Cleoniceras species","author":"Gabriel Paladino Ib\u00e1\u00f1ez","date":"May 9, 2024","format":false,"excerpt":"Ammonites are a group of extinct molluscs which somewhat resembled a shelled squid when they were alive.These ancient sea creatures had tentacles like the modern octopus, and spiral shells like Nautilus creatures. They first appeared on the fossil record 240 million years ago, in the Triassic Period, and died out\u2026","rel":"","context":"In &quot;Related posts&quot;","block_context":{"text":"Related posts","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/category\/related-posts\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":37102,"url":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2026\/06\/07\/epimayaites-species\/","url_meta":{"origin":37135,"position":2},"title":"Epimayaites species","author":"Gabriel Paladino Ib\u00e1\u00f1ez","date":"June 7, 2026","format":false,"excerpt":"Epimayaites is a genus of ammonites from the Late Jurassic, specifically the Oxfordian stage, approximately 163 to 157 million years ago. Its fossils are found in the marine limestones and marls of southwestern Madagascar \u2014 one of the richest Oxfordian ammonite sites in the Indian Ocean region. Specimens of Epimayaites\u2026","rel":"","context":"In &quot;Related posts&quot;","block_context":{"text":"Related posts","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/category\/related-posts\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":32005,"url":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2025\/07\/23\/ataxioceras-discobolum\/","url_meta":{"origin":37135,"position":3},"title":"Ataxioceras discobolum","author":"Gabriel Paladino Ib\u00e1\u00f1ez","date":"July 23, 2025","format":false,"excerpt":"Ataxioceras discobolum is a species of ammonite from the Late Jurassic, specifically the Unter\u2011Kimmeridgian (approximately 155\u2013153\u202fMa). It is found in the marine sediments of the Kulmbach\u2013Kirchleus area, in the Franconian Alb (Bavaria, Germany), a classic locality for Kimmeridgian studies in Europe. The shell of this ammonite is moderately evolute and\u2026","rel":"","context":"In &quot;Related posts&quot;","block_context":{"text":"Related posts","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/category\/related-posts\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":29828,"url":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2025\/07\/04\/trachyceras-multituberculatum\/","url_meta":{"origin":37135,"position":4},"title":"Trachyceras multituberculatum","author":"Gabriel Paladino Ib\u00e1\u00f1ez","date":"July 4, 2025","format":false,"excerpt":"Trachyceras multituberculatum is an impressive ammonite from the Carnian stage of the Late Triassic, found mainly in the marine rocks of Guizhou Province, southern China. Most fossils are discovered in thin layers of limestone and shale, often as single shells or fragments. This species is important for paleontologists because it\u2026","rel":"","context":"In &quot;Related posts&quot;","block_context":{"text":"Related posts","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/category\/related-posts\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":31627,"url":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2025\/07\/20\/quenstedticeras-species\/","url_meta":{"origin":37135,"position":5},"title":"Quenstedticeras species","author":"Gabriel Paladino Ib\u00e1\u00f1ez","date":"July 20, 2025","format":false,"excerpt":"Quenstedticeras is a genus of ammonites from the Late Middle Jurassic, specifically the Callovian stage, approximately 164 to 161 million years ago. Its fossils are especially abundant in the marine clays of the Dubki Clay Quarry, near Saratov, southwestern Russia\u2014one of the most productive and best-preserved Middle Jurassic ammonite localities\u2026","rel":"","context":"In &quot;Related posts&quot;","block_context":{"text":"Related posts","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/category\/related-posts\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]}],"jetpack_featured_media_url":"","_links":{"self":[{"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/posts\/37135","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/comments?post=37135"}],"version-history":[{"count":3,"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/posts\/37135\/revisions"}],"predecessor-version":[{"id":37139,"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/posts\/37135\/revisions\/37139"}],"wp:attachment":[{"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/media?parent=37135"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/categories?post=37135"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/tags?post=37135"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}