{"id":2004,"date":"2012-08-09T08:03:02","date_gmt":"2012-08-09T11:03:02","guid":{"rendered":"https:\/\/www.palaeontologyonline.com\/?page_id=2004"},"modified":"2012-08-09T08:14:08","modified_gmt":"2012-08-09T11:14:08","slug":"anomalocaridids","status":"publish","type":"page","link":"https:\/\/www.palaeontologyonline.com\/?page_id=2004","title":{"rendered":"Anomalocaridids"},"content":{"rendered":"<p>Anomalocaridids (members of the extinct <a title=\"Arthropods\" href=\"https:\/\/34.32.27.218\/glossary\/a\/arthropods\/\">arthropod<\/a> family\u00a0Anomalocarididae) are marine animals largely found in Cambrian deposits, including rocks from\u00a0the USA, Canada, Poland, \u00a0China,\u00a0\u00a0and Australia. Current evidence suggests they went extinct sometime after the <a title=\"Devonian (Period)\" href=\"https:\/\/34.32.27.218\/glossary\/d\/devonian-period\/\">Devonian<\/a> period. They were large animals, some may have been up to 2 m (7 ft) in length, and were most likely active predators.<\/p>\n<p><a href=\"http:\/\/en.wikipedia.org\/wiki\/Anomalocaridid\">More information<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Anomalocaridids (members of the extinct arthropod family\u00a0Anomalocarididae) are marine animals largely found in Cambrian deposits, including rocks from\u00a0the USA, Canada, Poland, \u00a0China,\u00a0\u00a0and Australia. Current evidence suggests they went extinct sometime after the Devonian period. They were large animals, some may have been up to 2 m (7 ft) in length, and were most likely active [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":339,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-2004","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.palaeontologyonline.com\/index.php?rest_route=\/wp\/v2\/pages\/2004","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.palaeontologyonline.com\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.palaeontologyonline.com\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.palaeontologyonline.com\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/www.palaeontologyonline.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=2004"}],"version-history":[{"count":3,"href":"https:\/\/www.palaeontologyonline.com\/index.php?rest_route=\/wp\/v2\/pages\/2004\/revisions"}],"predecessor-version":[{"id":2006,"href":"https:\/\/www.palaeontologyonline.com\/index.php?rest_route=\/wp\/v2\/pages\/2004\/revisions\/2006"}],"up":[{"embeddable":true,"href":"https:\/\/www.palaeontologyonline.com\/index.php?rest_route=\/wp\/v2\/pages\/339"}],"wp:attachment":[{"href":"https:\/\/www.palaeontologyonline.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=2004"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}