أسماك مدرعة - Armoured fish

هذه صفحة مكتوبة بالعربية البسيطة، انظر الصفحة الأصلية

درعيات الجلد
Temporal range: 430–360 Ma
Late Llandovery – Late Devonian
Bothriolepis panderi.jpg
Fossil of Bothriolepis panderi showing its caliper-like pectoral fins
التصنيف العلمي e
أصنوفة غير معروفة (أصلحها): الحياة
مملكة: الحيوانية
Phylum: حبليات
Infraphylum: Gnathostomata
الرتبة: درعيات الجلد
مك‌كوي، 1848


درعيات الجلد Placodermi، (باللاتينية: Placodermi) (مشتقة من الكلمتين اليونانيَّتين πλάξ = لوح وδέρμα = جلد، وتعني حرفيًا "لوحي الجلد") هي طائفة منقرضة من أسماك ما قبل التاريخ، فكية كبيرة الحجم، لها درقة سميكة تغطي أجسامها.[1] والتي تم التعرف عليها من المُستحاثات، والتي عاشت من العصر السيلوري المتأخر إلى نهاية العصر الديفوني. كانت رؤوسها وأقفاصها الصدرية مغطاة بألواح مدرعة مزودة بمفاصل، أما باقي جسمها فكان مغطى الحراشف أو عارٍ حسب النوع. وكانت لوحيات الأدمة من بين أوائل الأسماك الفكية، وقد تطورت فكوكها على الأرجح من أقواسها الخيشومية الأولى. وتمثل مستحاثة لأحد الأنواع تبلغ من العمر 380 مليون سنة أقدم مثال معروف للمواليد.[2] نشأت أولى لوحيات الأدمة التي أمكن التعرف عليها في العصر السيلوري المتأخر، وبدأت أعدادها في التعرض للانحدار الشديد خلال فترة انقراضات العصر الديفوني المتأخر، وأصبحت الطائفة منقرضة تمامًا بحلول نهاية العصر الديفوني.

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الخصائص[تحرير | عدل المصدر]

External anatomy of the placoderm Coccosteus decipiens

التطور والانقراض[تحرير | عدل المصدر]

تطور وانقراض درعيات الجلد. حسب مايكل بنتون،2005.[3]
Dunkleosteus, among the first of the vertebrate apex predators, was a giant armoured placoderm predator.

السجل الأحفوري[تحرير | عدل المصدر]

صورة تخيلية لأحفورة السمكة التي عثر عليها من فصيلة درعيات الجلد، الصين، 26 سبتمبر 2013.

في 26 سبتمبر عثر فريق دولي من العلماء في الصين على ما قد يكون حفرية لأول كائن معروف له وجه مميز وهي سمكة عمرها 419 مليون عام قد تكون حلقة مفقودة في تطور الفقاريات. ونشرت مجلة نيتشر خبر العثور على الحفرية في الصين وهي الأكثر بدائية بين الفقاريات المكتشفة ولها فك حديث به عظمة أسنان موجودة لدى البشر وقال جون لونج استاذ علم الحفريات بجامعة فليندرز في اديليد "أخيراً يحل هذا مشكلة قديمة عن نشأة الأسماك الحديثة." واندهش العلماء حين وجدوا أن السمكة ذات الدروع الكثيفة وهي عضو لم يكن معروفا من قبل في فصيلة درعيات الجلد المنقرضة لها جمجمة صغيرة معقدة وعظام فكية. وينفي هذا فيما يبدو نظريات سابقة تقول إن الفقاريات الحديثة ذات الهياكل العظمية تطورت من كائن يشبه سمكة القرش وله هيكل من الغضاريف.[4]

ويقدم الاكتشاف الجديد فرعاً مفقوداً في شجرة التطور يسبق الكائن الشبيه بسمكة القرش ويظهر أن الهيكل العظمي كان النموذج الاولي لكل من الفقاريات العظمية والغضروفية.

تاريخ الدراسة[تحرير | عدل المصدر]

التصنيف[تحرير | عدل المصدر]

رتب درعيات الجلد
Arthrodira Dunkleosteus interm1DB.jpg

Arthrodira ("jointed neck") were the most diverse and numerically successful of the placoderm orders, occupying roles from giant apex predators to detritus-nibbling bottom dwellers. They had a movable joint between armour surrounding the head and body. As the lower jaw moved down the head shield moved, allowing for a larger opening. All arthrodires, save for Compagopiscis, lacked teeth, and used instead the sharpened edges of a bony plate, termed a "tooth plate," as a biting surface (Compagopiscis had true teeth in addition to tooth plates). The eye sockets are protected by a bony ring, a feature shared by birds and some ichthyosaurs. Early arthrodires, such as the genus Arctolepis, were well-armoured fishes with flattened bodies. The largest member of this group, Dunkleosteus, was a true "superpredator" of the latest Devonian period, reaching 3 to as much as 9 metres in length. In contrast, the long-nosed Rolfosteus measured just 15 cm. Fossils of Incisoscutum have been found containing unborn fetuses, indicating that arthrodires gave birth to live young.[5]

Antiarchi Bothriolepis canadensis.jpg
Bothriolepis canadensis
Antiarchi ("opposite anus") were the second most successful order of placoderms known, after the Arthrodira. The order's name was coined by Edward Drinker Cope, who, after incorrectly identifying the first fossils as being those of an armored tunicate, mistakenly thought the eye-hole was the mouth, and the opening for the anal siphon was on the other side of the body, as opposed to having both oral and anal siphons together at one end. The front portions of their bodies were heavily armoured, to the point of literally resembling a box with eyes, with the sometimes scaled, sometimes naked rear portions often becoming sinuous, particularly with later forms. The pair of pectoral fins were modified into a pair of caliper-like, or arthropod-like limbs. In primitive forms, such as Yunnanolepis, the limbs were thick and short, while in advanced forms, such as Bothriolepis, the limbs were long and had elbow-like joints. The function of the limbs are still not perfectly understood, but most hypothesize that they helped their owners pull themselves across the substrate, as well as allowed their owners to bury themselves into the substrate.قالب:Ctn
Brindabellaspis stensioi.jpg
Brindabellaspis stensioi
Brindabellaspida ("Brindabella's shield") was a long-snouted placoderm from the Early Devonian. When it was first discovered in 1980, it was originally regarded as a weejasperaspid acanthothoracid due to anatomical similarities with the other species found at the same locality. According to Philippe Janvier, anatomical similarities in the brain of Brindabellaspis stensioi and the brain of a jawless fish suggest it is a basal placoderm closest to the ancestral placoderm. Various Early to Middle Devonian placoderm incertae sedis have also been inserted in the order.
Phyllolepis orvini
Phyllolepida ("leaf scales") were flattened placoderms found throughout the world. Like other flattened placoderms they were bottom-dwelling predators that ambushed prey. Unlike other flattened placoderms, they were freshwater fish. Their armour was made of whole plates, rather than the numerous tubercles and scales of Petalichthyida. The eyes were on the sides of the head, unlike visual bottom-dwelling predators, such as stargazers or flatfish which have eyes on the top of their head. The orbits for the eyes were extremely small, suggesting the eyes were vestigial and that the phyllolepids may have been blind.
Ptyctodontida Rhamphodopsis threiplandi.jpg
Rhamphodopsis threiplandi
Ptyctodontida ("beak teeth") were lightly armoured placoderms with big heads, big eyes and long bodies. They has a strong but superficial resemblance to modern day chimaeras. Their armour was reduced to a pattern of small plates around the head and neck. Like the extinct and related acanthothoracids, and the living and unrelated holocephalians, most of the ptyctodontids are thought to have lived near the sea bottom and preyed on shellfish. On account of their lack of armour, some paleontologists have suggested that the Ptyctodontida were not placoderms, but holocephalians or the ancestors of holocephalians. Anatomical examinations of whole fossil specimens have shown that the similarities between these two groups are superficial. The major differences were that holocephalians have shagreen on their skin while ptyctodontids do not, the armoured plates and scales of holocephalians are made of dentine while those of ptyctodontids are made of bone, the craniums of holocephalians are similar to sharks while those of ptyctodontids are similar to those of other placoderms, and most importantly, that holocephalians have true teeth while ptyctodonts have beak-like tooth plates. Ptyctodontids were sexually dimorphic, with the males having pelvic claspers and possibly claspers on the head as well.
Asterosteus stenocephalus.jpg
Rhenanida ("Rhine fish") were flattened, ray-like, bottom-dwelling predators with large, upturned mouths that lived in marine environments. The rhenanids were once presumed to be the most primitive, or at least the closest to the ancestral placoderm, as their armour was made of unfused components—a mosaic of tubercles—as opposed to the solidified plates of "advanced" placoderms, such as antiarchs and arthrodires. However, through comparisons of skull anatomies, rhenanids are now considered to be the sister group of the antiarchs. When rhenanids die, their mosaics come apart, and it has been suggested that the rarity of rhenanids in the fossil record reflects postmortem disassociation, and is not an actual rarity of the species.
Palaeacanthaspis vasta.jpg
Acanthothoraci ("spine chests") were a group of chimaera-like placoderms closely related to the rhenanid placoderms. Superficially, acanthoracids resembled scaly chimaeras or small, scaly arthrodires with blunt rostrums. They were distinguished from chimaeras by a pair of large spines that emanate from their chests, the presence of large scales and plates, tooth-like beak plates, and the typical bone-enhanced placoderm eyeball. They were distinguished from other placoderms due to differences in the anatomy of their skulls, and due to patterns on the skull plates and thoracic plates that are unique to this order. From what can be inferred from the mouthplates of fossil specimens, acanthothoracids were shellfish hunters were ecologically similar to modern-day chimaeras. Competition with their relatives, the ptyctodont placoderms, may have been one of the main reasons for the acanthothoracids' extinction prior to the mid-Devonian extinction event.
Petalichthyida ("thin-plated fish") were small, flattened placoderms, typified by their splayed fins and numerous tubercles that decorated all of the plates and scales of their armour. They reached a peak in diversity during the Early Devonian and were found throughout the world. The petalichthids Lunaspis and Wijdeaspis are among the best known. There was an independent diversification event that occurred in what is now Southern China, producing a handful of unique genera that were once placed in their own order, "Quasipetalichthyida," named after the first discovered species there, Quasipetalichthys haikouensis. Soon after the petalichthids' diversification, they went into decline. Because they had compressed body forms, it is supposed they were bottom-dwellers that chased after or ambushed smaller fish. Their diet is not clear, as none of the fossil specimens found have preserved mouth parts.

Pseudopetalichthys problematica.jpg
Pseudopetalicthys problematica
Pseudopetalichthyida ("false petalichthyids") is a group of elongated, possibly flattened fishes comprising three, poorly preserved and poorly studied genera. It is known only from rare fossils in Lower Devonian strata in Hunsrück, Germany. Like Stensioella heintzi, and the Rhenanida, the pseudopetalichthids had armour made up of a mosaic of tubercles. Like Stensioella heintzi, the pseudopetalichthids' placement within Placodermi is suspect. The matter is not easy to resolve because there are no complete, undamaged and articulated specimens. The anatomical studies done on the crushed specimens that have been found indicate that if they are placoderms consider then they are a group more advanced than the ptyctodonts. As such, pro-placoderm experts consider Pseudopetalichthyida to be the sister group of the Arthrodires + Phyllolepida + Antiarchi trichotomy and the Acanthothoraci + Rhenanida dichotomy.
Stensioella heintzi.jpg
Stensioella heintzi
Stensioellida ("[Heintz's] little Stensio") contains another problematic placoderm of uncertain affinity, known only from the Lower Devonian Hunsrück slates of Germany. Stensioella was a thin fish that,when alive, looked vaguely like an elongated ratfish, or a skinny Gemuendina with thin, strap-like pectoral fins. Similar to those of the Rhenanida, its armour was a complex mosaic of small, scale-like tubercles. The shoulder joints of its armour are similar to other placoderms, and there are superficial similarities in skull plates, and even more superficial similarities between its tubercles and the tubercles of the rhenanids. It is tentatively placed within Placodermi as a primitive placoderm, though some paleontologists believe the rationale for the placement is inadequate. The paleontologist Philippe Janvier has suggested that Stensioella is not a placoderm, but instead is a holocephalian. If this is true then the holocephalians diverged from sharks before the Chondrichthyan Devonian radiation.[6] Critics of Janvier's position say that aside from a bodyplan superficially similar to primitive holocephalians, the two groups have little anatomically else in common.

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مخطط الفرع الحيوي[تحرير | عدل المصدر]































انظر أيضاً[تحرير | عدل المصدر]

الهوامش[تحرير | عدل المصدر]

  1. ^ عبد الجليل هويدي، محمد أحمد هيكل (2004). أساسيات الجيولوجيا التاريخية. مكتبة الدار العربية للكتب.
  2. ^ "Fossil reveals oldest live birth". BBC. May 28, 2008. Retrieved May 30, 2008.
  3. ^ Benton, M. J. (2005) Vertebrate Palaeontology, Blackwell, 3rd edition, Figure 3.25 on page 73.
  4. ^ "العثور على حفرية لسمكة في الصين قد تكون حلقة مفقودة في تطور الفقاريات". رويترز. 2013-09-27. Retrieved 2013-09-27.
  5. ^ "Fish 380 Million Years Old Found With Unborn Embryo". Science Daily. June 6, 2008.
  6. ^ [1]

المصادر[تحرير | عدل المصدر]

  • Ahlberg ,P.E., Trinajstic, K., Johanson, Z. & Long, J.A. 2009. Pelvic claspers confirm chondrichthyan-like internal fertilization in arthrodires. Nature 460: 888–889.
  • Janvier, P. Early Vertebrates Oxford, New York: Oxford University Press, 1998. ISBN 0-19-854047-7
  • LONG, J.A. 1983. New bothriolepid fishes from the Late Devonian of Victoria, Australia. Palaeontology 26: 295–320
  • Long, J.A. 1984. New phyllolepids from Victoria and the relationships of the group. Proceedings of the Linnean Society of New South Wales 107: 263–308.
  • Long, J.A. The Rise of Fishes: 500 Million Years of Evolution Baltimore: The Johns Hopkins University Press, 1996. ISBN 0-8018-5438-5
  • Long, J.A. & Trinajstic, K. 2010. The Late Devonian Gogo Formation Lagerstatte – Exceptional preservation and Diversity in early Vertebrates. Annual Reviews of Earth and Planetary Sciences 38: 665–680
  • Long, J.A., Trinajstic, K., Young, G.C. & Senden, T. 2008. Live birth in the Devonian. Nature 453: 650–652.
  • Long, J.A., Trinajstic, K. & Johanson, Z. 2009. Devonian arthrodire embryos and the origin of internal fertilization in vertebrates. Nature 457: 1124–1127.
  • Zhu M, X Yu, B Choo, J Wang and L Jia (2012) "An antiarch placoderm shows that pelvic girdles arose at the root of jawed vertebrates" Journal of the Royal Society, Biology Letters, 8 (3): 453–456.

وصلات خارجية[تحرير | عدل المصدر]

الكلمات الدالة:
تمّ الاسترجاع من "https://www.marefa.org/درعيات_الجلد"