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Hoplopteryx

Hoplopteryx is a biology topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Hoplopteryx rather than just read about it. In short: Hoplopteryx is an extinct genus of slimehead from the Late Cretaceous, lasting from the middle of the Cretaceous to the end. It is one of the best-known fossil trachichthyiforms, and was widespread across the Northern Hemisphere, from throughout Europe east to the Middle East and west to North America.

Hoplopteryx — main illustration
Hoplopteryx — illustration

Key takeaways

  • Hoplopteryx belongs to biology; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Hoplopteryx to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Hoplopteryx from memory before moving on to harder problems.

Reference excerpt

Hoplopteryx is an extinct genus of slimehead from the Late Cretaceous, lasting from the middle of the Cretaceous to the end. It is one of the best-known fossil trachichthyiforms, and was widespread across the Northern Hemisphere, from throughout Europe east to the Middle East and west to North America.

Taxonomy The following valid species are known:

H. antiquus Agassiz, 1838 (type species) - late Campanian of Germany (Ahlen Formation) H. causae (Nolf, 2003) [otolith] - late Santonian of Spain H. coffeesandensis (Nolf & Dockery, 1990) [otolith] - Campanian of Mississippi, US H. dakotaensis Grandstaff & Parris, 2016 - Turonian of North Dakota, US (Carlile Shale) H. gephyrognathus Patterson, 1964 - Turonian of England (English Chalk) H. gibbus von der Marck, 1863 - late Campanian of Germany (Ahlen & Baumberge Formations) ?H. insculptus (Cope, 1869) - Maastrichtian of New Jersey, US (Navesink Formation) H. langfordi Stringer & Schwarzhans, 2020 [otolith] - early Maastrichtian of Mississippi, US (Coon Creek Formation) H. lewesiensis (Mantell, 1822) - mid-Cenomanian to Coniacian of England (English Chalk), Turonian of the Czech Republic (Bilá Hora Formation), Turonian of Voronezh Oblast, Russia, Turonian of France, Campanian of Texas, US (Gober Chalk) (=Zeus lewesiensis Mantell, 1822) H. macracanthus Patterson, 1964 - late Coniacian to early Campanian of England (English Chalk) H. oscitans (Nolf & Stringer, 1996) [otolith] - Maastrichtian of Mississippi, US (Coon Creek & Owl Creek Formations) H. simus Woodward, 1902 - mid-Cenomanian to Coniacian of England (English Chalk) H. supracretacea (Koken, 1891) [otolith] - Maastrichtian of Germany H. syriacus (Pictet & Humbert, 1866) - Santonian of Lebanon (Sahel Alma) H. spinulosus Woodward, 1942 - Santonian of Lebanon (Sahel Alma) H. stachei (Gorjanović-Kramberger, 1895) - Cenomanian of Slovenia (Komen Limestone)

A well-preserved specimen of Hoplopteryx is known from the Maastrichtian-aged Ciply-Malogne Phosphatic Chalk Formation, but still remains undescribed at the species level. Indeterminate remains are also known from the Maastricht Formation. The species ?H. ('Beryx') insculptus is only known from a well-preserved flank of scales. Although it has been previously attributed to Hoplopteryx, no reasoning has been given for this attribution, and its taxonomy thus remains uncertain. The apparent species "Hoplopteryx" lundensis Davis, 1890 from the Early Paleocene of Limhamns kalkbrott, Sweden has been reclassified into Proserranus. The species "H." lewisi (Davis, 1887) from the Cenomanian-aged Sannine Formation of Lebanon has been reclassified into Stichopteryx. A well-preserved specimen of H. lewesiensis from the English Chalk with preserved in situ otoliths has allowed for the morphology of Hoplopteryx otoliths to be better understood, and allowed for the placement of several previously enigmatic otolith-based species within this genus. The morphology of Hoplopteryx otoliths appears to closely resemble those of modern derived trachichthyids, especially the extant Trachichthys & Hoplostethus. This clashes with its external morphology, which shows many features not present in modern trachichthyiforms, causing them to be generally considered stem-group trachichthyids.

Description Hoplopteryx had a dorsal fin supported by nine unjointed, bony rays, deeply forked, homocercal tail, a moderately developed anal fin, and a pelvic fin located well forward. The snout is quite short, the eyes fairly large, and both jaws of the upturned mouth hold small teeth. Hoplopteryx was at a typical length 27 cm. The abundance of well-preserved Hoplopteryx remains throughout the English Chalk allowed for the construction of a time series measuring the body size of Hoplopteryx over the Cretaceous Thermal Maximum. These measurements suggest that as the climate warmed, the body size of Hoplopteryx significantly decreased

Habitat

Hoplopteryx was a marine fish, living primarily in shallow chalk seas. They also appear to have been dominant species in certain deepwater habitats as well, such as those that formed within the Mississippi Embayment near the end of the Cretaceous, with Hoplopteryx oscitans being the most common fish otolith found in the Owl Creek Formation.

Sources Fossils (Smithsonian Handbooks) by David Ward (Page 219) Grandstaff, Barbara S.; Parris, David C. (2016). "A new species of Hoplopteryx from the Carlile Formation (Cretaceous) of South Dakota". Proceedings of the South Dakota Academy of Science. 95: 73–84.

External links Hoplopteryx in the Paleobiology Database

References

Illustrations

Hoplopteryx illustration
Hoplopteryx: Life restoration of H. lewesiensis
Life restoration of H. lewesiensis
Hoplopteryx: Specimens of H. syriacus from Lebanon
Specimens of H. syriacus from Lebanon

Worked examples

Example 1 — a first encounter with Hoplopteryx

Start with the simplest possible case. Write down what Hoplopteryx claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In biology, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Hoplopteryx before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Hoplopteryx ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Hoplopteryx

In research
Hoplopteryx appears in biology research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Hoplopteryx in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Hoplopteryx is common in secondary-school and first-year university syllabi. It links to neighbouring topics Campanian genera, Cenomanian genus first appearances, Coniacian genera, so understanding it makes those chapters shorter.
In everyday life
Look for Hoplopteryx outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Hoplopteryx in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Hoplopteryx means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Hoplopteryx out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Hoplopteryx in simple terms?

Hoplopteryx is an extinct genus of slimehead from the Late Cretaceous, lasting from the middle of the Cretaceous to the end. It is one of the best-known fossil trachichthyiforms, and was widespread across the Northern Hemisphere, from throughout Europe east to the Middle East and west to North Amer…

Why does Hoplopteryx matter?

Because it connects several biology ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Hoplopteryx?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Hoplopteryx.

Tags

  • Campanian genera
  • Cenomanian genus first appearances
  • Coniacian genera
  • Cretaceous fish of Europe
  • Fossil taxa described in 1838
  • Fossils of England
  • Fossils of France
  • Fossils of Germany
  • Fossils of Lebanon
  • Fossils of Russia
  • Fossils of Slovenia
  • Fossils of Spain

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