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Sannine Formation

Sannine Formation is a earth science 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 Sannine Formation rather than just read about it. In short: The Sannine Formation, also called the Sannine Limestone, is a Cretaceous geologic formation in Lebanon. It is a Konservat-Lagerstätte that contains a high diversity of well-preserved fish, reptiles, and invertebrates from the Tethys Ocean within its three main localities: Haqel (alternatively Hakel or Haqil), Hjoula (alternatively Hadjoula, Hajoula, or Hgula), and Nammoura (alternatively Namoura).

Sannine Formation — main illustration
Sannine Formation — illustration

Key takeaways

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

Reference excerpt

The Sannine Formation, also called the Sannine Limestone, is a Cretaceous geologic formation in Lebanon. It is a Konservat-Lagerstätte that contains a high diversity of well-preserved fish, reptiles, and invertebrates from the Tethys Ocean within its three main localities: Haqel (alternatively Hakel or Haqil), Hjoula (alternatively Hadjoula, Hajoula, or Hgula), and Nammoura (alternatively Namoura). It is one of three major Cretaceous lagerstätte in Lebanon, alongside the older (Barremian-aged) Lebanese amber and the younger (Santonian-aged) Sahel Aalma site. The Sannine Formation localities, combined with Sahel Alma, are together referred to as the "Fish Beds" of Lebanon.

Description It is primarily Cenomanian in age, with Haqel and Hjoula being late Cenomanian, while the slightly older Nammoura site is middle Cenomanian. Although Lebanon is now a part of Asia, the depositional environment for both formations would have been located off the coast of northern Africa during the Cretaceous, which would technically make their biota African rather than Asian.

The Cretaceous formations of Lebanon laterally vary from east to west; the western lowland "coastal" sequence (containing Sahel Aalma) is over 2000 metres thick and primarily consists of deep water limestone and chalk, while the eastern "mountain" sequence (containing the Sannine Formation) is 500–700 metres thick and consists of shallow water limestone. Two different shallow-water environments are preserved by the formation: Nammoura preserves a nearshore inner continental shelf environment with significant terrestrial input, while Haqel & Hjoula preserve an outer continental shelf environment. The neritic nature of these habitats contrasts with the other major marine lagerstätte of the region, Sahel Aalma, which is thought to have been deposited in a deepwater continental slope environment. Pterosaur fossils have been recovered from the formation, including those of Mimodactylus and Microtuban. The pythonomorphs Pontosaurus, Eupodophis and probably Aphanizocnemus are known from the formation. Insects are also known from compression fossils, including those of a dragonfly, enigmatic pond-skater like insect Chresmoda. and a mesoblattinid cockroach. Compression fossils of angiosperm Sapindopsis are also known. Numerous species of fossil fish are known, including the ionoscopid Spathiurus dorsalis and pycnodontid Flagellipinna rhomboides. An incredible diversity of fossil pycnodonts of various, highly unusual body plans is known, in addition to the earliest representatives of modern fish groups such as acanthomorphs, African butterflyfish and eels.

History

The Sannine Formation and its fossil fishes have been known of since Roman Phoenicia. The earliest mention of them is in the Chronicon by Eusebius around 314 CE (references to earlier mentions by Herodotus are thought to be apocryphal), who mentions fossil fishes commonly being found during quarrying operations in the mountains, and cites them as evidence of the Biblical Flood. The site that these fish were recovered from is thought to correspond to the modern Haqel site. Around 1250, fossil fishes were presented to Louis IX during the Seventh Crusade and documented by Jean de Joinville, although it remains uncertain whether these originated from Haqel or the younger Sahel Alma site. The first European to visit a Lebanese fossil fish locality in person was Cornelis de Bruijn in 1698, who illustrated a fossil fish that corresponds with the species Prionolepis cataphractus from Haqel. The first scientific presentation on the fossil fishes of Haqel was in 1703 at the French Academy of Sciences, and the first scientific studies were conducted by Henri Marie Ducrotay de Blainville in 1818. Lady Hester Stanhope collected and circulated fossil fishes from Haqel and Sahel Alma during the early 19th century, contributing to the study of these specimens by scientists such as Louis Agassiz. The Hadjoula site was only discovered in the late 19th century, and the Nammoura site in the early 20th century.

Paleobiota

Vertebrates

Jawless fish

Cartilaginous fish

Ray-finned fish

Lobe-finned fish

Amniotes

Invertebrates

Arthropods

Molluscs

Echinoderms

Annelids

Plants

See also List of pterosaur-bearing stratigraphic units Paleontology in Lebanon

References

Illustrations

Sannine Formation illustration
Sannine Formation: Map of Lebanon showing the locations of the 4 famous Upper Cretaceous Lagerstätten
Map of Lebanon showing the locations of the 4 famous Upper Cretaceous Lagerstätten
Sannine Formation: Diagram of the depositional environments of the Upper Cretaceous Sannine Formation Lagerstätten with a selection of iconic flora and fauna
Diagram of the depositional environments of the Upper Cretaceous Sannine Formation Lagerstätten with a selection of iconic flora and fauna
Sannine Formation illustration
Sannine Formation illustration

Worked examples

Example 1 — a first encounter with Sannine Formation

Start with the simplest possible case. Write down what Sannine Formation claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, 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 Sannine Formation 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 Sannine Formation 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 Sannine Formation

In research
Sannine Formation appears in earth science 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 Sannine Formation 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
Sannine Formation is common in secondary-school and first-year university syllabi. It links to neighbouring topics Cenomanian Stage, Cretaceous System of Asia, Fossiliferous stratigraphic units of Asia, so understanding it makes those chapters shorter.
In everyday life
Look for Sannine Formation 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 Sannine Formation in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Sannine Formation 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 Sannine Formation out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Sannine Formation in simple terms?

The Sannine Formation, also called the Sannine Limestone, is a Cretaceous geologic formation in Lebanon. It is a Konservat-Lagerstätte that contains a high diversity of well-preserved fish, reptiles, and invertebrates from the Tethys Ocean within its three main localities: Haqel (alternatively Hake…

Why does Sannine Formation matter?

Because it connects several earth science 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 Sannine Formation?

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 Sannine Formation.

Tags

  • Cenomanian Stage
  • Cretaceous System of Asia
  • Fossiliferous stratigraphic units of Asia
  • Geologic formations of Lebanon
  • Lagerstätten
  • Lagoonal deposits
  • Limestone formations
  • Marl formations
  • Paleontology in Lebanon
  • Shallow marine deposits

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