Aeger Libanensis
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Aeger Libanensis
''Aeger libanensis'' is a species of fossil prawn belonging to the family Aegeridae. These prawns had very long pereiopods. Fossil record Fossils of ''Aeger libanensis'' are found in the Cenomanian (Late Cretaceous) marine outcrops at Hjoula and Mayfouq Mayfouq ( ar, ميفوق) is a village and municipality in the Byblos District of Keserwan-Jbeil Governorate, Lebanon. It is located 64 km north of Beirut. Mayfouq has an average elevation of 860 meters above sea level and its total land area ... in Lebanon (age range: from 93.9 to 100.5 million years ago.). Bibliography * Alessandro GarassinoThe macraran decapod crustaceans of the Upper Cretaceous of Lebanon* Roger (J.), 1946 - Les invertébrés des couches à poissons du Crétacé supérieur du Liban. Mémoires de la Société géologique de France, t. 23, mém. 51, p. 1-92 * Víctor M. Bravo-Cuevas, Katia A. González-Rodríguez, Carlos Esquivel-Macías, Christopher FielitAdvances on Stratigraphy and Pal ...
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Liban
Lebanon ( , ar, لُبْنَان, translit=lubnān, ), officially the Republic of Lebanon () or the Lebanese Republic, is a country in Western Asia. It is located between Syria to the north and east and Israel to the south, while Cyprus lies to its west across the Mediterranean Sea; its location at the crossroads of the Mediterranean Basin and the Arabian hinterland has contributed to its rich history and shaped a cultural identity of religious diversity. It is part of the Levant region of the Middle East. Lebanon is home to roughly six million people and covers an area of , making it the second smallest country in continental Asia. The official language of the state is Arabic, while French is also formally recognized; the Lebanese dialect of Arabic is used alongside Modern Standard Arabic throughout the country. The earliest evidence of civilization in Lebanon dates back over 7000 years, predating recorded history. Modern-day Lebanon was home to the Phoenicians, a marit ...
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Fossil
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the ...
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Dendrobranchiata
Dendrobranchiata is a suborder of Decapoda, decapods, commonly known as prawns. There are 540 extant species in seven families, and a fossil record extending back to the Devonian. They differ from related animals, such as Caridea and Stenopodidea, by the branching form of the gills and by the fact that they do not brood their eggs, but release them directly into the water. They may reach a length of over and a mass of , and are widely shrimp fishery, fished and shrimp farm, farmed for human consumption. Shrimp and prawns While Dendrobranchiata and Caridea belong to different Order (biology), suborders of Decapoda, they are very similar in appearance, and in many contexts such as commercial farming and Fishery, fisheries, they are both often referred to as "shrimp" and "prawn" interchangeably. In the United Kingdom, the word "prawn" is more common on menus than "shrimp", while the opposite is the case in North America. The term "prawn" is also loosely used to describe any large s ...
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Aegeridae
Aegeridae is a family of fossil A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved ... prawns. It contains two genera, '' Aeger'' and '' Acanthochirana''. References Dendrobranchiata Prehistoric crustacean families Middle Triassic first appearances Late Cretaceous extinctions {{paleo-crustacean-stub ...
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Pereiopod
The decapod (crustaceans such as a crab, lobster, shrimp or prawn) is made up of 20 body segments grouped into two main body parts: the cephalothorax and the pleon (abdomen). Each segment may possess one pair of appendages, although in various groups these may be reduced or missing. They are, from head to tail: Cephalothorax Head # antennules # antennae #mandibles # first maxillae # second maxillae The head also bears the (usually stalked) compound eyes. The distal portion of a mandible or maxilla which has a sensory function is known as a palp. Thorax / pereon #first maxillipeds #second maxillipeds #third maxillipeds #first pereiopods #second pereiopods #third pereiopods #fourth pereiopods #fifth pereiopods Maxillipeds are appendages modified to function as mouthparts. Particularly in the less advanced decapods, these can be very similar to the pereiopods. Pereiopods are primarily walking legs and are also used for gathering food. They are also the ten legs from which decapods ...
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Cenomanian
The Cenomanian is, in the ICS' geological timescale, the oldest or earliest age of the Late Cretaceous Epoch or the lowest stage of the Upper Cretaceous Series. An age is a unit of geochronology; it is a unit of time; the stage is a unit in the stratigraphic column deposited during the corresponding age. Both age and stage bear the same name. As a unit of geologic time measure, the Cenomanian Age spans the time between 100.5 and 93.9 million years ago (Mya). In the geologic timescale, it is preceded by the Albian and is followed by the Turonian. The Upper Cenomanian starts around at 95 Mya. The Cenomanian is coeval with the Woodbinian of the regional timescale of the Gulf of Mexico and the early part of the Eaglefordian of the regional timescale of the East Coast of the United States. At the end of the Cenomanian, an anoxic event took place, called the Cenomanian-Turonian boundary event or the "Bonarelli event", that is associated with a minor extinction event for marine spec ...
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Late Cretaceous
The Late Cretaceous (100.5–66 Ma) is the younger of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''creta'', the Latin word for the white limestone known as chalk. The chalk of northern France and the white cliffs of south-eastern England date from the Cretaceous Period. Climate During the Late Cretaceous, the climate was warmer than present, although throughout the period a cooling trend is evident. The tropics became restricted to equatorial regions and northern latitudes experienced markedly more seasonal climatic conditions. Geography Due to plate tectonics, the Americas were gradually moving westward, causing the Atlantic Ocean to expand. The Western Interior Seaway divided North America into eastern and western halves; Appalachia and Laramidia. India maintained a northward course towards Asia. In the Southern Hemisphere, Australia and Ant ...
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Hjoula
Hjoula ( ar, حجولا) is a municipality in the Byblos District of Keserwan-Jbeil Governorate, Lebanon. It is 70 kilometers north of Beirut. Hjoula has an elevation of between 920 and 1,100 meters above sea level. Hjoula has a total land area of 528 hectares. The village of Hjoula is known for its fertile soil and its woods, as well as Early Cretaceous fossils. Etymology The word is an Aramaic one, however the meaning is uncertain. Most historians and linguists suggest it means "Oval" due to its oval shape, while some others speculate it comes from the Syriac root "G-l-a" and subsequently to the word "Guola" which supposedly means "The place of the wandering salesman". History Many old relics and monuments were found in Hjoula. There was found a Phoenician inscription in "Jarabta". A Roman statue that represented a shepherd and his sheep was also found beside the lake, and was dated to the era of emperor Tiberius c. 20 CE; along small sets of coins that were written in Kufic wi ...
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Mayfouq
Mayfouq ( ar, ميفوق) is a village and municipality in the Byblos District of Keserwan-Jbeil Governorate, Lebanon. It is located 64 km north of Beirut. Mayfouq has an average elevation of 860 meters above sea level and its total land area is 588 hectares. Its inhabitants are predominantly Maronite Catholics. Mayfouq is often praised for its natural environment and wildlife, and has large areas of forestry. It has been a common location for sight-seeing tourists who wish to look at wild animals such as hyenas and foxes. Mayfouq has a municipality as of 1998 and the current president is Hady EL-Hachach. Educational institutions in Mayfouq include the convent primary school and a secondary school. Mayfouq was the second Maronite Patriarchal location in Lebanon. There are a number of churches in the village, including Our Lady of Ilige, Our Lady of Mayfouq, Mart Moura, Al Sayde Kfarchelli, and many other deserted churches such Mar Saba, St Georges (Mar Girgis). Convents in ...
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Fossil Taxa Described In 1946
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the absolute ...
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