La Voulte-sur-Rhône

La Voulte-sur-Rhône is a commune in the Ardèche department in southern France.

La Voulte-sur-Rhône
La Voulte-sur-Rhône seen from across the river
Coat of arms
Location of La Voulte-sur-Rhône
La Voulte-sur-Rhône
La Voulte-sur-Rhône
Coordinates: 44°48′01″N 4°46′48″E
CountryFrance
RegionAuvergne-Rhône-Alpes
DepartmentArdèche
ArrondissementPrivas
CantonRhône-Eyrieux
IntercommunalityConfluences Drôme Ardèche
Government
  Mayor (20082014) Marc Bolomey
Area
1
9.70 km2 (3.75 sq mi)
Population
 (2017-01-01)[1]
4,987
  Density510/km2 (1,300/sq mi)
Time zoneUTC+01:00 (CET)
  Summer (DST)UTC+02:00 (CEST)
INSEE/Postal code
07349 /07800
Elevation85–405 m (279–1,329 ft)
(avg. 98 m or 322 ft)
1 French Land Register data, which excludes lakes, ponds, glaciers > 1 km2 (0.386 sq mi or 247 acres) and river estuaries.

Population

Historical population
YearPop.±%
17931,168    
18001,369+17.2%
18061,261−7.9%
18211,419+12.5%
18311,920+35.3%
18362,189+14.0%
18412,459+12.3%
18463,155+28.3%
18513,153−0.1%
18563,045−3.4%
18613,285+7.9%
18663,160−3.8%
18723,534+11.8%
18764,615+30.6%
18814,958+7.4%
18864,219−14.9%
18913,148−25.4%
18962,604−17.3%
19012,738+5.1%
19062,651−3.2%
19112,760+4.1%
19213,043+10.3%
19264,032+32.5%
19314,326+7.3%
19363,113−28.0%
19464,047+30.0%
19544,489+10.9%
19625,537+23.3%
19685,978+8.0%
19755,892−1.4%
19825,297−10.1%
19905,116−3.4%
19995,168+1.0%
20085,017−2.9%

Lagerstätte

La Voulte-sur-Rhône is a marine Lagerstätte (sedimentary deposit) located in France. It is Middle Jurassic (Callovian) in age, and is known for the variety of fossils it produces, including cephalopods, such as Proteroctopus ribeti, Rhomboteuthis lehmani, and Vampyronassa rhodanica. Fossilized cephalopods are rare, and Voulte-sur-Rhône is prized among paleontologists as one of only a few known localities known to produce such cephalopod fossils. Fossil preservation is by pyrite, a geologically rare process. Other sites with pyrite preserved fossils are Beecher's Trilobite Bed and the Hunsrück Slate.[2] Also found at the site are ophiuroids, crustaceans, fish, and other pyritized specimens.[3] The exceptional preservation of the fossils at this site is most likely due to the result of oxygen deficient water at the time of the deposition of the fossils, and possibly repeated sediment blanketing.[4]

See also

References

  1. "Populations légales 2017". INSEE. Retrieved 6 January 2020.
  2. Paul A. Selden; John R. Nudds (2005), Evolution of Fossil Ecosystems (PDF), University of Chicago Press, IL, p. 192, ISBN 978-0-226-74641-8, archived from the original (PDF) on July 14, 2011 see page 41
  3. (Bartels, Briggs, and Brassel 1998)
  4. (sensu Seilacher, Reif, and Westphal 1985)



This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.