European land mammal age


The European Land Mammal Mega Zones are zones in rock layers that have a specific assemblage of fossils based on occurrences of fossil assemblages of European land mammals. These biozones cover most of the Cenezoic, with particular focus having been paid to the Neogene and Paleogene systems, the Quaternary has several competing systems. In cases when fossils of mammals are abundant, stratigraphers and paleontologists can use these biozones as a more practical regional alternative to the stages of the official ICS geologic timescale. European Land Mammal Mega Zones are often also confusingly referred to as ages, stages, or intervals.

Biostratigraphic methods

Mammal zones were, like all biozones, established using geographic place names where fossil materials were obtained. The basic unit of measure is the first/last boundary statement. This shows that the first appearance event of one taxon is known to predate the last appearance event of another. If two taxa are found in the same fossil quarry or at the same stratigraphic horizon, then their age-range zones overlap.
The terrestrial stratigraphy of the Cenozoic is more difficult than that of marine deposits. The geologic timescale of the ICS is therefore based on marine fossils, that don't occur in terrestrial sediments. This makes the correlation of terrestrial deposits with the ICS timescale often difficult. Correlation is possible when marine deposits interfinger with terrestrial deposits, but this isn't the case everywhere. A fine stratigraphic division of the terrestrial record can in most places only be made using fossils of land species. Small mammals are often the best choice as they are quite abundant in the terrestrial record, especially their teeth. Teeth have an even better chance of preservation than bones.
The European mammalian biozones were established for the Paleogene and Neogene separately. Some of these, especially for the Neogene, were already established in the 19th century. The Villafranchian was, for example, introduced by Lorenzo Pareto in 1865. A finer subdivision was established by Pierre Mein in 1975, who divided the Neogene in 17 zones, known as the MN zonation, indicated by the letters MN and a number.
Similarly, a more detailed subdivision for the Paleogene period was established. There are 30 such Mammal Paleogene zones.

Paleogene European mammal zones

There are 30 Mammal Paleogene zones covering the Paleogene.

Neogene European mammal zones

European Land Mammal Mega Zones most often have their bases at first appearances of a certain species or genus. The numbers are higher for younger zones. Due to a redefinition of the boundary between the Neogene and Quaternary periods, MN 17 is now in fact considered a Quaternary biozone.
BiozoneSmall mammalsLarge mammals
MN 17Kislangia gusi, Mimomys tornensis, Mimomys pliocaenicus, Mimomys reidiEucladoceros
MN 16Kislangia ischus, Mimomys polonicus, Kislangia cappettai, Mimomys hajnackensisEquus, Mammuthus, Homotherium, Megantereon, Ursus etruscus,
Pliohyaena perrieri, Gazellospira torticornis, Arvernoceros ardei, Hesperidoceras merlai, Cervus perrieri
MN 15Mimomys occitanus, Oryctolagus, Mimomys vandemeuleni, Mimomys davakosiChasmaporthetes lunensis
MN 14Promimomys, Trilophomys, Celadensia, Castor Sus arvernensis, Croizetoceros, Acinonyx, Felis issiodorensis
MN 13Paraethomys, Rhagapodemnus, Stephanomys, Apodemus, ApocricetusParabos, Paracamelus, Agriotheirum, Apocricetus, Nyctereutes, Hexaprotodon
MN 12Parapodemus barbarae, Huerzelerimys turoliensisPliocervus, Hispanodorcas, Palaeoryx, Occitanomys adroveri, Procapreolus
MN 11Parapodemus lugdunensis, Huerzelerimys vireti, Occitanomys sondaariBirgerbohlinia, Lucentia
MN 10Rotundomys, Pliopetaurista, Schreuderia, Progonomys cathalaiHyaenictis almerai, Adcrocuta eximia, Microstonyx major, Tragoportax gaufryi
MN 9CricetulodonHippotherium, Decennatherium, Machairodus
MN 7/8Megacricetodon ibericus, Megacricetodon gregariusParachleuastochoerus, Propotamochoerus, Palaeotragus, Protragocerus, Tetralophodon
MN 6Megacricetodon crusafonti, Megacricetodon gersiTethytragus, Hispanomeryx, Euprox, Listriodon
MN 5Megacricetodon collongensisMiotragocerus, Micromeryx, Heteroprox, Hispanotherium
MN 4Megacricetodon primitivusBunolistriodon, Dorcatherium, Chalicotherium, Eotragus, Prodeinotherium
MN 3Gomphotherium, Procervulus, Lagomeryx, Actoocemas, Palaeomeryx, Brachyodus, Anchitherium, Aureliachoerus, Hemicyon
MN 2Ligerimys, Prolagus, Lagopsis, Ritterneria mancaTeruelia, Lorancameryx, Oriomeryx, Pseudaelurus, Xenohyus, Andegameryx, Amphitragulus
MN 1Rhodanomys schlosseri, VasseuromysHyotherium

Quaternary European mammal zones

The first zonation for the Quaternary of Europe was proposed by Azzaroli in 1967. This was then expanded by Gliozzi et al. in 1997 to make a system of 3 'ages' subdivided into 13 'faunal units'. The scheme does not define boundaries but instead is accompanied by a range chart, where the entry and exit dates for the taxa are indicated. Each zone is named after a reference locality. Most of the reference locations are in Italy but the scheme is used in other European regions. The mammal ages and Faunal Units after Gliozzi et al. are:
Mammal AgeFaunal Unitsub-ageLarge Mammals
Villafranchian
TriversaEarly VillafranchianStepbanorhinus megarhinus, Sus minor, Alephis liryx, Felsinotherium gervaisi
Villafranchian
MontopoliEarly VillafranchianMammuthus gromwi, Equus lioenzwensi, Stephanorhinus etruscus
Villafranchian
Costa S. GiacomoMiddle VillafranchianCanis, Sus strozzii, Leptobos furtivus, Hystrix refossa, Gazellospira torticomis, Anancus arvernensis
Villafranchian
OlivolaLate VillafranchianPachycrocuta brevirostris, Panthera gombaszoegensis, Procamptoceras brivatense, Eucladoceros dicranios, Eucladoceros nestii, Pseudodama, Canis etruscus
Villafranchian
TassoLate VillafranchianHippopotamus antiquus, Praevibos, Leptobos vallisarni, Equus stehlini, Canis arnensis, Canis falconeri
Villafranchian
FarnettaLate VillafranchianLeptobos vallisarni, Eucladoceros dicranios, Eucladoceros nestii, Megaceroides obscurus, Microtus
Villafranchian
Piro NordLate VillafranchianBison, Megaceroides solilbacus
Galerian
Colle CurtiEarly GalerianEquus altidens, Equus bressanus, Equus sussenbornensis, Megaceroides verticornis
Galerian
SilviaMiddle GalerianCervus elaphus acoronatus
Galerian
IserniaMiddle GalerianPanthera leo, Palaeoloxodon antiquus, Mammuthus trogontherii, Stephanorhinus hundsheimensis, Megaloceros savini, Bos, Bison schoetensacki, Equus caballus, Pseudodama
Galerian
Fontana RanuccioLate GalerianHomotherium latidens, Cervus elaphus eostephanoceros, Dama clactoniana, Equus altidens, Equus sussenbornensis
Aurelian
Torre in PietraEarly AurelianCanis lupus, Ursus spelaeus, Megaloceros giganteus, Cervus elaphus rianensis
Aurelian
VitiniaMiddle AurelianDama dama tiberina, Equus hydruntinus
Aurelian
none designatedLate AurelianDama dama dama, Capra ibex, Coelodonta antiquitatis, Mammuthus primigenius

In 1982, Guérin proposed an alternative scheme, which extended the MN zonation scheme for the Neogene with additional units to cover the Quaternary. There have been further updates since. The MNQ scheme added an additional 12 units in total, MNQ 16–27.
For small mammals there is a third scheme, the MmQ, published by Agustí, Moyà‐Solà, and Pons‐Moyà in 1987. The scheme includes some large mammals for reference and thus has a wider application.

Other continental mammalian biozones