|UNESCO World Heritage Site|
|Location||Darmstadt-Dieburg, Hesse, Germany|
|Inscription||1995 (19th Session)|
|Area||42 ha (4,500,000 sq ft)|
|Buffer zone||22.5 ha (2,420,000 sq ft)|
The Messel Pit (German: Grube Messel) is a disused quarry near the village of Messel (Landkreis Darmstadt-Dieburg, Hesse) about 35 km (22 mi) southeast of Frankfurt am Main, Germany. Bituminous shale was mined there. Because of its abundance of fossils, it has significant geological and scientific importance. After almost becoming a landfill, strong local resistance eventually stopped these plans and the Messel Pit was declared a UNESCO World Heritage Site on 9 December 1995. Significant scientific discoveries are still being made and the site has increasingly become a tourist site as well.
Brown coal and later oil shale was actively mined from 1859. The pit first became known for its wealth of fossils around 1900, but serious scientific excavation only started around the 1970s, when falling oil prices made mining the quarry uneconomical. Commercial oil shale mining ceased in 1971 and a cement factory built in the quarry failed the following year. The land was slotted for use as a landfill, but the plans came to nought and the Hessian state bought the site in 1991 to secure scientific access. In the few years between the end of mining and 1974, when the state began preparing the site for garbage disposal, amateur collectors were allowed to collect fossils. The amateurs developed the "transfer technique" that enabled them to preserve the fine details of small fossils, the method still employed in preserving the fossils today.
Many of the known specimens from the site have come from amateur collectors and in 1996, an amnesty on previously collected fossils was put in effect, in the hope of getting privately owned collections back into public ownership and available to science.
The current surface of the Messel pit is roughly 60 m (200 ft) below the local land and is about 0.7 km2 (0.27 sq mi) in area. The oil-shale bed originally extended to a depth of 190 m (620 ft). 47 million years ago in the Eocene when the Messel deposits formed, the area was 10° further south than it is now. The period was very close to the Paleocene–Eocene Thermal Maximum and the climate and ecology of the site were very different. A large series of lakes, surrounded by lush sub-tropical forests supported an incredible diversity of life. The Messel lake bed was probably a center point for drainage from nearby rivers and creeks.
The pit deposits were formed during the Eocene Epoch of the Paleogene Period about 47 million years ago, based on dating of basalt fragments underlying fossilbearing strata. Oil shale, formed by the slow anoxic deposition of mud and dead vegetation on the lake bed, is the primary rock at the site. Its sediments extend 13 m (43 ft) downward and lie atop an older sandstone foundation. The fossils within the shale show a remarkable clarity and preservation due to the unique depositional characteristics of the lake and so the Messel pit represents a Konservat-Lagerstätte. The upper stratifications of the lake most certainly supported a variety of organisms, but the bottom was subject to little disturbance by current, spawning a very anoxic environment. This prevented many epifaunal and infaunal species from inhabiting this niche and thus bioturbation was kept at a minimum. Overturn of the lake layers (caused by seasonal variations) lowered oxygen content near the surface and led to a periodic "die-off" of aquatic species. Combined with a relatively low rate of deposition, 0.1 mm (0.0039 in) per year, this provided a prime environment for the preservation of fauna and flora.
Volcanic gas releases
The area around the Messel Pit is believed to have been geologically and tectonically active during the Eocene. Leading scientists[who?] hypothesize[example needed] that events much like the 1986 volcanic gas releases at Lake Nyos, Cameroon, could account for the large deposition of non-aquatic species (Franzen & Koster, 1994). Periodic subsurface shifts possibly released large concentrations of reactive gases (such as carbon dioxide and hydrogen sulfide) into the lake and adjoining ecosystems, killing susceptible organisms. During these releases, birds and bats might have fallen in if near the lake surface and terrestrials could be overwhelmed when near the lake shore. Since the lake was very deep, animals that fell in it drifted downwards into oxygen- and bacteria-poor water, where they were preserved remarkably well, being overlaid by successive layers of mud that petrified later, thus producing an aggregation of fossils of exceptional quality, quantity, integrity, and variety. However, other hypotheses have been postulated as well, and have suggested a Cyanobacteria bloom origin resulting in the poisoning of the animals. This last one was considered to be necessary in order to explain the occurrence of excellent fossils throughout the entire sedimentary sequence (Koenigswald & others, 2004).
The Messel Pit provides the best preserved evidence of Geiseltalian flora and fauna so far discovered. Most other sites are lucky to contain partial skeletons, but Messel boasts extensive preservation of structural integrity, even going so far as to preserve the fur, feathers and "skin shadows" of some species. Unusual preservation has sparked some closely reasoned interpretations. The symptomatic "dumb-bell"-shaped bite marks on either side of the leaf vein on a fossilised leaf have been identified as the death-grip of a carpenter ant terminally parasitized by the fungus Ophiocordyceps unilateralis, that, apparently then as today, commandeered its behavior, in order to release its spores from a favourable location; it is the earliest concrete sample of fungal behavioural manipulation.
The diversity of species is remarkable partly as a result of the hypothesized periodic gas releases. A brief summary of some of the fossils found at the site follows:
- Nine mating pairs of fossil turtles have been found. The turtles, Allaeochelys crassesculpta, were in coitus (in the act of having sex). They are male-female pairs, with the male's tail tucked under the female, which is how they copulate. Their death must have been rapid. It is supposed that the turtles had started mating in the aerated surface waters of the ancient lake. As they sank into deeper water, they were overcome by the release of toxic volcanic gas. They were then buried in the lakebed sediment. Turtles belonging to this clade are still living. They have lost their reptilian scales, and their skin absorbs oxygen from the water. Normally, this is an advantage: it helps them stay submerged for long periods. However, under anoxic conditions it is a disadvantage, because carbon dioxide and dissolved poisons are absorbed as well.
- Over 10,000 fossilized fish of numerous species
- Thousands of aquatic and terrestrial insects, some with distinct coloration still preserved
- Innumerable small mammals including pygmy horses, large mice, primates, ground dwellers (hedgehogs, marsupials, pangolins), aardvark relatives and bats.
- Large numbers of birds, particularly predatory species.
- Crocodiles, frogs, turtles, salamanders and other reptiles or amphibians
- Remains of over 30 distinct plant species, including palm leaves, fruits, pollen, wood, walnuts and grapevines
The following is only a partial list:
- Darwinius masillae, identified in 2009 as an adapiform primate
- Kopidodon, an extinct arboreal cimolestan
- Leptictidium, an extinct omnivorous hopping mammal (of the leptictid family)
- Propalaeotherium, an early relative of horses
- Ailuravus, a rodent
- Peradectes, a metatherian
- Palaeochiropteryx, a bat
- Lesmesodon, a small hyaenodontid
- Eomanis, an early pangolin
- Eurotamandua, a scaleless, anteater-like pangolin
- Europolemur, a primate
- Hyrachyus, ancestor of rhinoceroses
- Paroodectes, an early carnivorous mammal
- Pholidocercus, an early hedgehog
- Macrocranion, an early long-tailed hedgehog
- Masillamys, an early rodent
- Messelobunodon, an early artiodactyl
- Godinotia, an early primate
- Buxolestes, a semiaquatic, otter-like cimolestan
- Palaeotis, an early struthionid
- Strigogyps sapea (formerly Aenigmavis) a cariamiform
- Eocoracias, an early coraciiform with known coloration
- Messelornis, the Messel-bird; a species of gruiform
- Masillastega, a freshwater sulid
- Lapillavis, a possible trogonid relative
- Cypseloramphus, a basal apodiform
- The Messelasturidae (Messelastur and Tynskya), carnivorous relatives of modern parrots
- Palaeoglaux, an early owl with enigmatic breast feathers
- Paraprefica, an early potoo
- Paraortygoides, a galliform
- Masillaraptor, an early falconiform
- Parargornis, an early apodiform
- Messelirrisor, a tiny bucerotiform closely related to hoopoes and wood-hoopoes
- Selmes (an anagram of "Messel"), a mousebird with stubby toes
- Gastornis (formerly Diatryma), a large, flightless anseriform
- Hassiavis, a member of Cypselomorphae
- Quasisyndactylus, a member of Alcediniformes
- Vanolimicola, a possible charadriiform
- A currently unnamed lithornithid, a sandpiper-like paleognath, the first record of its kind in Middle Eocene Europe.
- Asiatosuchus, a large crocodile
- Diplocynodon, an alligator
- Hassiacosuchus, a durophagous alligator
- Bergisuchus, a sebecosuchian crocodiliform
- Eoconstrictor, 2-m snakes related to Neotropical boas, Boinae
- Messelopython, the oldest known relative of pythons
- Cryptolacerta, a lizard with affinities to amphisbaenians
- Geiseltaliellus, a lizard with affinities to Corytophaninae
- Allaeochelys crassesculpta, aquatic turtles related to Carettochelys
- A bowfin, variously described as Amia (the modern genus) or Cyclurus
- Amphiperca, an early perch
- Palaeoperca, another early perch
- Atractosteus, a gar
- Casaleia eocenica
- Cephalopone - Cephalopone grandis and Cephalopone potens
- Cyrtopone - Cyrtopone curiosa, Cyrtopone elongata, Cyrtopone microcephala, and Cyrtopone striata
- Gesomyrmex pulcher
- Messelepone leptogenoides
- Pachycondyla eocenica
- Pachycondyla lutzi
- Pachycondyla? messeliana
- Pachycondyla parvula
- Pachycondyla petiolosa
- Pachycondyla petrosa
- Protopone - Protopone? dubia, Protopone germanica, Protopone magna, Protopone oculata, Protopone sepulta, and Protopone vetula
- Pseudectatomma - Pseudectatomma eocenica and Pseudectatomma striatula
- Titanomyrma gigantea
- Titanomyrma simillima
- Ailanthus confucii, tree of heaven
- Anacardium germanicum, cashew tree
- Camelliacarpoidea messelensis, Messel camellia
- Canarium, member of the incense tree family
- Cyclanthus messelensis, panama hat family
- Myristicacarpum, member of the nutmeg family
- Darmstadtia biseriata, a member of the trumpet creeper family Bignoniaceae
- Mytilaria boglei, witch-hazel family
- Sloanea messelensis, Elaeocarpaceae
Exhibits from the pit may be seen in the Messel town, the fossil Museum in Messel http://www.messelmuseum.de/index_museum.html, the Museum of Hessen in Darmstadt (5 km (3.1 mi) from Messel) and also the Senckenberg Museum in Frankfurt-am-Main (some 30 km (19 mi) from Messel). Casual visitors can park close to the pit and walk around 300 m (0.19 mi) to a viewing platform overlooking the pit. Entrance to the pit is only possible as part of a specially organized tour.
|Wikimedia Commons has media related to Messel Pit fossil site.|
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- "Home". www.grube-messel.de (in German). Retrieved 2018-05-13.
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- Krister T. Smith; Stephan F. K. Schaal; Jörg Habersetzer: MESSEL - An Ancient Greenhouse Ecosystem. Schweizerbart Science Publishers, Stuttgart, 2018. ISBN 978-3-510-61411-0