Messel pit explained

Whs:Messel Pit Fossil Site
Image Upright:1.2
Location:Darmstadt-Dieburg, Hesse, Germany
Criteria:(viii)
Id:720bis
Coordinates:49.9175°N 8.7567°W
Year:1995
Extension:2010
Area:42ha
Buffer Zone:22.5ha

The Messel pit (German: link=no|Grube Messel) is a disused quarry near the village of Messel (Landkreis Darmstadt-Dieburg, Hesse) about 35km (22miles) southeast of Frankfurt am Main, Germany. Bituminous shale was mined there. Because of its abundance of well-preserved fossils of the Messel Formation dating from the middle of the Eocene, it has significant geological and scientific importance.[1] Over 1000 species of plants and animals have been found at the site.[1] 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 about the early evolution of mammals and birds are still being made at the Messel pit, and the site has increasingly become a tourist site as well.[1]

History

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.[2]

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.

Depositional characteristics

The current surface of the Messel pit is roughly 60m (200feet) below the local land and is about 0.7km2 in area. The oil-shale bed originally extended to a depth of 190m (620feet).[3]

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:

The following is only a partial list:

Mammals

Darwinius masillae, identified in 2009 as an adapiform primate[10]

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

Messelogale, 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

Birds

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[11]

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,[12] a member of Cypselomorphae

Quasisyndactylus,[12] a member of Alcediniformes

Vanolimicola, a possible charadriiform[13]

A currently unnamed lithornithid, a sandpiper-like paleognath, the first record of its kind in Middle Eocene Europe.[14]

Reptiles

Asiatosuchus, a large crocodile

Diplocynodon, an alligator

Hassiacosuchus, a durophagous alligator

Bergisuchus, a sebecosuchian crocodiliform

Eoconstrictor, 2-m snakes related to Neotropical boas, Boinae[15]

Messelophis, a tiny, live-bearing or viviparous boa [16]

Messelopython, the oldest known relative of pythons[17]

Cryptolacerta, a lizard with affinities to amphisbaenians

Geiseltaliellus, a lizard with affinities to Corytophaninae

Allaeochelys crassesculpta, aquatic turtles related to Carettochelys

Fish

A bowfin, variously described as Amia (the modern genus) or Cyclurus

Amphiperca, an early perch

Palaeoperca, another early perch

Atractosteus, a gar

eel

Insects

Hemiptera
HymenopteraFamily Formicidae (ants)

Family Apidae

Family Megachilidae

IUGS geological heritage site

Describing the Messel Pit Fossil Site as 'richest geosite in the world for understanding the living environment of the Eocene, as it includes exceptionally well-preserved fossils', the International Union of Geological Sciences (IUGS) included the site's Eocene record in its list of 100 'geological heritage sites', published in October 2022. The organisation defines an IUGS Geological Heritage Site as 'a key place with geological elements and/or processes of international scientific relevance, used as a reference, and/or with a substantial contribution to the development of geological sciences through history.'[19]

Access

Exhibits from the pit may be seen in the Messel town,[20] the fossil Museum in Messel,[21] the Hessisches Landesmuseum in Darmstadt (5km (03miles) from Messel)[22] and also the Senckenberg Museum in Frankfurt am Main (some 30km (20miles) from Messel).[23] Casual visitors can park close to the pit and walk around to a viewing platform overlooking the pit. Entrance to the pit is only possible as part of a specially organized tour.

See also

Further reading

External links

Notes and References

  1. Web site: Messel Pit Fossil Site . UNESCO World Heritage Centre . United Nations Educational, Scientific, and Cultural Organization . 2 July 2022.
  2. Web site: The Messel Pit Fossil Site. 2 April 2015. https://web.archive.org/web/20130207192517/http://messel-fossils.eu/. 7 February 2013.
  3. Grein . Michaela . Utescher . Torsten . Wilde . Volker . Roth-Nebelsick . Anita . Reconstruction of the middle Eocene climate of Messel using palaeobotanical data . Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen . 1 June 2011 . 260 . 3 . 305–318 . 10.1127/0077-7749/2011/0139 . 12 July 2019.
  4. Mertz, D. F., Renne, P. R. (2005): A numerical age for the Messel fossil deposit (UNESCO World Heritage Site) derived from / dating on a basaltic rock fragment. Courier Forschungsinstitut Senckenberg no 255: pp 7–75.
  5. https://www.theguardian.com/science/2010/aug/18/zombie-carpenter-ant-fungus Guardian.com, "'Zombie ants' controlled by parasitic fungus for 48 m years"
  6. United Nations Environment Programme-World Conservation Monitoring Centre (Content Partner); Mark McGinley (Topic Editor). 2008. "Messel Pit fossil site, Germany." In: Encyclopedia of Earth. Eds. Cutler J. Cleveland (Washington, D.C.: Environmental Information Coalition, National Council for Science and the Environment). [First published in the Encyclopedia of Earth 29 November 2007; Last revised 8 July 2008; Retrieved 22 May 2009. [http://www.eoearth.org/article/Messel Pit fossil site, Germany article]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 Early Eocene Climatic Optimum and the climate and ecology of the site were very different, characterised by a mean annual temperature of 22°C and a large series of maar lakes surrounded by lush sub-tropical forests that supported an incredible diversity of life.[3] 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.[4] 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 13m (43feet) 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, 0.1mm per year, this provided a prime environment for the preservation of fauna and flora.

    Volcanic gas releases

    See main article: Limnic eruption. The area around the Messel Pit is believed to have been geologically and tectonically active during the Eocene. Leading scientists hypothesize 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).

    Fossils

    See main article: Paleofauna of the Messel Formation and Paleoflora of the Messel Formation.

    The Messel Pit provides the best preserved evidence of Geiseltalian flora and fauna so far discovered, with over 1000 species identified. 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.[5]

  7. Amos, Jonathan 2012. Turtles fossilised in sex embrace. BBC News: Science & Environment. https://www.bbc.co.uk/news/science-environment-18495102
  8. 10.1098/rsbl.2012.0361 . 22718955 . 3440985 . Caught in the act: The first record of copulating fossil vertebrates . Biology Letters . 8 . 5 . 846–8 . 2012 . Joyce . W. G . Micklich . N . Schaal . S. F. K . Scheyer . T. M .
  9. Habersetzer . J. . Storch . G. . Cochlea size in extant chiroptera and middle eocene microchiropterans from messel . Naturwissenschaften . October 1992 . 79 . 10 . 462–466 . 10.1007/BF01139198. 1992NW.....79..462H . 12463331 .
  10. Franzen, J. L., Gingerich, P. D., Habersetzer, J., Hurum, J. H., Von Koenigswald, W., & Smith, B. H. (2009). Complete primate skeleton from the middle Eocene of Messel in Germany: morphology and paleobiology. PLoS one, 4(5), e5723. https://doi.org/10.1371/journal.pone.0005723
  11. 10.1206/0003-0082(2002)360<0001:TFGBPF>2.0.CO;2 . 2002 . 360 . 1–14 . The Fossil Galliform Bird Paraortygoides from the Lower Eocene of the United Kingdom . American Museum Novitates . Dyke . Gareth J . Gulas . Bonnie E . 2246/2913 . 59131455 .
  12. http://www.senckenberg.de/files/content/forschung/abteilung/terrzool/ornithologie/hassiavis.pdf Mayr, G.. (2004). New specimens of Hassiavis laticauda (Aves: Cypselomorphae) and Quasisyndactylus longibrachis (Aves: Alcediniformes) from the Middle Eocene of Messel, Germany. CFS Courier Forschungsinstitut Senckenberg. 252. 23-28.
  13. 10.1016/j.annpal.2017.01.001 . A small, 'wader-like' bird from the Early Eocene of Messel (Germany) . Annales de Paléontologie . 103 . 2 . 141–7 . 2017 . Mayr . Gerald . 2017AnPal.103..141M .
  14. 10.1016/j.annpal.2007.12.004 . First substantial Middle Eocene record of the Lithornithidae (Aves): A postcranial skeleton from Messel (Germany) . Annales de Paléontologie . 94 . 1 . 29–37 . 2008 . Mayr . Gerald . 2008AnPal..94...29M .
  15. Scanferla, A. & K.T. Smith (2020) Exquisitely preserved snake fossils of Messel: insight into the evolution, biogeography, habitat preferences and sensory ecology of early boas. Diversity 12(3): 100. https://doi.org/10.3390/d12030100
  16. Chuliver, M., A. Scanferla & K.T. Smith (2022) Live birth in a 47-million-year-old snake. The Science of Nature – Naturwissenschaften 109: 56. https://doi.org/10.1007/s00114-022-01828-3
  17. Zaher, H. & K.T. Smith (2020) Pythons in the Eocene of Europe reveal a much older divergence of the group in sympatry with boas. Biology Letters 16: 20200735. https://doi.org/10.1098/rsbl.2020.0735
  18. Szwedo . J. . 2008 . A new tribe of Dictyopharidae planthoppers from Eocene Baltic amber (Hemiptera: Fulgoromorpha: Fulgoroidea), with a brief review of the fossil record of the family . Palaeodiversity . 1 . 75–85.
  19. Web site: The First 100 IUGS Geological Heritage Sites . IUGS International Commission on Geoheritage . IUGS . 13 November 2022.
  20. Web site: Home. www.grube-messel.de. de-de. 13 May 2018.
  21. Web site: Home . Fossilien- und Heimatmuseum Messel . 24 July 2022 . de . 30 December 2022.
  22. Web site: Messel Pit – Hessisches Landesmuseum. www.hlmd.de. en. 13 May 2018.
  23. Web site: SENCKENBERG world of biodiversity Museums Museum Frankfurt The Museum Exhibitions World natural heritage "... www.senckenberg.de. en. 13 May 2018. https://web.archive.org/web/20170924225030/http://www.senckenberg.de/root/index.php?page_id=14925. 24 September 2017. dead.

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