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London Clay
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The London Clay is a marine geological formation of Ypresian (Lower Eocene Epoch, c. 56-49 Ma) age which crops out in the southeast of England. The London Clay is well known for the fossils it contains. The fossils from the Lower Eocene indicate a moderately warm climate, the flora being tropical or subtropical. Though sea levels changed during the deposition of the Clay, the habitat was generally a lush forest - perhaps like in Indonesia or East Africa today - bordering a warm, shallow ocean.
The London Clay consists of a stiff, bluish coloured clay which becomes brown when weathered.

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Encyclopedia
The London Clay is a marine geological formation of Ypresian (Lower Eocene Epoch, c. 56-49 Ma) age which crops out in the southeast of England. The London Clay is well known for the fossils it contains. The fossils from the Lower Eocene indicate a moderately warm climate, the flora being tropical or subtropical. Though sea levels changed during the deposition of the Clay, the habitat was generally a lush forest - perhaps like in Indonesia or East Africa today - bordering a warm, shallow ocean.
The London Clay consists of a stiff, bluish coloured clay which becomes brown when weathered. Nodular lumps of pyrite and crystals of selenite frequently occur within the clay, and large septarian concretions are also common. These have been used in the past for the manufacturing of cement. They were once dug for this purpose at Sheppey, near Sittingbourne, and at Harwich, and also dredged off the Hampshire coast. The clay itself has been used commercially for making bricks, tiles, and coarse pottery. It is infertile for gardens and crops.
Distribution
The London Clay is well developed in the London Basin, where it thins westwards from around in Essex and north Kent to around in Wiltshire. though it is not frequently exposed as it is to a great extent covered by more recent neogene sediments and Pleistocene gravel deposits. One location of particular interest is Oxshott Heath, where the overlying sand and the London Clay layers are exposed as a sand escarpment, rising approximately 25 metres. This supported a thriving brick industry in the area until the 1960s. The London Clay is also well developed in the Hampshire Basin, where an exposure thick occurs at Whitecliff Bay on the Isle of Wight and around is spread along 6km of foreshore at Bognor Regis, West Sussex.
Formation
The clay was deposited in a sea up to deep at the eastern end. Up to five cycles of deposition (representing transgression followed by shallowing of the sea) have been found, most markedly at the shallower, western end. Each cycle begins with coarser material (sometimes including rounded flint pebbles), followed by clay which becomes increasingly sandy. The final cycle ends with the Claygate Beds.
Claygate Beds
The youngest part of the London Clay, known as the Claygate Beds or Claygate Member forms a transition between the clay and the sandier Bagshot Beds above. This is shown separately on many geological maps, and often caps hills. It is up to thick at Claygate, Surrey. It is now believed to be diachronous, with the formation at Claygate for example being the same age as the end of the fourth cycle of deposition further east.
Fossil fauna and flora
Notable coastal exposures from which fossils can be collected are on the Isle of Sheppey in Kent and Walton-on-the-Naze, Essex in the London Basin, and Bognor Regis in the Hampshire Basin.
Animal fossils include bivalves, gastropods, nautilus, worm tubes, brittle stars and starfish, crabs, lobsters, fish (including shark and ray teeth), reptiles (particularly turtles), and a large diversity of birds. A few mammal remains have also been recorded. Preservation varies; articulated skeletons are generally rare. Of fish, isolated teeth are very frequent. Bird bones are not infrequently encountered compared to other lagerstätten, but usually occur as single bones and are often broken.
Plant fossils, including seeds and fruits, may also be found in abundance. The flora demonstrates the much hotter climate of that time, with plants such as Nypa (Nipah palms) being frequently encountered. Plant fossils have been collected from the London Clay for almost 300 years. Some 350 named species of plant have been found, making the London Clay flora one of the world's most varied for fossil seeds and fruits.
Vertebrates
Mammals
Birds
Reptiles
Crocodilians
Snakes
Turtles and tortoises
- Allaeochelys - a pig-nosed turtle
- Argillochelys, Eochelone, Puppigerus and "Thalassochelys" sp. - true sea-turtles
- Chrysemys bicarinata and C. testudiniformis - pond turtles
- Eosphargis - a leatherback sea-turtle
- Homopus comptoni - a tortoise
- Lytoloma crassicostatum and L. planimentum - prehistoric sea-turtles
- Palaeaspis - an African sideneck turtle
- Podocnemis bowerbanki - an American sideneck turtle
- Trionyx pustulatus and T. sp. - softshell turtles
- Dacochelys and Pseudotrionyx - incertae sedis
Bony fish
- Acestrus elongatus, A. ornatus, Aglyptorhynchus sulcatus, A. venablasi, Xiphiorhynchus parvus and X priscus - swordfish relatives
- Acipenser toliapicus - a true sturgeon
- Albula oweni - a bonefish
- Ampheristus toliapicus - a scorpionfish
- Ardiodus marriotti - incertae sedis
- Argillichthys toombsi - a lancetfish relative
- Aulopopsis depressifrons, A. egertoni and Labrophagus esocinus - aulopuses
- Beerichthys ingens and B. sp. - Two species of luvar or luvar-like fish
- Bramoides brieni and Goniocranion arambourgi - pomfrets
- Brychaetus muelleri - an arowana
- Bucklandium diluvii - a naked catfish
- Cylindracanthus rectus and Hemirhabdorhynchus elliotti - Blochiidae
- Cymbium proosti, Eocoelopoma colei, E. curvatum, E. gigas, E. hopwoodi, Eothynnus salmoneus, Scombramphodon crassidens, S. sheppeyensis, Scombrinus macropomus, S. nuchalis, Sphyraenodus priscus, Tamesichthys decipiens, Wetherellus brevior, W. cristatus, W. longior and Woodwardella patellifrons - mackerel and tuna relatives
- Diodon sp. - a porcupinefish
- Egertonia isodonta and Phyllodus toliapicus - Phyllodontidae
- Elops sp., Esocelops cavifrons, Megalops oblongus, M. priscus, Promegalops sheppeyensis and P. signeuxae - ladyfish
- Enniskillenus radiatus - acanthomorph
- Eutrichurides winkleri - a cutlassfish
- Halecopsis insignis - Halecopsidae
- Laparon alticeps and Whitephippus tamesis - spadefish
- Lehmanamia sheppeyensis - a bowfin
- Myripristis toliapicus, Naupygus bucklandi and Paraberyx bowerbanki - soldierfish
- Percostoma angustum, Plesioserranus cf. wemmeliensi and Serranopsis londinensis - groupers
- Podocephalus curryi, P. nitidus, Sciaenuropsis turneri and Sciaenurus bowerbanki - porgies
- Progempylus edwardsi - a snake mackerel
- Pseudosphaerodon antiquus and P. navicularis - wrasses?
- Pycnodus bowerbanki and P. toliapicus - Pychnodontidae
- Rhinocephalus planiceps and Trichurides sagittidens - hakes
- Rhynchorhinus branchialis and R. major - Eccelidae
- Tetratichthys antiquitatis - a jack mackerel
Cartilaginous fish
- Abdounia beaugi, Carcharhinus sp. and Physogaleus secundus - requiem sharks
- Aetobatis irregularis, Burnhamia daviesi, Myliobatis dixoni, M. latidens, M. raouxi and M. toliapicus - eagle rays
- Anomotodon sheppeyensis - a goblin shark
- Carcharias hopei, Jackelotodus trigonalis, Odontaspis winkleri, Palaeohypotodus rutoti and Striatolamia macrota - sand sharks
- Edaphodon bucklandi and Elasmodus hunteri - chimaeras
- Dasyatis davisi and D. wochadunensis - stingrays
- Galeorhinus lefevrei, G. minor, G. recticonus, G. ypresiensis, Mustelus whitei and Triakis wardi - hound sharks
- Heterodontus vincenti, H. wardenensis and H. woodwardi - bullhead sharks
- Hexanchus agassizi, H. collinsonae, H. hookeri, Notorhynchus serratissimus and Weltonia burnhamensis - cow sharks
- Isisteus trituratus and Squalus minor - dogfish sharks
- Isurolamna affinis, Isurus nova, I. praecursor, Lamna inflata, L. lerichei, Otodus obliquus and Xiphodolamia eocaena - white sharks
- Megascyliorhinus cooperi, Scyliorhinus casieri, S. gilberti, S. pattersoni and S. woodwardi - catsharks
- Pararhincodon sp? - an indeterminate shark
- Raja sp.? - an indeterminate ray
- Squatina prima - an angel shark
Invertebrates
Crustaceans
- Archiocarabus bowerbanki, Callianassa sp., Hoploparia gammaroides, Linuparus eocenicus, L. scyllariformis, Scyllarides tuberculatus, Scyllaridia koenigi and Thenops scyllariformis - lobsters and shrimps
- Arcoscapellum quadratum, Scalpellum minutum and S. quadratum - barnacles
- Campylostoma mutatiforme, Cyclocorystes pulchellus, Dromilites bucklandi, D. lamarki, Glyphthyreus wetherelli, Goniochela angulata, Harpactoxanthopsis cf. quadrilo, Mithracia libinioides, Oediosoma ambigua, Portunites incerta, P. stintoni, Xanthilites bowerbanki, Zanthopsis bispinosa, Z. dufori, Z. leachei, Z. nodosa and Z. unispinosa - crabs
- Squilla wetherelli - a mantis shrimp
Molluscs
Cephalopods
- Aturia ziczac, Cimomia imperialis, Deltoidonautilus sowerbyi, Euciphoceras regale, Eutrephoceras urbanum, Hercoglossa cassiniana and Simplicioceras centrale - nautiluses
- Belopterina levesquei, Belosepia blainvillei and B. sepioidea - cuttlefish
Clams and other bivalves
Gastropods
- Acrilla cymaea, Foratiscala perforata, Litoriniscala scalaroides and Undiscala primaeva - wentletraps
- Aporrhais sowerbii and Eotibia lucida - true conchs
- Bathytoma granata, B. turbida, Clavatula conica, Cochlespira gyrata, Conolithus concinnus, Endiatoma cerithiformis, Fusiturris selysi, F. simillima, F. wetherelli, Gemmula koninckii, Hemipleurotoma fasciolata, H. prestwichi, Pseudotoma topleyi, Surculites errans, S. velatus, Turricula crassa, T. helix, T. latimarginata, T. nanodis, T. symmetrica and T. teretrium - Conoidea
- Bonellitia clathratum and B. laeviuscula - nutmeg shells
- Bullinella sp., Crenilabium elongatum, ?Roxiana sp., Scaphander ?parisiensis and Tornatellaea simulata - opisthobranchs
- Camptoceratops prisca, Spiratella mercinensis, S. taylori and S. tutelina - sea-butterflies
- Cassis striata and Mambrina gallica - tun shells
- Cepatia cepacea, Daphnobela juncea, Litiopa sulculosa, Orthochetus elongatus and Stellaxis pulcher - incertae sedis
- Eocypraea oviformis - a cowrie
- Euspira glaucinoides and Sinum clathratum - moon snails
- Falsifusus londini, Fusinus coniferus, F. wetherelli, Pseudoneptunea curta, Siphonalia highgatensis, Streptolathyrus triliniatus, S. zonulatus, Wrigleya complanata and W. transversaria - true whelks
- Ficopsis multiformis - a fig shell
- Lacunella sp. - a periwinkle
- Mathilda sororcula - Mathildidae
- Murex subcristatus and Paziella argillacea - murex snails
- Pachysyrnola sp. and Turbonilla subterranea - pyramid shells
- Patella sp. - Patellidae
- Ptychatractus aff. interuptus, Scaphella wetherelli and Volutospina nodosa - volutes
- Rilla cf. tenuistriata - Streptaxidae
- Ringicula turgida - Ringiculidae
- Sassia morrisi - a triton shell
- Sigapatella sp. - Calyptraeidae
- Tornus sp. and Turboella cf. misera - Rissoidae
- Xenophora extensum - a carrier shell
Tusk shells
- Antalis anceps and A. nitens
Echinoderms
- Asteropecten crispatus, Coulonia colei, Hemiaster bowerbanki, Hippasteria tuberculata, Ophioglypha wetherelli and Teichaster stokesii - starfish
- Coelopleurus wetherelli and Schizaster sp. - sea urchins
- Democrinus londinensis - crinoid
- ?Ophiacantha sp., Ophioglypha wetherelli, Ophiomusium sp. and Ophiura wetherelli - brittlestars
Cnidarians
- Paracyathus brevis and P. caryophyllus - corals
- Graphularia wetherelli - hydrozoan
Other invertebrates
- Adenellopsis wetherelli, Aimulosia sp., Batopora clithridiata, Beisselina sp., Cribrilina sp., Didymosella sp., Dittosaria wetherelli, Entalophora sp., Idmonia sp., Lunulites sp., Nellia sp., Pachythecella incisa, Vibracellina sp. and Websteria crissioides - bryozoans
- Hemiptera gen. et sp. indet. - true bug
- Lingula tenuis, Terebratulina striatula and T. wardenensis - lampshells
- Stelleta sp. - sponge
Ichnofossils
- Ditrupa plana, Rotularia bognorensis and Serpula trilineata - polychaete worm tubes?
- Scolithos
Engineering
The presence of a thick layer of London Clay underneath London itself, providing a soft yet stable environment for tunnelling, was instrumental in the early development of the London Underground. The high degree of shrinkage and swelling of the clay with varying degrees of wetness can cause subsidence problems.
Agriculture "London clay is not hospitable to most plants... ploughing it up where it lies so near the surface as to be accessible to the plough is injurious to the surface soil and future crops. In Middlesex it is called 'ploughing up poison'"
See also
Footnotes
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