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Topic: Lutetian

	Lutetian Stage , Paleogene Period in Hampshire - Hampshire Museums Service
		In Hampshire and the Isle of Wight the Lutetian stage (formerly known as the Middle Eocene) is represented by approximately 151 metres of sands and clays, collectively known as the Bracklesham Group.
		The Lutetian stage began with a shallow marine or brackish estuarine phase, which was followed by the marine phase known as the Earnley formation.
		The fossil fauna of the Lutetian is dominated by invertebrates, particularly molluscs.
	www.hants.gov.uk /museum/geology/periods/lutetian.html (271 words)

	- Overselling of Whale Evolution - (Site not responding. Last check: 2007-11-02)
		The Ypresian is dated from 56.5 to 50 mya, the Lutetian from 50 to 42.1 mya, the Bartonian from 42.1 to 38.6 mya, and the Priabonian from 38.6 to 35.4 mya.
		Rodhocetus and Indocetus are nearly contemporaneous fossils from the early Lutetian of the Domanda Formation in Pakistan (whereas Pakicetus and Ambulocetus are from the Kuldana Formation).
		Gingerich and others place it in the middle Lutetian, but the holotype was collected from the basal portion of the lower Mokattam Formation in Egypt, which some experts date to the early Lutetian.
	www.trueorigin.org /whales.asp (3394 words)

	International Geology Review (Site not responding. Last check: 2007-11-02)
		In the west of the Eastern Pontides the Lutetian basal aged (Pelin, 1977) sedimentary units that are interfingered with the volcanites, covered the older units and the Çimen Da ğ nappe with an unconformity (Figs.
		The cover units situated on the ophiolite-melange belt are composed of Lutetian flysch (Koçyiğit, l990) to the north of Erzincan in the west.
		Thrusting of the Munzur limestones to the south onto the Keban continent was contemporaneous with the ophiolite emplacement (Fig.
	www.istanbul.edu.tr /eng/jeoloji/deprem/kaf/elmas1.htm (7033 words)

	[No title]
		A diversity of plants and lower vertebrates is preserved at Mahenge (Herendeen and Jacobs 2000; Harrison et al.
		The fish assemblage from Mahenge suggests an early middle Eocene (Lutetian) age (Murray 2000).
		Tanzanycteris mannardi is a relatively small bat (Table 1) about the size of Palaeochiropteryx tupaiodon from the Lutetian of Europe (Habersetzer and Storch 1987).
	palaeo-electronica.org /2002_2/africa/bat.htm (936 words)

	Ypresian / Lutetian Boundary Stratotype (Site not responding. Last check: 2007-11-02)
		Originally, the Lutetian was defined by De Lapparent in 1883 and revised by Blondeau (1981), who proposed a new stratotype 50 km North of Paris.
		According to present knowledge, in term of planktic foraminifera the base of the Lutetian is close to the first appearance of the genus Hantkenina, which coincides with the base of the P10 Zone of Berggren et al.
		And in term of shallow benthic foraminifera the base of the Lutetian is approximately placed at the base of the SBZ13 Zone of Serra-Kiel et al.
	wzar.unizar.es /perso/emolina/ypresian.html (2012 words)

	[No title] (Site not responding. Last check: 2007-11-02)
		A late early Eocene (Ypresian) to early middle Eocene (Lutetian) age range for the Fossil Butte palynoflora is suggested by the co-occurrence of Bombacacidites, Eucommia, Pistillipollenites mcgregorii, Platycarya platycaryoides, and Momipites triradiatus.
		The results of this comparison confirm that most of the Fossil Butte palynoflora is late early Eocene (late Ypresian or Lostcabinian) in age as suggested by the occurrence of Lambdotherium in the middle unit (Froehlich and Breithaupt, 1997).
		The early middle Eocene age is suggested by a series of K-Ar age dates on a tuff (known as the "K-spar tuff" by Buchheim, 1994) in the uppermost part of the middle unit.
	www2.nature.nps.gov /geology/paleontology/pub/grd3_3/fobu3.htm (2377 words)

	Malatyna, a New Foraminiferal Genus from the Lutetian of Malatya Region (East Turkey), Geologia Croatica, 46/2, ... (Site not responding. Last check: 2007-11-02)
		Malatyna, a New Foraminiferal Genus from the Lutetian of Malatya Region (East Turkey), Geologia Croatica, 46/2, 181-188, Zagreb, 1993
		SIREL, E. Malatyna, a New Foraminiferal Genus from the Lutetian of Malatya Region (East Turkey)
		Malatyna drobneae n.gen.n.sp., a new nautiloid miliolid with cribrate aperture is found in the shallow water limestone (Upper Lutetian) of the Yesilyurt area, SW of Malatya.
	www.geologia-croatica.hr /abstract/gc-46-2-02.html (60 words)

	Journal of Paleontology: HARPACTOCARCINUS FROM THE EOCENE OF ISTRIA, CROATIA, AND THE PALEOECOLOGY OF THE ZANTHOPSIDAE ... (Site not responding. Last check: 2007-11-02)
		The "marls with crabs" have been assigned a lower middle Eocene, specifically middle Lutetian, age in the Floricici region (Juracic, 1979), from which we collected specimens of Harpactocarcinus (Drobne et al., 1979; Pavlovec et al., 1991; Cosovic and Drobne, 1998).
		Subsequently, an early Lutetian age was assigned to the "marls with crabs" in the regions of Buzet and Roc (Pavlovec and Pavsic, 1986) at localities from which we also collected specimens of Harpactocarcinus.
		The planktonic foraminifera Morozovella lehneri (Cushman and Jarvis, 1929) and "Globigerinatheka" senni (Beckmann, 1953) are typical of the P-11 Biozone (sensu Berggren et al., 1995) of Lutetian age.
	www.findarticles.com /p/articles/mi_qa3790/is_200507/ai_n14715379 (1152 words)

	S. Can Genc's web pages - AN EXAMPLE OF THE POST-COLLISIONAL MAGMATISM- Turkish Journal of Earth Science, 6, 33-42, ... (Site not responding. Last check: 2007-11-02)
		These fragments of the two collided continents were covered collectively by the continental-shallow marine sediments as a common cover during the Maastrichtian.
		However, the geologic data obtained from the region shows that there was no contemporary subduction system that to the magmatic activity may be associated with.
		Therefore the Lutetian magmatic rocks are evaluated to be the products of the post-collisional magmatism.
	atlas.cc.itu.edu.tr /~scangenc/abst07.html (260 words)

	Alpine deformation at the western termination of the Axial Zone, Southern Pyrenees (Site not responding. Last check: 2007-11-02)
		The Roncal formation was deposited during the Middle Lutetian [Puigdefàbregas and Sánchez Carpintero, 1978a,b], indicating a similar age for the Urzainqui thrust.
		Since the Larra thrust was probably active during Middle-Late Lutetian to Bartonian times [Montes, 1992] and the Gavarnie thrust during Priabonian to Rupelian times [Puigdefàbregas, 1975; Teixell, 1992], the Urzainqui thrust is most likely connected to the Larra floor thrust.
		The timing of this syntectonic sedimentation and activity of the Urzainqui thrust has a profound influence on the timing of the thrusting activity of the Ardibidipicua thrusts.
	www.virtualexplorer.com.au /2002/8/schellart/paper4.html (3373 words)

	DCT - Pedro Proença paper
		During this stage it occurs the emplacement of the sub-volcanic complexes of Sintra, Sines and Monchique, basaltic extrusions at Lisbon-Leiria region, diapirism and reactivation of the Nazaré-Lousã fault (uplift of the south-eastern block).
		During the upper Lutetian - lower Chattian structural stage, the relative motion between Iberia and Europe became convergent and the Pyrenean compression very intense.
		On the western border of the Hesperian Massif occurs an important distensive reactivation of NE-SW fractures, tilting the blocks to SW and developing elongated tectonic troughs perpendicularly to the imposed traction.
	www.uc.pt /cienterra/id/ppc/p10.html (2639 words)

	WADIA INSTITUTE OF HIMALAYAN GEOLOGY, DEHRA DUN (Site not responding. Last check: 2007-11-02)
		The study of biostratigrphic successions suggests that marine conditions commenced in Maastrichtian and continued till Early Lutetian during which the Kakara-Subathu succession was deposited.
		The first regression is related to collision between the two plates, which resulted in uplift of the region in the early Late Ypresian times during which the beds of Cordiopsis subathooensis-Turritella subathooensis Zone were deposited.
		The second regression which took place in the Early Lutetian time (47 Ma) is attributed to uplift of the region due to continued collision between the two plates during which beds of Musculus muttali-Parinomya blanfordiana Zone were deposited.
	mst.nic.in /dst/a_report/9900/wihgd.htm (1921 words)

	Bioerosion on the tests of Lutetian and Egerian corals - a comparison ("Coral-Ditch", Bajót and Wind ... (Site not responding. Last check: 2007-11-02)
		Traces of bioerosion occurring on the tests of solitary and colonial corals of Lutetian and Egerian age collected from two different Hungarian localities is compared.
		The number of specimens bearing traces of bioerosion are 214 among the Lutetian corals and 549 among the Egerian ones.
		Abundance and distribution of the traces show that the settlement of the endolithic animals could take place in different phases.
	www.pal.nhmus.hu /MFT/HOP/fodor.html (261 words)

	Journal of Paleontology: New species of protocetid archaeocete whale, Eocetus Wardii (Mammalia: Cetacea) from the ...
		Gaviacetus, and Takracetus are known from the Domanda Formation of Pakistan, which is early Lutetian in age (Gingerich, et al., 1995).
		Babiacetus is known from Drazinda Formation of Pakistan and the "gypseous shale bed of Babia Hills", India (Trivedy and Satsangi, 1984), both of which are late Lutetian in age (Gingerich et al., 1995).
		Georgiacetus is known from the latest Lutetian or earliest Bartonian "Blue Bluff" unit of the McBean Formation in Georgia (Hulbert et al., 1998), and the latest Lutetian or earliest Bartonian upper Santee Formation of South Carolina (Albright, 1996).
	www.findarticles.com /p/articles/mi_qa3790/is_199905/ai_n8830622 (1297 words)

	Sedimentological Society of Egypt - SSE (Site not responding. Last check: 2007-11-02)
		The Samalut Formation (Early to Middle Lutetian) has its lower part as a mound reefs, while open marine platform environment dominated during the depoaition of its upper part.
		The Rayan rocks (Late Lutetian) indicate deposition in an oscillating shelf that received siliciclastic and carbonate sediments.
		The Gebel Hof Formation (Late Lutetian) was probably deposited in a shallow subtidal environment.
	www.salty2k.com /sse/abstracts/vol9/SAYEDAHMED.html (158 words)

	ELASMO.COM Fossil Genera: Isurolamna - Extinct mackerel shark
		9) for a tooth in the Bories collection from the Early Lutetian of Fontas, near Fabrezan, in the Corbières region SW France.
		This tooth may actually be the second upper and the horizon may prove to be Late Ypresian (NP 12, not Lutetian).
		The name was used as a species, as opposed to a variety, by Leriche in 1936 (Leriche 1936a: 296) in a paper on reworked basal Oligocene teeth from NE Holland.
	www.elasmo.com /genera/cenozoic/sharks/isurolamna.html (1293 words)

	Sumarios varios
		Concerning the Lutetian deposist studied in the Amer-Vic and Empordà areas, four sedimentary cycles have been characterised.
		In the southeastern Ebro Foreland Basin, the marine deposits of Lutetian and Bartonian age show excellent out-crop conditions, with a grat lateral and horizontal continuity of lithostratigraphic units.
		This contribution is a sedimentary and biostratigraphic synthesis of the basic outcrop and section of the Lutetian and Bartonian marine and transitional deposits in the southeastern sector of the Ebro Foreland Basin.
	europa.sim.ucm.es:8080 /compludoc/AA?a=Saula&donde=otras&zfr=0 (573 words)

	MAGNETOSTRATIGRAPHY AND POLARITY CHRON ASSIGNMENTS (Site not responding. Last check: 2007-11-02)
		Measurements with the shipboard pass-through magnetometer suggest that a sliver of polarity Zone C21r of basal Lutetian (lowermost middle Eocene) may be present below the lower Lutetian hiatus spanning the majority of Chron C21r and all of Chron C21n.
		The upper Lutetian portion of the middle Eocene is represented by polarity Chrons C20r, C20n, C19r, and C19n.
		The middle Eocene Lutetian and Bartonian stages are relatively expanded, and the magnetostratigraphy pattern displays an excellent record of polarity Chrons C21n through C17n, including indications of the brief Subchrons C17n.1r and C17n.2r within polarity Chron C17n (Fig.
	www.ga.gov.au /odp/publications/171B_SR/chap_09/c9_4.htm (2950 words)

	Gosport area, South Hampshire - Geological Localities in Hampshire - Hampshire Museums Service
		Access to the geology of the Paleogene (Ypresian, Lutetian and Bartonian stages) underlying the Gosport area has been restricted to engineering contracts and coastal localities.
		Temporary localities in the area include outfall pipe excavations into various parts of the Lutetian stage between Shoot Lane and Browndown and pumping station excavations into the Ypresian stage at Brewers Lane.
		The Lutetian and Bartonian stage, localities at Lee-on-the-Solent and Elmore were buried by engineering work in 1997.
	www.hants.gov.uk /museum/geology/locality/gosport.html (163 words)

	Implications of Magnetostratigraphic Correlations
		The basal Lutetian is represented by a hiatus across the margin, and there are indications of erosion of the uppermost Ypresian and differences of timing of resumption of sedimentation at the various sites.
		Above this basal Lutetian hiatus, the thickness pattern of individual polarity zones (e.g., polarity zones corresponding to Chrons C20r and C20n) display the typical seaward thinning.
		This end Lutetian event is also reflected as a minor hardground in the cored sediments of Site 1052.
	owen.nhm.ac.uk /odp/publications/171B_SR/chap_09/c9_6.htm (1051 words)

	Aznag (Ouarzazate basin, Morocco), a new African middle Eocene (Lutetian) vertebrate-bearing locality with selachians ... (Site not responding. Last check: 2007-11-02)
		Aznag (Ouarzazate basin, Morocco), a new African middle Eocene (Lutetian) vertebrate-bearing locality with selachians and mammals -- Tabuce et al.
		Aznag (Ouarzazate basin, Morocco), a new African middle Eocene (Lutetian) vertebrate-bearing locality with selachians and mammals
		Lutetian Aznag locality represents the only known Eocene mammalian
	bsgf.geoscienceworld.org /cgi/content/abstract/176/4/381 (633 words)

	SVIBOR - Papers - project code: 1-09-084
		Uneven chemical composition of the Eocene bauxites, their sporadic occurrences in developed paleorelief and characteristic paleogeographic composition of the immediate overlying rock, point out at different genetical conditions during the time when they were formed.
		Sediments from the Ragancini-Liani, Osp and terna sections, thanks to accompanied macroforaminifera were assigned as the Early Lutetian, while those from the Piæan section belong to the Middle Lutetian in age.
		Late Lutetian, the largest part of the flysch deposits belongs to the Bartonian (NP-17), while near Oprtalj city, deposits are indentified as the Late Eocene in age (NP-18).
	www.mzos.hr /svibor/1/09/084/rad_e.htm (4339 words)

	Creation Matters May/June 1998, Vol. 3, No. 3
		In the standard scheme (Figure 1), Pakicetus inachus is dated to the late Ypresian, but several experts acknowledge that it may date to the early Lutetian.
		[18] If the younger date (early Lutetian) is accepted, then Pakicetus is nearly, if not actually, contemporaneous with Rodhocetus, an early Lutetian fossil from another formation in Pakistan.
		According to the standard scheme, Protocetus is dated to the middle Lutetian, but some experts have dated it in the early Lutetian.
	www.creationresearch.org /creation_matters/98/cm9805.html (4680 words)

	Palaeos Vertebrates: Glossary H-I
		Habib Rahi Formation: Middle Eocene (Lutetian) of Pakistan.
		Neither true nor false, Haeckel's Law remains an important tool in understanding and analyzing phylogenetic problems.
		Harudi Formation: Middle Eocene (Lutetian) of far western India (Gujarat).
	www.palaeos.com /Vertebrates/Lists/Glossary/GlossaryHI.html (3910 words)

	Philadelphia Rare Books and Manuscripts: Erotica (Site not responding. Last check: 2007-11-02)
		privately (by Charles Carrington) for the Lutetian Bibliophiles’ Society, 1900.
		There seem to have been two Lutetian Bibliophiles’ issues of this anthology of curiosa, both dated 1900, one with the publishing location given as London and one with London and Paris; the latter is described as having a title-page reading “Weird Woman” [sic].
		The collations of both recorded issues match, as do their internal statements noting the edition limitation.
	www.prbm.com /interest/erotica.shtml (460 words)

	ELASMO.COM Fossil Genera: PRISTIDAE - Extinct sawfishes
		[Lutetian, Lwr-Upr Eocene Anglo-Franco Basin and North Africa], P.
		lathami in the Woodstock Member of the Nanjemoy (Ypresian) and the Piney Point Formation (Lutetian) of Maryland and Virginia.
		Teeth of this species have been collected from the Castle Hayne Formation (Middle Eocene) of North Carolina.
	www.elasmo.com /genera/cenozoic/batoids/pristid.html (1771 words)

	Bartonian Stage -- Encyclopædia Britannica (Site not responding. Last check: 2007-11-02)
		Together with the underlying Lutetian Stage, it constitutes the Middle Eocene; the Bartonian is overlain by the Priabonian Stage.
		the second of four stages in the Eocene Series, representing all those rocks deposited on a global basis during the Lutetian Age (52 to 43.6 million years ago).
		Together with the overlying Bartonian Stage, the Lutetian Stage constitutes the Middle Eocene.
	www.britannica.com /eb/article-9001598 (839 words)

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