lulu devine Un Official Fan Site Tribute

lulu devine : This Is An Un Official Fan Site Tribute
lulu divine Lulu Devine, Lulu Divine
Porn Queen Actress Superstar

lulu devine

PERFORMER AKA Lulu Devine, Lulu Divine BIRTHDAY November 17, 1955 (64 years old) ASTROLOGY Scorpio BIRTHPLACE Boston, MA YEARS ACTIVE 1990-1998 (Started around 35 years old)
Lulu Devine (born Cynthia Stathopoulos on November 17, 1955 in Boston, Massachusetts) is a former American big-bust feature dancer, model, and pornographic video actress. Lulu turned to dance as a feature dancer during the late 1980s, and by 1990 began a pornographic video career. Lulu is also the older sister of fellow big-bust feature dancer and porn actress Toppsy Curvey.

Contents 1 Talk show, magazine appearances 2 "Bandito" sports game crashing runs 3 Police charges 4 References 5 External links Talk show, magazine appearances Lulu has appeared on numerous talk shows, such as (Jerry Springer Show, The Jenny Jones Show), The Howard Stern Show, and The Sally Jessy Raphael Show and also has made appearances at the Adult Entertainment Expo with fellow big-bust performers Chelsea Charms, Minka, and Kayla Kleevage. Devine has appeared in men's magazines such as Score, Gent, Hustler's Busty Beauties, and D-Cup Magazine. "Bandito" sports game crashing runs Devine is the older sister of fellow big-bust feature entertainer and adult model Toppsy Curvey. In the Tampa area, Lulu is also notoriously recognized in local pro sports circles for her "Kissing Bandit" routine, made famous by former "Kissing Bandit", TV personality, big-bust model and three-time Playboy centerfold Morganna Roberts. Numerous times in the past she has accompanied her sister Toppsey on her "bandito" runs, as to where she and her sister Lulu would run out on the fields during Tampa Bay Rays baseball and Tampa Bay Buccaneers pro football games and kiss the players. Police charges In early 2005, Hillsborough County, Florida sheriff's deputies raided her Brandon house and arrested her on a misdemeanor charge of prostitution. She was surprised, she said when officials announced the discovery of a "dungeon" in her two-bedroom home in a working-class neighborhood. After posting $250 bail, Devine gave an interview at her dining room table that Friday morning. She was later convicted and fined, then released. The story gained national attention and was shown on various television news media affiliate broadcasts, as well as tabloid journalism sources.[1] 1998 Chessie Moore NonSex 1 D Busen Extra 2 1990 Big Top Video DO Girls Around the World 3: D-Cup Holiday 1990 Big Top Video MastOnly DRO Incredible Sisters 1994 Big Top Video NonSex O Lesbians In Heat 1998 VSP LezOnly DO On Location in Palm Springs 1996 Big Top Video NonSex One of its main aims, a project begun in 1974, is to establish a multidisciplinary standard and global geologic time scale that will ease paleontological and geobiological comparisons region to region by benchmarks with stringent and rigorous strata criteria called Global Boundary Stratotype Section and Points (GSSPs) within the fossil record. (i.e. section of the rock record as of a core sample section or accessible exposed strata, which when a core sample are usually "trayed" in long pieces, also called "sections" about a meter in length.) Methodology Additionally the ICS defines an alternative type of benchmark and criteria called Global Standard Stratigraphic Ages (GSSAs) where the characteristics and dating criteria set solely by physical sciences methods (such as magnetic alignment sequences, radiological criteria, etcetera.) as well as encouraging an international and open debate amongst Earth scientists in the paleontology, geology, geobiology and chronostratigraphy fields, among others. The International Commission on Stratigraphy has spawned numerous subcommittee level organizations organized and mobilized on a local country-wide or regional basis that are the true working committees of the IUGS, and these do the field work, basis comparisons in conference or co-ordination research committee meetings of local or wide-scale scope. Publications The ICS publishes various reports and findings as well as revised references periodically, summarized in the International Stratigraphic Chart, a combined working proposal and guideline-to-date released after the last ICS deliberations prior to the upcoming (next) meeting of the IUGS. Until the IUGS accepts the recommendations, they are unofficial since the IUGS parent approves or dismisses the individual deliberation reports of the ICS, which are presented as recommendations, and span dating and strata selection criteria, and related issues including nomenclatures. In de facto everyday matters, the deliberative results reported out of any meetings of the ICS are widely accepted and immediately enter everyday use, except in the rare cases where they result in a strong body of dissenting opinion, which matters are resolved before the full IUGS. One such controversy arose in 2009 when the ICS deliberated and decided that the Pliocene Series of the current but unofficially named Quaternary Period should be shifted into the Neogene System and Neogene Period.[2] Despite the strong debate,[3] the Quaternary saw official ratification as a geological unit from the IUGS in June 2009, placing its lower boundary to the Gelasian Stage/Age at Monte San Nicola, Sicily, Italy (until then uppermost part of the Pliocene Series/Epoch, and thus of the Neogene System/Period), 2.58 Ma BP.[4] Logo The logo of International Commission on Stratigraphy was designed after the Chinese character of "mountain". The Neogene ( /'ni?.??d?i?n, 'ni?.o?-/ NEE-?-jeen, NEE-oh-)[3][4] (informally Upper Tertiary or Late Tertiary) is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period 23.03 million years ago (Mya) to the beginning of the present Quaternary Period 2.58 Mya. The Neogene is sub-divided into two epochs, the earlier Miocene and the later Pliocene. Some geologists[who?] assert that the Neogene cannot be clearly delineated from the modern geological period, the Quaternary. The term "Neogene" was coined in 1853 by the Austrian palaeontologist Moritz Hörnes (1815–1868).[5] During this period, mammals and birds continued to evolve into modern forms, while other groups of life remained relatively unchanged. Early hominids, the ancestors of humans, appeared in Africa near the end of the period.[citation needed] Some continental movement took place, the most significant event being the connection of North and South America at the Isthmus of Panama, late in the Pliocene. This cut off the warm ocean currents from the Pacific to the Atlantic Ocean, leaving only the Gulf Stream to transfer heat to the Arctic Ocean. The global climate cooled considerably over the course of the Neogene, culminating in a series of continental glaciations in the Quaternary Period that follows. Contents 1 Divisions 2 Geography 3 Climate 4 Flora and fauna 5 Disagreements 6 References 7 External links Divisions In ICS terminology, from upper (later, more recent) to lower (earlier): The Pliocene Epoch is subdivided into 2 ages: Piacenzian Age, preceded by Zanclean Age The Miocene Epoch is subdivided into 6 ages: Messinian Age, preceded by Tortonian Age Serravallian Age Langhian Age Burdigalian Age Aquitanian Age In different geophysical regions of the world, other regional names are also used for the same or overlapping ages and other timeline subdivisions. The terms Neogene System (formal) and Upper Tertiary System (informal) describe the rocks deposited during the Neogene Period. Geography The continents in the Neogene were very close to their current positions. The Isthmus of Panama formed, connecting North and South America. The Indian subcontinent continued to collide with Asia, forming the Himalayas. Sea levels fell, creating land bridges between Africa and Eurasia and between Eurasia and North America. Climate The global climate became seasonal and continued an overall drying and cooling trend which began at the start of the Paleogene. The ice caps on both poles began to grow and thicken, and by the end of the period the first of a series of glaciations of the current Ice Age began. Flora and fauna Marine and continental flora and fauna have a modern appearance. The reptile group Choristodera became extinct in the early part of the period, while the amphibians known as Allocaudata disappeared at the end. Mammals and birds continued to be the dominant terrestrial vertebrates, and took many forms as they adapted to various habitats. The first hominins, the ancestors of humans, may have appeared in southern Europe and migrated into Africa.[6][7] In response to the cooler, seasonal climate, tropical plant species gave way to deciduous ones and grasslands replaced many forests. Grasses therefore greatly diversified, and herbivorous mammals evolved alongside it, creating the many grazing animals of today such as horses, antelope, and bison. Eucalyptus fossil leaves occur in the Miocene of New Zealand, where the genus is not native today, but have been introduced from Australia.[8] Disagreements The Neogene traditionally ended at the end of the Pliocene Epoch, just before the older definition of the beginning of the Quaternary Period; many time scales show this division. However, there was a movement amongst geologists (particularly marine geologists) to also include ongoing geological time (Quaternary) in the Neogene, while others (particularly terrestrial geologists) insist the Quaternary to be a separate period of distinctly different record. The somewhat confusing terminology and disagreement amongst geologists on where to draw what hierarchical boundaries is due to the comparatively fine divisibility of time units as time approaches the present, and due to geological preservation that causes the youngest sedimentary geological record to be preserved over a much larger area and to reflect many more environments than the older geological record.[9] By dividing the Cenozoic Era into three (arguably two) periods (Paleogene, Neogene, Quaternary) instead of seven epochs, the periods are more closely comparable to the duration of periods in the Mesozoic and Paleozoic eras. The International Commission on Stratigraphy (ICS) once proposed that the Quaternary be considered a sub-era (sub-erathem) of the Neogene, with a beginning date of 2.58 Ma, namely the start of the Gelasian Stage. In the 2004 proposal of the ICS, the Neogene would have consisted of the Miocene and Pliocene epochs.[10] The International Union for Quaternary Research (INQUA) counterproposed that the Neogene and the Pliocene end at 2.58 Ma, that the Gelasian be transferred to the Pleistocene, and the Quaternary be recognized as the third period in the Cenozoic, citing key changes in Earth's climate, oceans, and biota that occurred 2.58 Ma and its correspondence to the Gauss-Matuyama magnetostratigraphic boundary.[11][12] In 2006 ICS and INQUA reached a compromise that made Quaternary a subera, subdividing Cenozoic into the old classical Tertiary and Quaternary, a compromise that was rejected by International Union of Geological Sciences because it split both Neogene and Pliocene in two.[13] Following formal discussions at the 2008 International Geological Congress in Oslo, Norway,[14] the ICS decided in May 2009 to make the Quaternary the youngest period of the Cenozoic Era with its base at 2.58 Mya and including the Gelasian age, which was formerly considered part of the Neogene Period and Pliocene Epoch.[15] Thus the Neogene Period ends bounding the succeeding Quaternary Period at 2.58 Mya.

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