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Journal articles on the topic 'Vincent Gulf Region Eocene'

Author: Grafiati

Published: 4 June 2021

Last updated: 24 July 2025

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1

WAGNER, JENNIFER D., DANIEL J. PEPPE, JENNIFER M. K. O’KEEFE, and CHRISTOPHER N. DENISON. "PLANT COMMUNITY CHANGE ACROSS THE PALEOCENE–EOCENE BOUNDARY IN THE GULF COASTAL PLAIN, CENTRAL TEXAS." Palaios 38, no. 10 (2023): 436–51. http://dx.doi.org/10.2110/palo.2022.008.

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Abstract Long-term global warming during the early Paleogene was punctuated by several short-term ‘hyperthermal’ events, the most pronounced being the Paleocene–Eocene Thermal Maximum (PETM). During this long-term warming, tropical climates expanded into extra-tropical areas, creating a widespread band of thermophilic flora that reached into the paratropics, possibly as far north as mid-latitude North America in some regions. Relatively little is known about these paratropical floras, despite distribution across the North American Gulf Coastal Plain. We assess floras from the Gulf Coastal Plai

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Carreño, Ana Luisa, and Thomas M. Cronin. "Middle Eocene Ostracoda from Baja California Sur, Mexico." Journal of Micropalaeontology 12, no. 2 (1993): 141–53. http://dx.doi.org/10.1144/jm.12.2.141.

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Abstract. One genus and six new species of ostracodes are described from the Bateque Formation on the Pacific Coast of Baja California Sur, Mexico. Planktonic foraminifers indicate a mid Eocene age and the whole assemblage is characteristic of a shallow warm-water environment. Paijenborchella mezquitalensis sp. nov. is the second record of the genus Paijenborchella from the Eocene of North America. Except for this species and the new genus Bajacythere, the ostracode association has strong affinities with those described from the lower Tertiary Gulf Coast region.

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Uhen, Mark D., and David Taylor. "A basilosaurid archaeocete (Cetacea, Pelagiceti) from the Late Eocene of Oregon, USA." PeerJ 8 (October 2, 2020): e9809. http://dx.doi.org/10.7717/peerj.9809.

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Background Basilosaurid archaeocetes are known from the Late Eocene of virtually all coastlines bearing coeval marine rocks except the North Pacific Basin, until now. Here we report on three consecutive posterior thoracic vertebrae of a large, basilosaurid archaeocete from a Late Eocene horizon in the Keasey Formation in Oregon. Methods These vertebrae were morphologically and morphometrically compared to other vertebrae of similar age from around the world. Results The specimens were determined to be different from all currently named species of fossil cetacean, but most similar to those foun

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Sontag, Elżbieta, and Ryszard Szadziewski. "Biting midges (Diptera: Ceratopogonidae) in Eocene Baltic amber from the Rovno region (Ukraine)." Polish Journal of Entomology / Polskie Pismo Entomologiczne 80, no. 4 (2011): 779–800. http://dx.doi.org/10.2478/v10200-011-0058-4.

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Biting midges (Diptera: Ceratopogonidae) in Eocene Baltic amber from the Rovno region (Ukraine) The paper presents the results of an examination of 714 biting midges (Diptera: Ceratopogonidae) preserved in Baltic amber from the Rovno deposits in Ukraine. A new species - Leptoconops rovnensis sp. n. - is described and illustrated. 29 of the fossil species reported here have already been described from other deposits of Baltic amber: 26 of these were also found in amber from the Gulf of Gdańsk and 18 in amber from Bitterfeld (Saxony). The most common genera of biting midges in Ukrainian amber ar

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Jiang, Mark M. "Middle Eocene through basal Miocene sequence bio-stratigraphy of the western Gulf Coast region." Marine and Petroleum Geology 14, no. 7-8 (1997): 855–66. http://dx.doi.org/10.1016/s0264-8172(97)00049-4.

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6

Lin, Yani, Tianze Zhang, and Kelly H. Liu. "Turbidite lobe deposits in a canyon-fill system." Interpretation 9, no. 2 (2021): C17—C21. http://dx.doi.org/10.1190/int-2020-0111.1.

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Geological feature: Turbidite lobe deposits in a canyon-fill system Seismic appearance: Isolated and irregularly shaped sandstone pods Alternative interpretations: Mid-channel bars in a braided channel system Features with similar appearance: Alluvial fans Formation: Lower Wilcox Group Age: Late Paleocene to Early Eocene Location: Shelf edge at the Central Gulf Coast Region of Texas Seismic data: Donated by a petroleum exploration company in Houston, Texas Analysis tools: Seismic attributes such as instantaneous phase, root-mean-square amplitude, and spectral decomposition

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Scheibner, C., A. M. Marzouk, and J. Kuss. "Maastrichtian-Early Eocene litho-biostratigraphy and palægeography of the northern Gulf of Suez region, Egypt." Journal of African Earth Sciences 32, no. 2 (2001): 223–55. http://dx.doi.org/10.1016/s0899-5362(01)90005-3.

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8

Cotton, Laura J., Wolfgang Eder, and James Floyd. "Larger foraminifera of the Devil's Den and Blue Hole sinkholes, Florida." Journal of Micropalaeontology 37, no. 1 (2018): 347–56. http://dx.doi.org/10.5194/jm-37-347-2018.

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Abstract. Shallow-water carbonate deposits are well-known from the Eocene of the US Gulf Coast and Caribbean. These deposits frequently contain abundant larger benthic foraminifera (LBF). However, whilst integrated stratigraphic studies have helped to refine the timing of LBF overturning events within the Tethys and Indo-Pacific regions with respect to global bio- and chemo-stratigraphic records, little recent work has been carried out in the Americas. The American LBF assemblages are distinctly different from those of Europe and the Indo-Pacific. It is therefore essential that the American bi

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9

Tomo, Ikuko, and Catherine M. Kemper. "Strandings in St Vincent Gulf Bioregion, South Australia: 12-Year Study Monitors Biology and Pathology of Cetaceans." Oceans 3, no. 4 (2022): 439–63. http://dx.doi.org/10.3390/oceans3040030.

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The semi-enclosed environment of the St Vincent Gulf Bioregion and its fauna are impacted by many human activities. Long-term monitoring of cetaceans is vital. Records of collected specimens (173) and those not examined by the South Australian Museum (98 non-specimens) from 2009–2020 were analyzed. Necropsies were carried out on most carcasses using gross, histopathological, and diagnostic assessment of pathogens, organs, and skin lesions. The relative age and circumstance of death were assigned. Baleen whales (five species) and odontocetes (eight species) were studied. Indo-Pacific bottlenose

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Golubovskaya, E. V. "Specific features of the geochemistry of Eocene-Miocene rocks in the Perovskii Gulf, northern Aral region." Lithology and Mineral Resources 42, no. 3 (2007): 281–88. http://dx.doi.org/10.1134/s0024490207030078.

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11

Carter, Burchard D., and Michael L. McKinney. "Eocene echinoids, the Suwannee Strait, and biogeographic taphonomy." Paleobiology 18, no. 3 (1992): 299–325. http://dx.doi.org/10.1017/s0094837300010861.

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Faunal similarity among regions is often used as a means of identifying regions of endemism in fossil faunas. At least two large-scale taphonomic effects can affect apparent faunal similarity: stratigraphic and facies mismatching. In stratigraphic mismatching, an unconformity represents removal of most or all of a complete assemblage zone in one region, and the constituent taxa are mistakenly interpreted as having never inhabited that region. In facies mismatching, environmental differences between two regions (possibly unrecognized) cause the inference of a barrier that never existed. The two

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12

Tucker, Annette B., and Rodney M. Feldmann. "Fossil decapod crustaceans from the lower Tertiary of the Prince William Sound Region, Gulf of Alaska." Journal of Paleontology 64, no. 3 (1990): 409–27. http://dx.doi.org/10.1017/s0022336000018643.

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Sixty-five fossil brachyuran crabs, collected from rocks of the Orca Group, Tokun Formation, and Poul Creek Formation, have been assigned to six species, five of which were described previously. One of these, Pilumnoplax hannibalanus, is reassigned to Neopilumnoplax. Morphologic descriptions of Raninoides vaderensis, Eumorphocorystes naselensis, Portunites alaskensis, and Branchioplax washingtoniana are emended. Orbitoplax plafkeri n. gen. and sp. is described from the Poul Creek Formation on Wingham Island. The diagnosis of age for the Orca Group has been problematic. However, the well-preser

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Jackson, William T., Matthew P. McKay, Donald A. Beebe, et al. "Late Cretaceous sediment provenance in the eastern Gulf Coastal Plain (U.S.A.) based on detrital-zircon U-Pb ages and Th/U values." Journal of Sedimentary Research 91, no. 10 (2021): 1025–39. http://dx.doi.org/10.2110/jsr.2020.177.

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ABSTRACT Detrital-zircon U-Pb geochronology documents a regional- to continental-scale drainage reorganization along the eastern Gulf Coastal Plain (USA) from the Late Cretaceous (Cenomanian) to the Paleocene–Eocene. We present detrital-zircon U-Pb ages and Th/U values from the Maastrichtian Ripley Formation to determine the sedimentary provenance and to provide spatiotemporal resolution of drainage reorganization. The Ripley Formation contains a 12.7% overall average abundance of detrital zircons with low (&lt; 0.1) Th/U values relative to the underlying Cenomanian Tuscaloosa Group (3.6%)

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Carter, B. D., T. H. Beisel, W. B. Branch, and C. M. Mashburn. "Substrate preferences of Late Eocene (Priabonian/Jacksonian) echinoids of the eastern Gulf Coast." Journal of Paleontology 63, no. 4 (1989): 495–503. http://dx.doi.org/10.1017/s0022336000019715.

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Thin sections and acetate peels of the sediment within, and adhering to the outsides of, tests of Late Eocene echinoids from the southeastern United States have proven to be useful checks on inferences from test morphology concerning substrate preference. Previous characterizations of species' sediment preferences have concentrated primarily on the functional morphology of spatangoids, and relied particularly heavily upon Recent relatives of nonspatangoids. Reassessment of the preferences of spatangoids has led to a few discrepancies between interpretations herein and those of previous workers

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Van Vliet-Lanoë, Brigitte, Jean-Louis Mansy, Jean-Pierre Henriet, Michel Laurent, and Jean-Pierre Vidier. "A tectonic inversion by steps during the Cenozoic : the Dover Strait." Bulletin de la Société Géologique de France 175, no. 2 (2004): 175–95. http://dx.doi.org/10.2113/175.2.175.

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Abstract The Boulonnais is a dome incised by a former marine gulf inset into a zone of tectonic inversion from the Middle Eocene, which was already partly excavated at least at the Upper Eocene. New sedimentological and paleopedological data obtained within the Boulonnais, completed with old seismic profiles, allow a better understanding of the inversion process which developed step by step. The initial breaching probably took place in the late Eocene. The Dover Strait was probably opened during the Lutetian, a part of the Oligocene and the late Neogene. Oligocene and Pliocene faunal assemblag

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Jablonski, D., S. Pono, and O. A. Larsen. "PROSPECTIVITY OF THE DEEPWATER GULF OF PAPUA AND SURROUNDS IN PAPUA NEW GUINEA (PNG)—A NEW LOOK AT A FRONTIER REGION." APPEA Journal 46, no. 1 (2006): 179. http://dx.doi.org/10.1071/aj05011.

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Despite limited well control and paucity of seismic data, a regional study of the deepwater portion of the Gulf of Papua, Papua New Guinea (PNG), indicates a number of large structures at a variety of stratigraphic levels that are capable of holding significant volumes of hydrocarbons. The main structural elements east of the Fly River Platform the Pandora Ridge, Pandora Trough, Aure Trough, Port Moresby Trough and the northern portion of the Eastern Plateau were established during the Paleozoic and further enhanced by Late Cretaceous to Early Paleocene Coral Sea rifting in the southeast. Stru

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Smith, Kathlyn M., Alexander K. Hastings, Ryan M. Bebej, and Mark D. Uhen. "Biogeographic, stratigraphic, and environmental distribution of Basilosaurus (Mammalia, Cetacea) in North America with a review of the late Eocene shoreline in the southeastern coastal plain." Journal of Paleontology 96, no. 2 (2021): 439–51. http://dx.doi.org/10.1017/jpa.2021.90.

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AbstractA new specimen of Basilosaurus cetoides was discovered on the banks of the Flint River in Albany, Georgia, USA, in 2010. This fossil, which was the most complete specimen of the species from Georgia to date, consisted of five nearly complete and two partial post-thoracic vertebrae, tentatively identified as S4 through Ca6. During excavation, however, the site was looted and most of the specimen was lost to science. Nonetheless, we use this discovery as an opportunity to update the current state of knowledge on the stratigraphic, biogeographic, and environmental distribution of Basilosa

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Frieling, Joost, Emiel P. Huurdeman, Charlotte C. M. Rem, et al. "Identification of the Paleocene–Eocene boundary in coastal strata in the Otway Basin, Victoria, Australia." Journal of Micropalaeontology 37, no. 1 (2018): 317–39. http://dx.doi.org/10.5194/jm-37-317-2018.

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Abstract. Detailed, stratigraphically well-constrained environmental reconstructions are available for Paleocene and Eocene strata at a range of sites in the southwest Pacific Ocean (New Zealand and East Tasman Plateau; ETP) and Integrated Ocean Discovery Program (IODP) Site U1356 in the south of the Australo-Antarctic Gulf (AAG). These reconstructions have revealed a large discrepancy between temperature proxy data and climate models in this region, suggesting a crucial error in model, proxy data or both. To resolve the origin of this discrepancy, detailed reconstructions are needed from both

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Holford, Simon, Richard Hillis, Ian Duddy, et al. "Cenozoic post-breakup compressional deformation and exhumation of the southern Australian margin." APPEA Journal 51, no. 1 (2011): 613. http://dx.doi.org/10.1071/aj10044.

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We present results from a margin-wide analysis of the history of post-breakup Cenozoic compressional deformation and related exhumation along the passive southern margin of Australia, based on a regional synthesis of seismic, stratigraphic and thermochronological data. The Cenozoic sedimentary record of the southern margin contains regional unconformities of intra-Lutetian and late Miocene–Pliocene age, which coincide with reconfigurations of the boundaries of the Indo-Australian Plate. Seismic data show that post-breakup compressional deformation and sedimentary basin inversion—characterised

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20

Bryars, Simon R., and Mark Adams. "An allozyme study of the blue swimmer crab, Portunus pelagicus (Crustacea : Portunidae), in Australia: stock delineation in southern Australia and evidence for a cryptic species in northern waters." Marine and Freshwater Research 50, no. 1 (1999): 15. http://dx.doi.org/10.1071/mf98075.

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Allozyme analysis was used to examine the species-level systematics and stock structure of the Australian blue swimmer crab Portunus pelagicus. Fifty-seven crabs from eight sites were screened in an overview study for allozyme variation at 35 loci. This overview study revealed the presence of two species, differing at a Nei D of 0.14 (2% fixed differences), in the Darwin region of northern Australia. One of these species corresponds to the common P. pelagicus found throughout Australia, whereas the other is most likely either an undescribed ‘cryptic’ species, or the east-Asian species P. tritu

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Fan, Yan, Caifu Xiang, Songling Yang, et al. "Hydrocarbon Accumulation Characteristics of the Perdido Fold Belt, Burgos Basin, Gulf of Mexico—A Comparison Between the Central and Eastern Regions." Energies 18, no. 7 (2025): 1834. https://doi.org/10.3390/en18071834.

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Frequent salt tectonic activities within the Perdido fold belt complicate hydrocarbon accumulation, severely constraining hydrocarbon exploration. In this paper, the characteristics and differences of hydrocarbon accumulation in the Wilcox and Frio Formations in the central and eastern regions of the Perdido fold belt are analyzed through geochemical analysis, hydrocarbon generation simulation, and regional tectonic restoration. The results indicate the following: (1) Hydrocarbon in the Wilcox and Frio Formations in both the central and eastern regions of the Perdido fold belt originates from

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Bryars, Simon R. "Can regional nutrient status be used to predict plant biomass, canopy structure and epiphyte biomass in the temperate seagrass Amphibolis antarctica?" Marine and Freshwater Research 60, no. 10 (2009): 1054. http://dx.doi.org/10.1071/mf08194.

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The seagrass Amphibolis antarctica is an important component of coastal soft-sediment ecosystems across southern Australia. Large-scale losses of A. antarctica at several locations have been linked to anthropogenic nutrient inputs. The present study comprised a field survey to test whether the spatial patterns of plant biomass, canopy structure and epiphyte biomass in A. antarctica could be predicted based on expectations related to nutrient status across two regions within Gulf St Vincent, South Australia. Specific predictions were that: (1) plant biomass, plant density, plant height, leaf cl

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Cobiella-Reguera, Jorge L. "Emplacement of the northern ophiolites of Cuba and the Campanian-Eocene geological history of the northwestern Caribbean-SE Gulf of Mexico region." Geological Society, London, Special Publications 328, no. 1 (2009): 315–38. http://dx.doi.org/10.1144/sp328.13.

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Duque, Maria Rosa. "Using Heat Flow Density Values Obtained in the Gulf of Cadiz and Gorringe Bank, Atlantic Ocean." IOP Conference Series: Earth and Environmental Science 906, no. 1 (2021): 012113. http://dx.doi.org/10.1088/1755-1315/906/1/012113.

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Abstract The geothermal heat flow measured at the surface of the Earth is originated by different heat sources located at different depths of the planet. The main sources of heat flow in the crust are associated with radioactive decay of Uranium, Thorium and Potassium, in rocks. In some regions, additional heat sources must be considered such as exothermic chemical reactions. The value of the heat flow coming from deep regions, designated by “heat from the mantle”, must be obtained using indirect methods. In this work, the geoid height was used as indicator of alterations “in heat from the man

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Fowler, A. J., C. Huveneers, and M. T. Lloyd. "Insights into movement behaviour of snapper (Chrysophrys auratus, Sparidae) from a large acoustic array." Marine and Freshwater Research 68, no. 8 (2017): 1438. http://dx.doi.org/10.1071/mf16121.

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Snapper is a significant fishery species in Australasia whose movement behaviour remains poorly understood. This was addressed in the present study at the within-region scale using acoustic telemetry in the Gulf St Vincent, South Australia. Over 3 years from May 2011, 54 snapper were monitored throughout ~160km2 using 41 acoustic receivers. The dispersion of >500000 detections varied in space and time, reflecting three types of space use, dependent on different types of movement behaviour. One station, near a large shipwreck, accounted for 67.8% of all detections, particularly during winter

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Jost, Anne, Sophie Violette, Jean-Claude Macquar, and Gilles Dromart. "Fluid palaeo-circulation generated by the Pyrenean orogeny and its potential role in the formation of lead-zinc deposits in the Cévennes region: a modelling approach." Bulletin de la Société Géologique de France 175, no. 4 (2004): 317–29. http://dx.doi.org/10.2113/175.4.317.

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Abstract Recent studies of the host rock palaeomagnetism of the lead-zinc deposits on the Cévennes margins pointed towards regional fluid circulation from the early to middle Eocene. The hypothesis has therefore been put forward that mineralising fluids might have migrated as a consequence of the Pyrenean uplift. Based on this assumption, a digital model was developed to describe this palaeo-circulation along two reconstituted cross-sections, in early Eocene times. One of them extends from the Gulf of Lion to the Les Malines deposits at the southern end of the Cévennes mountains; the other o

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Fournier, Marc, Claude Lepvrier, Philippe Razin, and Laurent Jolivet. "Late Cretaceous to Paleogene post-obduction extension and subsequent Neogene compression in the Oman Mountains." GeoArabia 11, no. 4 (2006): 17–40. http://dx.doi.org/10.2113/geoarabia110417.

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ABSTRACT After the obduction of the Semail ophiolitic nappe onto the Arabian Platform in the Late Cretaceous, north Oman underwent several phases of extension before being affected by compression in the framework of the Arabia-Eurasia convergence. A tectonic survey, based on structural analysis of fault-slip data in the post-nappe units of the Oman Mountains, allowed us to identify major events of the Late Cretaceous and Cenozoic tectonic history of northern Oman. An early ENE-WSW extensional phase is indicated by synsedimentary normal faults in the Upper Cretaceous to lower Eocene formations.

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Al-Fahmi, Mohammed, L. Cooke Michele, and John C. Cole. "Modeling of the Dammam outcrop fractures: Case study for fracture development in salt-cored structures." GeoArabia 19, no. 1 (2014): 49–80. http://dx.doi.org/10.2113/geoarabia190149.

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ABSTRACT The exposed Cenozoic carbonates of the Dammam Dome are studied to: (1) characterize fractures and associated structures; (2) interpret the fracture mechanism; and (3) gain insights into fracture development within dome-like structures in the subsurface of the Arabian Gulf region. The fieldwork is integrated with structural analysis of the near-surface horizons mapped from interpretations of 3-D reflection seismic and borehole logs. Fractures are mapped from the outcrops of the middle limestone unit of the Eocene Rus Formation. The outcrops are concentrated in the central, northern and

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Van Vliet-Lanoë, Brigitte, Guillaume Gosselin, Jean-Louis Mansy, et al. "Une révision de l’histoire cénozoïque du Pas-de-Calais." Annales de la Société Géologique du Nord, no. 17 (December 1, 2010): 59–80. http://dx.doi.org/10.54563/asgn/1782.

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The Strait of Dover is possibly an element of the European rift, subsiding from the Paleoene to the Quaternary but mostly during the Oligocene extension phase resulting from the opening of the Northern Atlantic. But as it is superimposed on a zone in tectonic inversion, the tension could be limited in expression by the reactivation of the Variscan front. The inversion of the Variscan front accommodates most of the shortening induced by the Pyrenean Orogeny and the opening of the Northern Atlantic to the Western border of the European plate. The Boulonnais depression constitutes a marine gulf f

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Van Vliet-Lanoë, Brigitte, Guillaume Gosselin, Jean-Louis Mansy, et al. "Une révision de l’histoire cénozoïque du Pas-de-Calais." Annales de la Société Géologique du Nord, no. 17 (December 1, 2010): 59–80. http://dx.doi.org/10.54563/asgn.1782.

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The Strait of Dover is possibly an element of the European rift, subsiding from the Paleoene to the Quaternary but mostly during the Oligocene extension phase resulting from the opening of the Northern Atlantic. But as it is superimposed on a zone in tectonic inversion, the tension could be limited in expression by the reactivation of the Variscan front. The inversion of the Variscan front accommodates most of the shortening induced by the Pyrenean Orogeny and the opening of the Northern Atlantic to the Western border of the European plate. The Boulonnais depression constitutes a marine gulf f

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Corbett, Evan, Sami W. Rifai, Graziela Miot da Silva, and Patrick A. Hesp. "Temporal and Spatial Distribution of 2022–2023 River Murray Major Flood Sediment Plume." Remote Sensing 17, no. 10 (2025): 1711. https://doi.org/10.3390/rs17101711.

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This study examined a sediment plume from Australia’s largest river, The River Murray, which was produced during a major flood event in 2022–2023. This flood resulted from successive La Niña events, causing high rainfall across the Murray–Darling Basin and ultimately leading to a significant riverine flow through South Australia. The flood was characterised by a significant increase in riverine discharge rates, reaching a peak of 1305 m³/s through the Lower Lakes barrage system from November 2022 to February 2023. The water quality anomaly within the coastal region (<~150 km offshore) was e

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Wilson, Brent, and Michael A. Kaminski. "Rare species of West Indian aspect in the Holocene of Liverpool Bay and their biogeographic and environmental significance." Micropaleontology 69, no. 1 (2023): 103–12. http://dx.doi.org/10.47894/mpal.69.1.03.

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The Gulf Stream, although not directly responsible for the mild, temperate climate of the British Isles, transports vast quantities of water across the North Atlantic Ocean. An extension of the Caribbean-Loop-Florida current system, this strong current cools and becomes more saline by evaporation as it flows NE across the North Atlantic Ocean. Nevertheless, it is able to transport benthic foraminifera across oceanic distances, the fauna around Bermuda containing many species described from the Caribbean Sea. Examining two cores taken from the shallow middle neritic Holocene Surface Sands Forma

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Martínez-Hernández, Enrique, and Elia Ramírez-Arriaga. "Palaeocorología de angiospermas de la flora mexicana durante el Mesozoico y Terciario. Algunas evidencias palinológicas." Botanical Sciences, no. 58 (April 27, 2017): 87. http://dx.doi.org/10.17129/botsci.1490.

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The historical phytogeography is closely related to climatic changes and with the modifications of Ecosystems through time caused by th e p la te tecto nics. This pa lin ostratig rap hic review is the result of the surveys carried out in several sedimentary basin from Baja California to Chiapas, Mexico. The paleochorology of angiosperms in Mexican terrains began in the Lower Cretaceous (Barremian-Aptian) in the northern state of Durango, where at the "Gran Tesoro" appeared jugella sensu Srivastava ( 1994) and Tricolpites cf. T. minutus Brenner, 1963. In the same age, in Michoacán state, southe

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Kotthoff, U., D. R. Greenwood, F. M. G. McCarthy, K. Müller-Navarra, S. Prader, and S. P. Hesselbo. "Late Eocene to middle Miocene (33 to 13 million years ago) vegetation and climate development on the North American Atlantic Coastal Plain (IODP Expedition 313, Site M0027)." Climate of the Past 10, no. 4 (2014): 1523–39. http://dx.doi.org/10.5194/cp-10-1523-2014.

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Abstract. We investigated the palynology of sediment cores from Site M0027 of IODP (Integrated Ocean Drilling Program) Expedition 313 on the New Jersey shallow shelf to examine vegetation and climate dynamics on the east coast of North America between 33 and 13 million years ago and to assess the impact of over-regional climate events on the region. Palynological results are complemented with pollen-based quantitative climate reconstructions. Our results indicate that the hinterland vegetation of the New Jersey shelf was characterized by oak–hickory forests in the lowlands and conifer-dominate

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Jolivet, Laurent, Armel Menant, Vincent Roche, et al. "Transfer zones in Mediterranean back-arc regions and tear faults." BSGF - Earth Sciences Bulletin 192 (2021): 11. http://dx.doi.org/10.1051/bsgf/2021006.

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Slab tearing induces localized deformations in the overriding plates of subduction zones and transfer zones accommodating differential retreat in back-arc regions. Because the space available for retreating slabs is limited in the Mediterranean realm, slab tearing during retreat has been a major ingredient of the evolution of this region since the end of the Eocene. The association of detailed seismic tomographic models and extensive field observations makes the Mediterranean an ideal natural laboratory to study these transfer zones. We review in this paper the various structures in back-arc r

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Mousavi, Naeim, and Javier Fullea. "3-D thermochemical structure of lithospheric mantle beneath the Iranian plateau and surrounding areas from geophysical–petrological modelling." Geophysical Journal International 222, no. 2 (2020): 1295–315. http://dx.doi.org/10.1093/gji/ggaa262.

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SUMMARY While the crustal structure across the Iranian plateau is fairly well constrained from controlled source and passive seismic data, the lithospheric mantle structure remains relatively poorly known, in particular in terms of lithology. Geodynamics rely on a robust image of the present-day thermochemical structure interpretations of the area. In this study, the 3-D crustal and upper mantle structure of the Iranian plateau is investigated, for the first time, through integrated geophysical–petrological modelling combining elevation, gravity and gravity gradient fields, seismic and petrolo

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Lokho, Kapesa, JosÉ Francisco Carrasco, Shantajhara Biswal, Kezhakielie Whiso, and Ansuya Bhandari. "First report of Eocene echinoids from the Sylhet Limestone, Mikir Hills of Assam, India: palaeontological, palaeogeography and palaeoenvironmental significance." Journal of the Palaeontological Society of India, November 5, 2023. http://dx.doi.org/10.1177/05529360231205313.

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This article reports two echinoid taxa viz. Ilarionia sindensis Duncan and Sladen (1884) and Porocidaris schmidelii Münster in Goldfus (1830) from the middle Eocene Sylhet Limestone of Mikir Hills, Assam. P. schmidelii is found from the Lutetian (middle Eocene) to the Priabonian (upper Eocene) in the following regions: NE of Spain, Biarritz (Southwestern France), Angoumé (Southern Aquitaine, France), Carinthia (Southern Austria), Venetian region of Italy Provence, Southern Alps of French, Istria (Croatia), Persian Gulf, Oman and Egypt. I. sindensis was first reported from the Eocene of Sindh p

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Mark M. Jiang. "Middle Eocene Through Basal Miocene Sequence Biostratigraphy of the Western Gulf Coastal Region: ABSTRACT." AAPG Bulletin 78 (1994). http://dx.doi.org/10.1306/a25feecd-171b-11d7-8645000102c1865d.

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Craddock, William H., James L. Coleman, and Andrew R. C. Kylander‐Clark. "Detrital zircon age spectra of middle and upper Eocene outcrop belts, U.S. Gulf Coast region." Basin Research, June 30, 2020. http://dx.doi.org/10.1111/bre.12464.

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KASIŃSKI, Jacek Robert, Regina KRAMARSKA, Barbara SŁODKOWSKA, Vadim SIVKOV, and Marcin PIWOCKI. "Paleocene and Eocene deposits on the eastern margin of the Gulf of Gdańsk (Yantarny P-1 borehole, Kaliningrad region, Russia)." Geological Quarterly 64, no. 1 (2020). http://dx.doi.org/10.7306/gq.1513.

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Landau, Bernard M., Carlos Marques da Silva, and Mathias Harzhauser. "The genus Euthria (Gastropoda, Tudiclidae) in the Pliocene of the Atlantic Mondego Basin of Portugal: a glocal taxon in the Atlanto-Mediterranean Neogene." Journal of Paleontology, April 28, 2025, 1–13. https://doi.org/10.1017/jpa.2024.83.

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Abstract Today, the range of the genus Euthria encompasses the Mediterranean and the eastern Atlantic, the region around southern Africa, and extends into the western Indo-Pacific. The genus, which has a geological history dating back to the Eocene of Europe, has recently undergone taxonomic revision in several European Neogene basins. These studies revealed a pronounced expansion during the Oligocene and Neogene in the Atlanto-Mediterranean region and the Paratethys, and these studies highlighted the overall diversity of the genus combined with a pronounced regional endemism. This paper revie

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