bluuebunny/crossref_metadata_2025_split huggingface dataset:
Good News and Bad News in Two Highly Industrialized Puget Sound, Washington (u.s.a.) Embayments
Authors: Martin Ruth A. , Nesbitt Elizabeth A. 
Published: August 2019

AbstractIn this study, an offshoot of studies undertaken by the Washington State Department of Ecology (WDOE), the density and diversity of foraminiferal assemblages in Commencement and Elliott bays, two heavily industrialized embayments in Puget Sound, Washington (U.S.A) were compared and correlated with concentrations of metal pollutants and total polycyclic aromatic hydrocarbons (PAH). Samples used in this study were collected by the WDOE between 1998 and 2014, allowing comparison over a temporal range encompassing the beginnings of environmental remediation in both bays. The composition of the foraminiferal assemblages is typical of polluted estuaries globally, with the major taxa being Elphidiella hannai, Cribroelphidium excavatum, Bucella frigida and Eggerella advena. Foraminiferal density and diversity showed negative correlations with pollutants, however, these correlations were significant for only a few pollutants, and trends could not be attributed to any single one. Both embayments showed increasing diversity over time, and both had high proportions of calcareous tests that displayed signs of dissolution, indicating corrosive conditions in the water. In Elliott Bay the percentage of partially dissolved tests increased over time, suggesting remediation efforts have not been successful in all areas.
On the Taxonomic Identity of the Planktonic Foraminiferal Species Globorotalia Barisanensis Le Roy, 1939
Authors: Zachariasse Willem Jan , Berggren William A. , Si Weimin , Huber Brian T. 
Published: August 2019

Abstract
Examination of the holotype of Globorotalia barisanensis Le Roy, 1939, has revealed that this species from the Middle Miocene of central Sumatra is non-keeled, contradicting the synonymizing of G. barisanensis with Globorotalia fohsi. Because the type sample is untraceable, we examined the available type specimens (holotype and eight paratypes), notes and data presented by previous researchers, and material from the near-topotype locality of Paragloborotalia siakensis, to clarify Le Roy's concept of G. barisanensis. Our investigation has revealed that the Middle Miocene of central Sumatra contains two different groups of globorotaliids: the Globorotalia menardii group and the G. fohsi group, and that G. barisanensis belongs to the latter.
The paratypes examined belong to Globorotalia peripheroacuta and to forms transitional between G. peripheroacuta and Globorotalia praefohsi. The holotype, as described by Le Roy, is included in G. peripheroacuta as well, despite the observation that it differs from the paratypes in the abnormally inflated final chamber. In retrospect, the specimen selected as the holotype was an unfortunate choice as it has long been misinterpreted and used to denominate the earliest representatives of the G. fohsi group (viz. G. fohsi barisanensis) until G. barisanensis was reinterpreted as a junior synonym of G. fohsi based on a flawed redrawing of a fully keeled holotype of G. barisanensis. We conclude that Le Roy's concept of G. barisanensis was broad and may have included G. fohsi and Globorotalia peripheroronda as well. Remarkably, after 67 years of misinterpretation since Bolli (1950), G. barisanensis appears to be a valid name and a senior synonym of G. peripheroacuta. However, we recommend that it will be more practical to conserve the latter name, which is well established in the literature.
Photochemical Efficiencies of Diatom Symbionts in Hospite in Amphistegina Gibbosa (foraminifera) Across Seasons in the Florida Keys, Usa
Authors: Méndez-Ferrer Natasha , Hallock Pamela , Jones David L. 
Published: August 2019

Abstract
Benthic foraminiferal taxa that host algal endosymbionts can serve as model organisms in understanding photo-oxidative stress in environments where algal symbioses are prevalent. This study examined photochemical performance of the diatom symbionts within the foraminifer Amphistegina gibbosa. Data on bleaching prevalence and photochemical efficiency for photosystem II (PSII) were obtained from specimens collected at Tennessee Reef, Florida reef tract, USA, as close as logistically feasible to each equinox and solstice in 2012 and 2013. Specimens were collected at 6 m and 18 m depths, isolated, visually characterized, and assessed for maximum quantum yield of PSII using a pulse-amplitude modulated (PAM) fluorometer. Rapid-light curves (RLCs) were performed in the laboratory on specimens within a few hours of collection. Trials examined the effects of depth, sampling date, and degree of host bleaching. Consistent with field studies in the 1990s, proportions of A. gibbosa populations exhibiting visible loss of symbionts (i.e., “bleaching”) were lowest in December, with between-season and between-year differences in maxima. Maximum quantum yields ranged from 0.66–0.76. Significant differences between sampling dates were found at the 6 m site, with highest yields in winter and lowest in summer. At the 18 m site, maximum quantum yields differed both by sampling date and by degree of bleaching. Rapid light curves revealed that relative electron transport rates were highest in specimens exhibiting no visible symbiont loss; derived-photosynthetic parameters of α (initial slope of the RLC) and Ek (minimum saturating irradiance) did not differ significantly across different degrees of symbiont loss. Overall results indicate that even individuals exhibiting substantial symbiont loss retain some fully functional symbionts.
Cyrea Szymborska Gen. Et Sp. Nov., a New Textulariid Foraminifer from the Mediterranean Sea
Authors: Holzmann Maria , Rigaud Sylvain , Amini Shahrouz , Voltski Ivan , Pawlowski Jan 
Published: August 2019

Abstract
Textulariid foraminifera are characterized by a multichambered test with an agglutinated wall structure. Recent molecular work has shown that the order Textulariida appears as a paraphyletic group within the class Globothalamea. While larger members of the textulariids are fairly well known, smaller forms like the ones described here are often overlooked or synonymized with known species. A new species and genus was isolated from algal samples collected on the French coast of the Mediterranean Sea. Cyrea szymborska gen. and sp. nov., has a trochospiral chamber arrangement, measuring 100–210 µm in diameter. The organic wall is brownish, opaque, and sparsely agglutinated with diatom frustules and mineral grains, mostly 20 µm or smaller in size. The proloculus is not agglutinated. The extra-umbilical aperture forms a low arch. It is smooth, not agglutinated, and located on the last chamber. The biochemistry of the organic wall was investigated using Raman spectroscopy, showing that it is made of a meshwork of proteoglycans. A combined analysis of SSU and LSU rDNA sequences confirms the position of Cyrea among textulariids, distantly from all other genera. Molecular analyses revealed two phylotypes belonging to the new genus, one of which is formally described here.
Late Quaternary Paleoenvironmental Reconstruction, Using Benthic Foraminifera and Ostracoda, of Marine Sedimentary Beds On the Southern Coast of Laizhou Bay, Bohai Sea, China
Authors: Cui Xiaohui , Li Shoujun , Xu Hua , Zhang Zhuo , Zhao Xiuli , Gao Zongjun , Wei Ning , Zhang Xiangyu 
Published: August 2019

Abstract
Extensive studies of Quaternary transgressions have been conducted in Bohai Sea, but debates continue regarding the sedimentary evolution and timing of transgressions, especially in the Pleistocene section. Benthic foraminifers and ostracodes from three boreholes (GK138, GK111, GK95) at Laizhou Bay, Bohai Sea, were utilized to interpret the paleoenvironments of deposition and elucidate the coastal response to global sea-level changes since the late Quaternary. Benthic foraminiferal species identified included 32 species from 15 genera; ostracodes included 28 species from 16 genera. Three marine sedimentary beds were recognized based on sedimentary characteristics, down-core changes in environmental proxies (benthic foraminifers and ostracodes), accelerator mass spectrometry (AMS) 14C, and optically stimulated luminescence (OSL) dates. These three beds were interpreted as: marine sedimentary bed 3 (M3), deposited in the late-middle Pleistocene; marine sedimentary bed 2 (M2), deposited during the late Pleistocene; and marine sedimentary bed 1 (M1), deposited during the Holocene. Three microfossil assemblages were identified, all indicating nearshore conditions. Assemblage III indicated a fluvially influenced or paralic environment during a relatively small-scale late-middle Pleistocene transgression that produced bed M3. Assemblage II indicates an intertidal-subtidal environment where bed M2 was deposited during the late Pleistocene transgression. Assemblage I indicates somewhat more marine influence in a subtidal environment where bed M1 was deposited during the Holocene marine transgression.
Molecular Studies On Foraminifers: Past, Present, and Future
Authors: Bhatt Karan A. , Trivedi Mrugesh H. 
Published: August 2019

AbstractApplications of molecular techniques have become integral to most fields of biological research, including evolutionary biology. Over the past two decades, studies of molecular genetics of foraminifers have emerged to enhance taxonomic identification with broad applications, including biodiversity, environmental assessments, and paleoceanographic studies. However, the results are widely scattered across the literature, thereby inhibiting advances in such research on foraminifers, especially regionally. In this review, we discuss the developments and contributions in the field of molecular genetics as applied to foraminifers, offering a guide to beginners in this area of research. Furthermore, this review highlights new opportunities for foraminiferal research that will pave the way for future studies in this field.
Upper Hauterivian-upper Barremian Planktonic Foraminiferal Assemblages from the Arroyo Gilico Section (southern Spain)
Authors: Silva Isabella Premoli , Soldan Dario Marcello , Petrizzo Maria Rose 
Published: August 2019

AbstractLate Hauterivian−earliest late Barremian planktonic foraminifera from the Arroyo Gilico section (Subbetic domain, Betic Cordillera) have been investigated to correlate their distribution to ammonite zonation and calcareous nannofossil bioevents. The 72-m-thick section spans the interval between the upper Hauterivian ammonite Crioceratites binelli Subzone, Crioceratites baleraris Zone and the lowermost upper Barremian ammonite Barrancyloceras barremense Subzone, Toxancyloceras vandenheckii Zone. Planktonic foraminiferal assemblages are rich and relatively diverse. At the base of the section in the C. binelli Subzone, as already known, Hedbergella sigali, H. infracretacea, H. daminiae, and Lilliputianella semielongata are recorded. New findings include common Hedbergella praetrocoidea and H. aptiana along with rare specimens resembling H. excelsa based on their long and elevated spire. Early appearances of taxa continue up-section with the lowest occurrences (LOs) of H. ventriosa, then Lilliputianella eocretacea in the overlying Crioceratites krenkeli Subzone, followed by H. gorbachikae, while the LO of the ‘clavate’ Lilliputianella pauliani occurs just before the end of the Hauterivian within the topmost Pseudothurmannia picteti Subzone. The lower Barremian is punctuated by a number of successive appearances, including the typical Globigerinelloides blowi recorded in the upper lower Barremian Kotetishvilia compressissima Zone. The acme of the ‘clavate’ morphotypes occurs in the Moutoniceras moutonianum Zone across the Mid-Barremian Event (MBE); besides common L. semielongata, the taxa consistently present are L. pauliani with both typical and transitional morphologies, L. eocretacea, and to a minor extent “Globigerinelloides” sigali.
Neogene Benthic Foraminiferal Biofacies, Paleobathymetry, and Paleoenvironments of a Gulf of Mexico Transect
Authors: Katz Miriam E. , Miller Kenneth G. , Kaminski Michael A. , Browning James V. 
Published: August 2019

AbstractWe document Neogene benthic foraminiferal biofacies changes on a depth transect of six Gulf of Mexico industry wells (sidewall and cutting samples) that is oblique to the coast and extends from Main Pass to Green Canyon (offshore Alabama to Louisiana, USA). Calcareous nannofossil and planktonic foraminiferal biostratigraphic control provides the framework to make interwell comparisons of the benthic foraminiferal biofacies; these comparisons provide the basis for paleobathymetric and paleoenvironmental interpretations and to identify useful benthic foraminiferal biostratigraphic markers in this region.Benthic foraminiferal faunas indicate that Neogene paleodepths were slightly shallower at the eastern wells and deepened towards the western wells. Calcareous benthic foraminiferal biofacies dominated by Uvigerina spp. indicate that paleoenvironments characterized by low-oxygen conditions and/or high productivity occurred periodically during deposition along the transect. This is supported by repeated occurrences of a distinctive assemblage of agglutinated foraminifera (known as the “Agua Salada Fauna”) that is typical of dysaerobic environments.Evidence of intensified low-oxygen/high-productivity environments are recorded in lowermost Middle Miocene sediments at some locations and are present at all wells in Upper Miocene deposits. In Upper Miocene-Pliocene sediments, oxygen levels appear to have been related to paleodepth, indicating that the development of lower oxygen conditions was the result of an expansion or migration of the oxygen minimum zone. Our results are consistent with a global cause for the expansion of the oxygen minumum zone during the Late Miocene and widespread increase in export production. Our study shows that despite problems in well cuttings (cavings, inconsistent sampling) and complications in regional salt and fault tectonics, well transects can provide coherent benthic foraminiferal biofacies patterns that reveal paleobathymetric and paleoenvironmental changes in the Gulf of Mexico.
Distribution of Encrusting Foraminifera At San Salvador, Bahamas: a Comparison By Reef Types and Onshore−offshore Zonation
Authors: Tichenor Hal Ray , Lewis Ronald D. 
Published: August 2019

AbstractForaminifera attached permanently to hard substrates have received relatively little research attention in distributional studies compared to free-living specimens. Because attached (encrusting) species are commonly found on hard substrata, such as coral rubble, and they are sensitive to environmental variables controlled by water depth and distance from shore, these species can be useful in paleoecologic research. This study examined the distribution of encrusting foraminifera found at the outer Bahamian island of San Salvador to describe onshore-to-offshore zonation and to characterize foraminiferal assemblages found in different reef types. Cobbles were collected along two transects on the leeward side of the island and at numerous locations on the windward side, including a bank barrier reef and the eastern platform edge. Encrusting foraminifera found on the undersides of cobbles were quantified and identified by taxa, morphotype, and taphonomic grade. Significant differences were found in the distribution of encrusting foraminiferal species across the carbonate platform, based on both counts of individuals and area of substrate covered. The zonation was particularly evident between platform-top and platform-margin assemblages. Nearshore assemblages were dominated by well-preserved Homotrema rubrum. Patch reefs, especially those found further from shore, were characterized by a relatively diverse assemblage with prominent Planorbulina spp. whereas bank barrier reefs were dominated by H. rubrum, often with Gypsina plana. Platform-margin assemblages were the most distinct because they were dominated by large, sheet-like G. plana, with other taxa being small, sparse, and poorly preserved.
Interactions of Globobulimina Auriculata with Nematodes: Predator Or Prey?
Authors: Glock Nicolaas , Wukovits Julia , Roy Alexandra-Sophie 
Published: August 2019

Abstract
Studies of carnivorous behaviour of benthic foraminifers are rare and mostly focused on laboratory experiments. Controlled experiments have shown that some agglutinated and intertidal species prey on meio- to macrofaunal metazoans. Here we present observations of the behaviour of specimens of the infaunal benthic foraminiferal species, Globobulimina auriculata and G. turgida, made within several hours of collection from ∼117 m depth in the Alsbäck Deep of the Gullmar Fjord, Sweden. We observed live nematodes within the tests of G. auriculata. Video observations recorded over a 17-hour period showed a G. auriculata specimen with a living nematode whose tail appeared to be entangled within the foraminifer's reticulopodial network. The nematode eventually coiled around the foraminifer's aperture and became much less active, though ingestion into the foraminifer's test was not documented. If these observations indicate feeding by G. auriculata, they differ from previous observations of predation by Ammonia tepida, which utilised external reticulopodial activity to extract the soft tissue of its prey. An alternative interpretation of the video observations, consistent with the observations of the live nematodes inside G. auriculata, was that the nematode was attempting to prey upon the foraminifer.
The G. turgida specimens, in contrast, relatively quickly surrounded themselves in soft sediment spheres commonly seen in deposit-feeding foraminifers, and were never observed with nematodes within their tests. We speculate that these contrasting feeding strategies might reduce competition and facilitate the coexistence of these two globobuliminid species.
Moscovian–asselian (middle Pennsylvanian–earliest Cisuralian) Smaller Foraminifers from the Asad-abad Section (sanandaj-sirjan Zone, Central Iran)
Authors: Yarahmadzahi Hamed , Vachard Daniel 
Published: August 2019

AbstractCarboniferous and Permian strata crop out in Central Iran. The Asad-Abad section has yielded Gzhelian and Asselian fusulinid levels. Here we describe the smaller foraminifers of this section for the first time and introduce four biozones based on these taxa. Biozone I with Monotaxinoides? melanogaster n. sp. is interpreted to be early?-middle? Gzhelian in age (with possible reworkings affecting up to Moscovian/Kasimovian? levels) based upon the principle of superposition and of previous datings of the underlying series, but in the absence of direct datings by fusulinids of this lowermost part of the section. Further, Monotaxinoides? are generally known in the Bashkirian-Moscovian. Biozone II includes Raphconilia spp., Protonodosaria spp., and Rectogordius? minimus n. sp. and is interpreted as middle?-late Gzhelian in age. Biozone III includes Turrispiroides spp., Calcivertella anguinea, Calcitornella heathi, and Vervilleina crescenticamerata n. sp., and we base its early Asselian age on associated fusulinids. Finally, Biozone IV includes Cribrogenerina? sp. and Nodosinelloides longissima; its middle to late Asselian age, based on fusulinids, is confirmed by associated smaller foraminifers. The foraminiferal assemblages display marked differences in composition and stratigraphic distribution compared with those of Alborz and Tabas Block. Principally, they have unexpected similarities with several North American assemblages, especially the three new species: Monotaxinoides? melanogaster n. sp., Rectogordius? minimus n. sp., and Vervilleina crescenticamerata n. sp.
Definition of Foraminiferal Zones in the Famennian Stage (upper Devonian) of Tajikistan
Authors: Sabirov Abudvakhid 
Published: August 2019

AbstractSeven foraminiferal zones [Parathurammina dagmarae–Saltovskajina scitula–Neoarchaesphaera, Septaglomospiranella primaeva, Quasiendothyra (Eoquasiendothyra) bella, Q. (Eoendothyra) communis, Q. (E.) regularis, Q. (Q.) kobeitusana–Endoglomospiranella imminuta, and Q. (Q.) konensis–End. Nigra] have been identified from Famennian Stage carbonate sections in Tajikistan and compared to foraminiferal sequences from the Franco-Belgian Basin, the Russian part of the Eastern European Platform, the Ural Mountains (Russia), and Kyrgyzstan. The lower Famennian boundary is marked by the rapid extinction of all Frasnian Stage multicameral forms, which are replaced by a complex of single-chambered foraminifers of the P. dagmarae–S. scitula–Neoarchaesphaera Zone. This boundary practically coincides with the base of the middle Palmatolepis triangularis conodont zone. The upper Famennian boundary is recognized by the sharp change from endothyroid foraminifers of the Quasiendothyra konensis–Endoglomospiranella nigra Zone to a complex of simple mono- and bilocular forms of the Carboniferous Bisphaera malevkensis–Earlandia minima Zone. This boundary in the most intensely studied section at Shishkat is located 16 cm below the boundary of the Siphonodella praesulcata and S. sulcata conodont zones.
Late Serpukhovian Foraminifers Near the Mississippian-pennsylvanian Boundary At South Syncline Ridge, Southern Nevada, Usa: Implications For Correlation
Authors: Brenckle Paul L. , Manger Walter L. , Titus Alan L. , Nemyrovska Tamara I. 
Published: August 2019

AbstractA few, thin, Mississippian siliciclastic limestone beds, interbedded with ammonoid (uppermost Eumorphoceras Zone)-bearing shales within the South Syncline Ridge section on the Nuclear Test Site in southern Nevada, contain an abundant, low-diversity assemblage of late Serpukhovian/late Chesterian calcareous foraminifers dominated by the archaediscaceans Neoarchaediscus altiluminis, Brenckleina rugosa, Eosigmoilina robertsoni, and Betpakodiscus of the group B. attenuatus. These limestone beds were deposited in a shallow-water, clastic facies of the Scotty Wash Formation and, based on common conodont occurrences, correlate southeast to the Bird Spring Formation below the Mississippian-Pennsylvanian GSSP at Arrow Canyon, Nevada. The South Syncline Ridge foraminifers are comparable to those found in coeval beds at Arrow Canyon and represent the only other known foraminiferal assemblage to exist in association with uppermost Eumorphoceras Zone ammonoids in North America outside of Arkansas in the southern Midcontinent. Reconciliation of regional conodont and ammonoid zonations shows that the range of eosigmoiline foraminifers (E. robertsoni and B. rugosa), now generally considered an upper Serpukhovian index, extends from a position either just below or at the lower-upper boundary of the Serpukhovian Stage into the lower part of the Bashkirian Stage in North America; their upper range falls within the lower part of the Homoceras ammonoid zone beginning in the upper part of the Serpukhovian Stage. Discussion of the foraminiferal taxa includes support for retaining the genus Betpakodiscus rather than synonymizing it under Tubispirodiscus, as proposed by some specialists during the past few years.