bluuebunny/crossref_metadata_2025_split huggingface dataset:
STRATIGRAFIA E SEDIMENTOLOGIA DEI "CALCARI E MARNE A <em>RHAETAVICULA CONTORTA</em> AUCTT. (NORICO-RETICO) DELLA TOSCANA NORD-OCCIDENTALE - NUOVA SUDDIVISIONE FORMAZIONALE
Authors: FAZZUOLI MILVIO , FOIS ELISABETTA , TURI ALESSANDRO 
Published: November 2023

Nine sections from the "Limestones and marls with Rhaetavicula contorta" Auctt. (Norian-Rhaetian) of the Tuscan Nappe in eastern Liguria and northwestern Tuscany, have been examined for their stratigraphic and sedimentological characteristics. The results obtained have been integrated with data pertaining to the previously studied Pania di Corfino section.
Two formations were identified and studied in detail: that of Pania di Corfino and that of La Spezia.
Where present, the Pania di Corfino Formation accounts for the lower portion of the sections. It consists mainly of thick beds and massive layers of dolomites, dolomitic limestones and limestones. Thinly-bedded dark limestones appear less frequently, while layers rich in clay are rare. The top of the formation is surely of Rhaetian age, in some sections, as indicated by the presence of Triasina hantkeni Majzon; in the others, it is Norian-Rhaetian. The age of the bottom portion can be regarded as Norian-Rhaetian in all the sections; the presence of considerably thick deposits beneath the established Rhaetian layers in some sections, however, suggests an Early Rhaetian or even Late Norian age.
The depositional environment of the Pania di Corfino Formation may be envisaged as an epicontinental carbonate platform with predominantly restricted water circulation on which fine carbonate sediments are deposited beneath the wave base; features suggesting a tidal flat are rare. The environment of deposition was, for brief periods only, that of a platform with open circulation in which the effects of wave-motion were prominent; features strictly relatable to a true platform edge have not been found.
UNA SEQUENZA PALINOLOGICA DI ETA' RUSCINIANA NEI SEDIMENTI LACUSTRI BASALI DEL BACINO DI AULLA-OLIVOLA (VAL DI MAGRA)
Authors: BERTOLDI REMO 
Published: November 2023

Palynological investigations were carried out on the basal sediments of the Aulla-Olivola basin, precisely on the Aulla lacustrine deposit, which underlies by about 200 m, both stratigraphically and geometricall", the Olivola village, known for its famous Villafranchian fauna.
This research has revealed;

a very rich palynoflora and a long, complex, vegetational succession. dominated by arboreal formations, with high abundance of exotic taxa, including also tropical-subtropical elements;
a climatic Sequence characterized by oscillations reflecting seasonality, especially in pluvial regime. A most evident climatic change occurs in the middle of the sequence.

Moreover, the palynological sequence made it possible:

to assign the examined sequence to the Pliocene, because of the abundance of "Tertiary" elements (Taxodium-type, Sciadopitys, Sequoia-type, Nyssa, Palmae, etc.);
to-ascertain the rather archaic character of the Aulla pollenflora because of the significant occurrence Of pollen assemblages mainly confined to pre-Pliocene and early Pliocene (Symplocos, Sapotaceae, Clethraceae/Cyrillaceae-type, Magnolia-type, Sapindaceae- type, Sterculiaceae, cfr. Castanopsis, Tricolporopollenites sp. of archaic-type, etc.);
to compare the Aulla pollenflora with Other Pliocene pollen microfloras from Italy and Other areas and to evidence affinities and differences.

From these comparisons it appears clearly that the Aulla lacustrine episode represents the most ancient continental Pliocene deposit discovered in Italy by means of pollen analyses so far. In fact, the palynological and climatic features indicate that the pollen sequence of Aulla is certainly older than the establishement of glacial/interglacial climatic cycles in the Northern Hemisphere (—2,5 Ma). Also the Villafranca d'Asti deposit (Early Villafranchian in age) is older than 2,5 Ma on the base of the paleomagnetic data. But the pollen floras of Villafranca d'Asti (Fornace R.D.B.) do not include the pre- Pliocene and early Pliocene elements, which characterize the Aulla pollen records.
All these considerations lead to Suggest an older chronostratigraphic collocation of the Aulla sequence, most likely in a pre-Vilafranchian interval, i.e., in the Ruscinian stage interval. The large floristic affinities with the pollen zones of the Brunssumian of the Netherlands, entirely included in the Ruscinian stage, and also the pollen affinities with the continental middle-Pliocene western-alpine deposits support the chronostratigraphical assignation of the Aulla deposit to a (probably late) Ruscinian phase.
Finally, the pollen record of Aulla represents a particular uniform floristic biozone, which is named here "Macrian" phase, easily distinguished from the contiguous vegetational biozones.
The results reported above allow to extend the chronostratigraphic scheme of the paleofloristic evolution in Northern-Central Italy during the Pliocene.
MICROFACIES AND SPHINCTOZOAN ASSEMBLAGE OF SOME LOWER PERMIAN BRECCIAS FROM THE LERCARA FORMATION (SICILY)
Authors: SENOWBARI-DARYAN BABA , DI STEFANO PIETRO 
Published: November 2023

Some paleozoic calcareous blocks characterized by a rich fossil association, never described before, have been found as elements of the breccias resedimented in the siliciclastic deposits of the Lercara Formation (Western Sicily). These blocks occur in the Cozzo Intronata area (Lercara) and along the River San Filippo (Roccapalumba) mixed with the already known ?Carboniferous calcareous breccias with productid.
The sponge-Tubiphytes boundstone and the algal foraminiferal grainstone/packstone are the two main lithofacies types of these new discovered elements. Their Lower Permian age is supported by fusulinids and algae. They probably derived from the dismantling of a carbonate platform margin.
The present paper, besides describing the sedimentological and paleontological features of these deposits, is particularly devoted to the systematic study of the sphinctozoan sponges that played an important role as framebuilder organisms of the reef limestones together with the abundant inozoans.
10 species are here described. Girtyocoelia beedei (Girty) and Sollasia ostiolata Steinmann are the most frequent species. Other species are rare. A new genus (Parauvanella) and a new species (Cystauletes lercarensis) are introduced.
REMARKS ON THE SCYTHIAN-ANISIAN BOUNDARY
Authors: YI—GANG WANG, 
Published: November 2023

Different definitions of the Scythian—Anisian boundary are discussed. Based on taxa and sequence of Keyserlingites faunas at 19 Boreal localities and 6 Tethyan localities, Keyserlingites faunas are considered to be Late Sparhian in the Boreal province and Early Anisian in the Tethyan province. Keyserislingites not appropriate for cosmopolitan zoning. The base of Lenotropites—Japonites zone of Central Qinghai, China appears to indicate base Middle Triassic: it has abundant earliest Anisian ammonite faunas of mixed Boreal—Tethyan character (ecotone) providing direct correlation between these provinces.
Correlations of Anisian (Aegean), Spathian and the Anisian—Scythian boundary are made between different localities, particularly between the Tethyan and Boreal provinces and between basin and platform facies. Olenikites zone is coeval to Subcolumbites zone; Lenotropites caurus zone to Lenotropites—Japonites zone; Columbites zone to Tirolites cassianus zone;and Subcolumbites zone to Tirolites carniolicus zone.
Scythian—Anisian mixed faunas and stratigraphic condensation are also discussed.
NEW' DATA ON PLANKTONIC FORAMINIFERA BIOSTRATIGRAPHY FROM THE NEOGENE OF THE GARGANO PENINSULA (FOGGIA, SOUTHERN ITALY)
Authors: GIGLIOLA VALLERI 
Published: November 2023

This paper concerns detailed analyses on planktonic foraminifera biostratigraphy of a section outcropping in the area of Poggio Imperiale, the western side of Gargano (FG)
The sediments overlying the mesozoic carbonate platform have been assigned to Globorotalia puncticulata Zone (Early Pliocene) and to Globorotalia inflata Zone (Late Pliocene). A Middle Pliocene stratigraphic gap has been recognised.
IL ROSSO AMMONITICO INFERIORE (BAIOCIANO - CALLOVIANO) NEI MONTI LESSINI SETTENTRIONALI (VERONA)
Authors: CLARI P. A. , MARINI P. , PASTORINI M. , PAVIA G. 
Published: November 2023

The aim of this paper is the description, from both the biostratigraphical and sedimen• tological point of view, Of the lower member of the Rosso Ammonitico Veronese, one of the most known red, nodular, pelagic limestones of the mediterranean Jurassic.
The R.A.V. is a condensed sequence Of red, mostly nodular, limestones, Often rich in internal molds Of ammonites, which is areally restricted to the "Trento Ridge", a structural high isolated in the early Jurassic by the rifting Of a Triassic, large epicontinental carbonate—platform. It spans in age from late Bajocian to Tithonian and is separated from the underlying shallow—water carbonates Of Liassic and Aalenian age by a sharp break in sedimentation, underlined by a mineralized hard ground, which lasted for all early and middle Bajocian.
Two members may bc recognized in the R.A.V.: a lower (Rosso Ammonitico Inferiore) and an upper one (Rosso Ammonitico Superiore) separated by a stratigraphic gap. The lower member, ranging in age from late Bajocian to middle Callovian, is well developed only in the southern part of the 'Trento Ridge" (i. e. in the Lessini Veronesi area) and has a variable thickness which reaches a maximum of 8 meters.
In search of the Palaeogene-Neogene Boundary Stratotype
Authors: GELATI R. , STEININGER F. F. 
Published: November 2023

In publishing the first results of its research works (Giornale di Geologia, vol. XLIV, fasc. l-Il, 1981 ) the Palaeogene/Neogene Boundary Working Group, while not having defined any final object yet, has nonetheless enabled us to: a) recall attention to the existence of lithofacies (e. g. turbidites, volcanoclastic rocks) of great significance with respect to the geodynamical situation of the Mediterranean; b) to clarify the significance of some first class faunal markers, particularly as regards planktonic foraminfera.
These results permitted to direct the course of subsequent research works carried out by the Group, m the way of giving to the International Commission on Stratigraphy. some objective data for a satisfactory solution of the problem.
I CORALLI DEL CALCARE Dl ZU (TRIASSICO SUPERIORE) DELLA LOMBARDIA (ITALIA)
Authors: FANTINI SESTINI N. , MOTTA E. 
Published: November 2023

The present study deals with a detailed taxonomic study Of the Scleractinia from the middle and upper parts of the Calcare di Zu (Zu Limestone), a formation outcropping in the Central Lombardy and dated as Rhaetian (Late Triassic).
The specimens examined belong to the Collections of the Natural History of the Cities of Bergamo and Milano. Some specimens deposited at the Museum in Milano belong to the original collection of Stoppani (figured by this author in 1857 to 1865 papers).
According the present revision, the genus Stylophyllopsis Frech, 1890 is a junior synonym of the genus Lepiconus Stoppani, 1857 and Retiophyllia paraclathrata Roniewicz, 1974 is a junior synonym of Retiophyllia langobardica (Stoppani, 1857). The fauna consists of 11 species, belonging to the genera: Cyathocoenia, Astraeomorpha, Pamiroseris, Palaeastraea, Lepiconus, Stylophyllum, Retiophyllia and «Thecosmilia».
Some of the identified species are known only from Stoppani Collection. Someothers, instead, have a larger distribution and are recorded from the northern Side of the Alps, from the Tatra Mountains, Iran, Pamir, and from Northern America.
ASPETTI STRATIGRAFICI E STRUTTURALI DELL'ELEMENTO DI BORGHETTO D'ARROSCIA (ALPI MARITTIME)
Authors: GALBIATI B. , OXILIA M. 
Published: November 2023

The Borghetto d' Arroscia sequence begins with a little known basel post, followed by two lithostratigraphic Units: the M. Bignone Quartzites (Paleocene ? —Eocene ? ) and the Ubaga Limestones (Eocene).
Three deformation phases affected the tectonic evolution of the Borghetto d'Arroscia element. They are shown by the minor structures (at outcrop scale) and by the major ones, surveyed at 1/10.000 scale. The first two phases are vergent outwards. The former (Fl ) is characterized by southvergent recumbent folds, the latter (Fl b) gives cut planes slightly dipping, forming the overthrust surface to the same direction. The third phase (F2) is retrovergent and does not change the general structural setting already reached.
The Concretization of Criminal Sanctions by Judges to Support Corruption Eradication
Authors: Soetopo Maria Grasia Sari 
Published: November 2023

The criminal act of corruption is a crime that has long been known to mankind. Various efforts in Indonesia have been carried out to increase the effectiveness of corruption eradication. Such support is demonstrated by the Supreme Court through the issuance of Supreme Court Regulation Number 1 of 2020 concerning Sentencing Guidelines for Article 2 and Article 3 of the Eradication of Corruption Crimes Law (Perma No. 1 of 2020). However, this regulation lacks concrete formulation of criminal sanctions and insight of corruption impacts on society. The aim of this research is to analyze approaches for judges in concretizing their considerations when imposing criminal sanctions to support the eradication of corruption. This research was prepared using normative legal research methods and supported by descriptive economic analysis. The result of this study shows the need for improvements to Perma No. 1 of 2020 by focusing the impacts of corruption on legal developments in society. These efforts, moreover, need to be supported by reviewing the range of criminal sanctions contained in the provisions of Article 2 and Article 3 of the Law concerning the Eradication of Corruption Crimes, as well as Article 603 and Article 604 of Law Number 1 of 2023 concerning the Criminal Code.
APLICAÇÃO DA JURIMETRIA PARA O APRIMORAMENTO DA PRESTAÇÃO JURISDICIONAL
Authors: Dos Santos Albuquerque Otávio 
Published: November 2023

O objetivo deste trabalho é fazer uma reflexão sobre a importância da Jurimetria para a resolução de conflito com razoável duração do processo e com qualidade, nos termos previstos em nossa Constituição Federal de 1988, na Era Digital. Verifica-se que, com as crescentes demandas judiciais, faz-se necessária a utilização da tecnologia para que o Poder Judiciário cumpra efetivamente com o que determina a nossa Carta Magna acerca da entrega da tutela jurisdicional com qualidade e razoável duração. A Jurimetria é um método científico que tem por escopo analisar o comportamento do demandante do serviço do Poder Judiciário e as decisões tomadas pelo órgão judicante em blocos de processos relacionados a assuntos estratégicos, cujos resultados, ao serem cruzados com o comportamento litigante do demandante, permitem analisar o impacto social das decisões judiciais na sociedade, contribuindo para o aperfeiçoamento de políticas públicas e de prestação da tutela jurisdicional. A Jurimetria consiste em uma nova metodologia de compreensão da realidade social, em que se juntam a Estatística e o Direito, buscando interpretar, de forma qualitativa e quantitativa, a realidade levada diariamente ao julgamento do Poder Judiciário por meio dos processos judiciais. Não se pretende aqui esgotar o assunto, mas evidenciar os benefícios que podem ser alcançados com o seu emprego para a jurisprudência, bem como tecer breves críticas sobre os pontos positivos e negativos de sua aplicabilidade. Essa análise somente poderá ocorrer com o uso de método da estatística. Criada nos anos 50 nos Estados Unidos e desenvolvida posteriormente na Holanda, a Jurimetria congraça a Ciência, a Estatística e o Direito, permitindo novas formas de interpretação dos dados existentes no Poder Judiciário.
LGPD E PROPORCIONALIDADE
Authors: Alberton Junior Germano 
Published: November 2023

Neste artigo, visa-se relacionar as normas de controle das atividadesde tratam ento de dados, especialmente os princípios estabelecidos nos incisos II e III do art. 6º da Lei Geral de Proteção de Dados – LGPD, com as fases do teste de proporcionalidade, a fim de estabelecer a compatibilidade entre essas categorias e a possibilidade de um procedimento de fundamentação progressiva para as decisões acerca dos conflitos entre as atividades de tratamento dos dados e o princípio que determina a proteção dos dados pessoais.
Improving germination and growth performances of millet grown under saline conditions through seed priming
Authors: Ellouzi Hasna , Amraoui Souhir , Hanana Mohsen 
Published: November 2023

L’amorçage (priming) est une technique de traitement pré-germinatif qui consiste à imbiber la semence puis à la re-déshydrater avant la percée de la radicule. Notre travail consiste à étudier l’effet de deux agents de prétraitement des graines, notamment le PEG (20%) et l’AG3 (50 ppm) sur les performances germinatives, la croissance et l’hydratation des plantules de mil cultivées en présence de 100 mM NaCl. Notre objectif principal consiste à améliorer le phénotype et le comportement du mil cultivé sous contrainte saline via l’optimisation de l’amorçage des semences. Les résultats obtenus montrent que tous les types d’amorçage ont un effet bénéfique. Toutefois, le prétraitement des graines avec l’AG3 semble fortement associé à des processus mettant en jeu la croissance. Ce composé stimule de 100% la germination dès le 6ème jour de mise en germination en milieu salin. Cet effet est accompagné d’une amélioration de la croissance (193%) et d’une meilleure hydratation (330%), relativement aux plantes témoins. Cette réponse est primordialement liée à une capacité de détecter rapidement le stress salin et de le rendre facilement interprétable et même bénéfique pour sa croissance en milieux extrêmes.
СПРОБА Б. ШЕРЕМЕТЄВА СТАТИ ГЕТЬМАНОМ (1700–1701 рр.)
Authors: Павленко Сергій 
Published: November 2023

Метою запропонованої студії є висвітлення подій 1700–1701 рр. щодо невдалої спроби Б. Шереметєва посісти гетьманське крісло. Методи. Проблемно-хронологічний. Моніторинг джерел, студій про події 1690-х – поч. 1700-х рр. Новизна. Уперше автор звернув увагу на джерела, які демонструють активну участь царського високопосадовця Б. Шереметєва у змові, яка мала привес- ти до повалення гетьмана І. Мазепи. Для цього був обраний зручний момент – участь багатьох козацьких полків у поході, віддаленість володаря булави від похідного табору, негаразди з організацією наказним гетьманом І. Обидовським військових дій. Участь родича володаря булави, київського полковника К. Мокієвського, у заходах із зміни влади в Батурині на користь боярина Б. Шереметєва показує, що фактично старшина була вже готова здати свого володаря на розтерзання Москві. Вона вже прийняла згадане як неминучу реальність, санкціоновану самим царем. Поламала плани змовників і кандидата на гетьманську посаду несподівана смерть племінника І. Мазепи, ніжинського полковника І. Обидовського. Висновки. Події 1700–1701 рр. указують на дуже хистке становище І. Мазепи у владній системі Московського царства. Б. Шереметєв ще в 1693 р. отримав докази таємної антицарської діяльності гетьмана. Саме він був натхненником та співучасником доносу Д. Забіли 1699 р., а у 1700 р. написав доповідь царю про зрадливість українців. Отримавши під час походу 1700–1701 рр. зверхність над козацькими полками, боярин став таємним організатором скинення І. Мазепи з уряду. Завадила цим підступним діям раптова і несподівана смерть І. Обидовського, який, схоже, вирішив у такий спосіб зруйнувати плани зловмисників, попередити дядька про загрозу його правлінню.
УЧАСТЬ ЗЕМСТВ ТА СIЛЬСЬКОГОСПОДАРСЬКИХ ТОВАРИСТВ НАДДНIПРЯНСЬКОЇ УКРАЇНИ В ОРГАНIЗАЦIЇ ЗОВНIШНЬОЇ ТОРГIВЛI АГРАРНОЮ ПРОДУКЦIЄЮ наприкінці ХIХ – на початку ХХ ст.
Authors: Пилипенко Олександр 
Published: November 2023

Метою розвідки є вивчення iсторiї виникнення та дiяльності земств та ciльськогосподарських товариств, їх участь в експортi аграрної продукції з українських губерній Російської імперії наприкінці ХІХ – поч. ХХ ст., аналіз з’ясування місця і ролі українських земель у загальноімперській структурі експортно-імпортних відносин; визначення залежності державного регулювання у цій сфері від місцевої господарської специфіки та пріоритетів регіональних підприємницьких кіл. Методи дослідження добиралися відповідно до поставленої мети на основі принципів об’єктивізму та науковості. Переважно використовувався метод аналізу та дедукції для інтерпретації архівних джерел. Наукова новизна полягає в тому, що виокремлено такі провідні передумови діяльності земств та сільськогосподарських товариств: історичні, географічні, фiнансовi, освiтнi, демографічні, соціальні. Акцентовано на значенні цього виду діяльності земств і сільськогосподарських товариств у повiтах та селищах, де вони працювали. Досліджено основнi види дiяльностi земств та сільськогосподарських товариств, головні чинники, що визначали якісні й кількісні характеристики наприкінці ХІХ – на поч. ХХ ст.: соціально-політичні, соціально-економічні, господарські. Доведено, що зазначені передумови та чинники справили значний вплив на формування провідних тенденцій розвитку та діяльності українських сільськогосподарських товариств у порефор- мений період. Виділено основні періоди діяльності земств та сільськогосподарських товариств. Охарактеризовано окремі види господарської діяльності. Простежено тенденції та зміст цієї діяльності в контексті проведення земської реформи і суспільно-економічного розвитку країни. Зазначено, що кінець ХІХ – поч. ХХ ст. характеризувалися не тільки безпосередньо діяльністю великого капіталу, але й селянських організацій. У результаті вивчення діяльності земств Київської, Харківської, Подільської та інших губерній визначено головні тенденції розвитку громадських організацій. Зроблено висновок, що діяльність сільськогосподарських товариств залежала вiд багатьох факторiв: економічного розвитку губернiй, рiвня органiзацiї зовнiшньої торгiвлi, темпiв проведення економiчних реформ.