A Class I Odorant Receptor Enhancer Shares a Functional Motif with Class II Enhancers Tetsuo Iwata1,2,4, Satoshi Tomeoka3,4 & Junji Hirota1,3*
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DNA·RNA Triple Helix Formation Can Function As a Cis-Acting Regulatory
DNA·RNA triple helix formation can function as a cis-acting regulatory mechanism at the human β-globin locus Zhuo Zhoua, Keith E. Gilesa,b,c, and Gary Felsenfelda,1 aLaboratory of Molecular Biology, National Institute of Diabetes and Digestive and Kidney Diseases, National Institutes of Health, Bethesda, MD 20892; bUniversity of Alabama at Birmingham Stem Cell Institute, University of Alabama at Birmingham, Birmingham, AL 35294; and cDepartment of Biochemistry and Molecular Genetics, University of Alabama at Birmingham, Birmingham, AL 35294 Contributed by Gary Felsenfeld, February 4, 2019 (sent for review January 4, 2019; reviewed by James Douglas Engel and Sergei M. Mirkin) We have identified regulatory mechanisms in which an RNA tran- of the criteria necessary to establish the presence of a triplex script forms a DNA duplex·RNA triple helix with a gene or one of its structure, we first describe and characterize triplex formation at regulatory elements, suggesting potential auto-regulatory mecha- the FAU gene in human erythroid K562 cells. FAU encodes a nisms in vivo. We describe an interaction at the human β-globin protein that is a fusion containing fubi, a ubiquitin-like protein, locus, in which an RNA segment embedded in the second intron of and ribosomal protein S30. Although fubi function is unknown, the β-globin gene forms a DNA·RNA triplex with the HS2 sequence posttranslational processing produces S30, a component of the within the β-globin locus control region, a major regulator of glo- 40S ribosome. We used this system to refine methods necessary bin expression. We show in human K562 cells that the triplex is to detect triplex formation and to distinguish it from R-loop stable in vivo. -
Ldb1 Is Essential for Development of Nkx2.1 Lineage Derived Gabaergic and Cholinergic Neurons in the Telencephalon
Developmental Biology 385 (2014) 94–106 Contents lists available at ScienceDirect Developmental Biology journal homepage: www.elsevier.com/locate/developmentalbiology Ldb1 is essential for development of Nkx2.1 lineage derived GABAergic and cholinergic neurons in the telencephalon Yangu Zhao a,n,1, Pierre Flandin b,2, Daniel Vogt b, Alexander Blood a, Edit Hermesz a,3, Heiner Westphal a, John L. R. Rubenstein b,nn a Program on Genomics of Differentiation, Eunice Kennedy Shriver National Institute of Child Health and Human Development, NIH, Bethesda, MD 20892, USA b Department of Psychiatry and the Nina Ireland Laboratory of Developmental Neurobiology, University of California San Francisco, San Francisco, CA 94143, USA article info abstract Article history: The progenitor zones of the embryonic mouse ventral telencephalon give rise to GABAergic and cholinergic Received 1 June 2013 neurons. We have shown previously that two LIM-homeodomain (LIM-HD) transcription factors, Lhx6 and Received in revised form Lhx8, that are downstream of Nkx2.1, are critical for the development of telencephalic GABAergic and 8 October 2013 cholinergic neurons. Here we investigate the role of Ldb1, a nuclear protein that binds directly to all LIM-HD Accepted 9 October 2013 factors, in the development of these ventral telencephalon derived neurons. We show that Ldb1 is expressed Available online 21 October 2013 in the Nkx2.1 cell lineage during embryonic development and in mature neurons. Conditional deletion of Ldb1 Keywords: causes defects in the expression of a series of genes in the ventral telencephalon and severe impairment in the Differentiation tangential migration of cortical interneurons from the ventral telencephalon. -
Open Dogan Phdthesis Final.Pdf
The Pennsylvania State University The Graduate School Eberly College of Science ELUCIDATING BIOLOGICAL FUNCTION OF GENOMIC DNA WITH ROBUST SIGNALS OF BIOCHEMICAL ACTIVITY: INTEGRATIVE GENOME-WIDE STUDIES OF ENHANCERS A Dissertation in Biochemistry, Microbiology and Molecular Biology by Nergiz Dogan © 2014 Nergiz Dogan Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy August 2014 ii The dissertation of Nergiz Dogan was reviewed and approved* by the following: Ross C. Hardison T. Ming Chu Professor of Biochemistry and Molecular Biology Dissertation Advisor Chair of Committee David S. Gilmour Professor of Molecular and Cell Biology Anton Nekrutenko Professor of Biochemistry and Molecular Biology Robert F. Paulson Professor of Veterinary and Biomedical Sciences Philip Reno Assistant Professor of Antropology Scott B. Selleck Professor and Head of the Department of Biochemistry and Molecular Biology *Signatures are on file in the Graduate School iii ABSTRACT Genome-wide measurements of epigenetic features such as histone modifications, occupancy by transcription factors and coactivators provide the opportunity to understand more globally how genes are regulated. While much effort is being put into integrating the marks from various combinations of features, the contribution of each feature to accuracy of enhancer prediction is not known. We began with predictions of 4,915 candidate erythroid enhancers based on genomic occupancy by TAL1, a key hematopoietic transcription factor that is strongly associated with gene induction in erythroid cells. Seventy of these DNA segments occupied by TAL1 (TAL1 OSs) were tested by transient transfections of cultured hematopoietic cells, and 56% of these were active as enhancers. Sixty-six TAL1 OSs were evaluated in transgenic mouse embryos, and 65% of these were active enhancers in various tissues. -
Chronological Constraints of Pyroclastic Deposits on Anafi Island
15th International Congress of the Geological Society of Greece Athens, 22-24 May, 2019 | Harokopio University of Athens, Greece Bulletin of the Geological Society of Greece, Sp. Pub. 7 Ext. Abs. GSG2019-160 Chronological constraints of pyroclastic deposits on Anafi Island, (Cyclades, Greece): Are they Minoan? Katerina Theodorakopoulou1, Konstantinos Kyriakopoulos1, Kostas Stamoulis2, Magali Rizza3, Roberto Sulpizio4, M. Cihat Alçiçek4, Constantin D. Athanassas6 1 Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Greece, [email protected] 2 University of Ioannina-Archaeometry Center, Greece 3 Centre Européen de Recherche et d’Enseignement des Géosciences de l’Environnement, Aix-en-Provence, France 4 Department of Earth and Geo-environmental Sciences, University of Bari Aldo Moro, Italy, 5 Department of Geology, Pamukkale University, Denizli, Turkey 6 Department of Geological Sciences, School of Mining and Metallurgical Engineering, National Technical University of Athens, Greece This study attempts to clarify whether formerly-documented pyroclastic deposits (Keller et al. 2014, McCoy and Dunn, 2002) belong to the Minoan eruption of Santorini or an earlier event. The ‘Minoan’ eruption, occurred in the 17th century BCE (1627–1600 BCE, Friedrich et al., 2006) and had widespread impacts on the civilization of the Aegean an Eastern Mediterranean (Marinatos, 1939). Anafi Island could be a key site for the dispersal of Minoan tephra as it is the most nearby island of Santorini. Despite its proximity, only a few spots with pyroclastic deposits have been found on the island (Keller et al. 2014, McCoy and Dunn, 2002). The occurrence of tephra layers of the Minoan eruption on Rhodes, Kos and western Turkey (Keller, 1980; Eastwood et al., 1999), suggests that Anafi must have covered by Minoan tephra, which was probably eroded and swept away afterwards (Keller et al., 2014). -
Greeka Guide to Anafi
Anafi in Cyclades Information about villages, beaches, sightseeing, restaurants, activities and more... All the information is this guide is sorted by popularity. For more information please visit our section of Anafi on Greeka.com. What is Greeka.com? Greeka.com is just the most popular website about Greece and the Greek Islands. What to do after you trip? Just visit www.greeka.com and write about your experience, rate the locations you visited and upload your pictures. Map of Anafi Organize your trip to Anafi Greeka.com can also help you organize your entire holiday in Anafi. Thousands of people use our services every year. You can use Greeka.com to: - Buy your ferry tickets online - Book your car rentals - Organize your transfers by taxi and bus - Create a custom island hopping package - Visit Greek areas in an organized tour Anafi p 2/6 Anafi Guide About Anafi Anafi is a small island, located to the east of Santorini. Its shape is triangular and its land is mostly rocky. This island, because of its size, hasn't been too much developed in tourism so it is a great destination for peace and quiet seekers. According to the myth, Anafi rose from the sea to provide shelter for the Argonatus and to protect them from the wild sea. It has got a semi-mountainous structure with Vigla, Kalamos and Agios Ioannis Theologos being their highest peaks. Anafi has many beaches, most of them with fine soft sand and some others pebbled. The port of Agios Nikolaos is the busiest part of Anafi. -
TA GREECE ITINERARIES at a Glance
Mesmerizing Greece Because the Endless Blue just can’t be experienced any other Top Itinerary Options Powered by Endless Blue © by Powered While Greece has a multitude of itinerary options, its most popular are the islands that are found in the region called the Cyclades with islands such as Mykonos, Paros, Naxos and of course the world famous Santorini. Second most popular island cluster is the Argo Saronic known for its calm waters, protected coves and traditionally Greek Islands. Some of the islands and coast that are part of this itinerary are the islands of Hydra, location to many Hollywood movies and its donkey only transportation - no cars allowed. The island of Spetses famous for its architecture and pristinely kept island. And of course the Peloponnesus Coast where one can visit the world famous Epidavros the birthplace of theatre. Another popular option with Captains is the combination of these two distinctly different regions giving you the perfect balance of iconic white washed houses with blue shutters combined with majestic stone architecture. History abounds in these two regions ranging from ancient theatre to exquisite antiquity around every corner. Itineraries are always subject to weather conditions at the time of charter but rest assured that the Captain is well experienced in Greek waters Pure Cyclades with Iconic Santorini A look inside: Pure Cyclades are characterized DAY NM Destination by the iconic pictures of blue water against 1 40 Athens-Kea white washed homes perched high on hill tops. The islands are comprised of; Mykonos, 2 40 Kea to Sifnos Amorgos, Anafi, Andros, Antiparos, Delo, Ios, Endless Blue © by Powered Kea, Kimolos, Kythnos, Milos, Naxos, Paros, 3 23 Sifnos to Milos Santorini, Serifos, Sikinos, Sifnos, Syros, Tinos, Folegandros, as well as the "Minor Cyclades" 4 55 Milos to Santorini comprising Donousa, Irakleia, Koufonisia and 5 22 Santorini to Ios Schinoussa. -
Contemporary Kinematics of the South Aegean Area (Greece) Detected with Continuous GNSS Measurements
EGU2020-7656, updated on 03 Oct 2021 https://doi.org/10.5194/egusphere-egu2020-7656 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Contemporary Kinematics of the South Aegean Area (Greece) Detected with Continuous GNSS Measurements Vassilis Sakkas, Chrysa Doxa, Andreas Tzanis, and Haralambos Kranis National & Kapodistrian University of Athens, Department of Geology and the Geoenvironment, Athens, Greece ([email protected]) We examine the kinematic characteristics of the crustal deformation in the broader southern Aegean region using 47 permanent GNNS stations distributed across the eastern Peloponnesus, Attica, Cyclades, Dodecanese, Crete and the coast of western Anatolia. Our analysis is based on the study of velocity vectors relative to local reference points at the western and eastern halves of the study area, as well as on the strain field calculated from absolute velocity vectors across the study area. We demonstrate that the South Aegean region undergoes complex distributed block deformation. At the eastern end of the study area this varies from N210°-N220° extension and with crustal thinning across NE Peloponnesus – Attica, to N210°-N220° compression between the central- eastern Peloponnesus and western Crete, both consistent with the geodynamic setting of the Hellenic Subduction System. A principal feature of the S. Aegean crust appears to be a broad shear zone extending between the islands of Samos/Ikaria and Kalymnos, Paros/Naxos and Amorgos and Milos – Santorini; It exhibits left-lateral kinematics and its southern boundary appears to coincide with the Amorgos – Santorini ridge and comprise the Anhydros basin and associated volcanic field (including Columbo and Santorini). -
Stuttgarter Beiträge Zur Naturkunde
download Biodiversity Heritage Library, http://www.biodiversitylibrary.org/ ? ^Stuttgarter Beiträge zur Naturkunde Serie A (Biologie) Herausgeber: Staatliches Museum für Naturkunde, Rosenstein 1, D-7000 Stuttgart 1 Stuttgarter Beitr. Naturk. Ser. A Nr. 423 22 S. Stuttgart, 15. 11. 1988 The Terrestrial Isopod Genus Schizidium in Western Asia (Oniscidea: Armadillidiidae) By Helmut Schmalfuss, Stuttgart ^'/{<?,/^ With 63 figures ^ ^ l -^.h! 1 -f^OOf^ Summary ^'*-'*'->a=^^^-^'^''''ütb After re-examination of types and investigation of new collections of the western Asiatic species ascribed to the genus Schizidium the foUowing taxa are considered to be valid species: S. davidi (DoUfus, 1887), S. festai (Dollfus, 1894), S. fissum (Budde-Lund, 1885), S. hybndum (Budde-Lund, 1896), S. oertzeni (Budde-Lund, 1896), S. persicum Schmalfuss, 1986, and S. ti- herianum Verhoeff, 1923. Armadillidium hifidum Dollfus, 1905 and probably Schizidium alm.anum Verhoeff & Strouhal, 1967 are Junior Synonyms of S. fissum; Pareluma minuta Omer-Cooper, 1923, Schizidium kalalae Frankenberger, 1939, Armadillidium euphrati Vandel, 1980, and possibly Armadillidium granum Dollfus, 1892 are junior Synonyms of S. davidi. The new species S. osellai, S. reinoehli and S. rausi from Turkey apd S. golovatchi from Armenia are described. New records are presented for S. davidi, S. fissum, S. hybridum, S. oertzeni, and 5'. tiberianum. The diagnostic characters of all treated species are illustrated. Zusammenfassung Die Nachuntersuchung von Typenmaterial und die Auswertung neuer Aufsammlungen der westasiatischen Schizidium-Knen erweisen die folgenden Taxa als gültige Arten: S. davidi (Dollfus, 1887), S. festai (Dollfus, 1894), S. fissum (Budde-Lund, 1885), 5. hybridum (Budde- Lund, 1896), S. oertzeni (Budde-Lund, 1896), S. persicum Schmalfuss, 1986 und S. -
Die Molluskenfauna Der Insel Rhodos, 2. Teil
© Biologiezentrum Linz/Austria; download unter www.biologiezentrum.at Die Molluskenfauna der Insel Rhodos, 2. Teil Christa Frank Stapfia 48, 1997 © Biologiezentrum Linz/Austria; download unter www.biologiezentrum.at © Biologiezentrum Linz/Austria; download unter www.biologiezentrum.at Stapfia 48 179 pp. 30.6.1997 Die Molluskenfauna der Insel Rhodos, 2. Teil1 Christa FRANK Mit einem Vorwort von O.E. PAGET (Wien) Anschrift der Verfasserin: Univ.-Doz. Dr. Christa FRANK Josefstädter Straße 64/11 1080 Wien 1 Herrn Hofrat Dir. Dr. Oliver E. Paget zu seinem 75. Geburtstag im April 1997 in herzlicher Freundschaft gewidmet. © Biologiezentrum Linz/Austria; download unter www.biologiezentrum.at INHALT Vorwort 4 1 Bibliographische Übersicht: Malakologische Literatur, die Insel Rhodos betreffend (1976-1996) 5 1.1 Neue Sammeldaten und Beschreibungen neuer Arten von Rhodos 7 1.2 Veränderungen in der Taxonomie 10 1.3 Ökologische und tiergeographische Studien, die den südlichen ägäischen Raum betreffen 16 2 Fundorte, Geologie und Vegetation 18 2.1 Allgemeines 18 2.2 Die Fundorte 19 2.3 Geologie 25 2.4 Vegetation 26 3 Erklärung der im Text verwendeten Abkürzungen und Hinweise 31 4 Bemerkungen zur Systematik 32 Hygromiidae Tryon 1866 33 Helicidae Rafinesque 1815 36 5 Die festgestellten Arten 36 Metatheba HESSE 1914 37 Metatheba rothi (L. PFEIFFER 1841) 37 Monacha FlTZlNGER 1833 39 Monacha cartusiana (O.F'. MÜLLER 1774) 40 Monacha parumcincta (ROSSMAESSLER 1837) 40 Monacha cartusiana (O.F. MÜLLER 1774), inkl. M. olivieri (FERUSSAC 1821) non RSSM 40 Monacha parumcincta (MENKE1828) 42 Monacha syriaca (EHRENBERG 1831) 43 Cochlicella A. FERUSSAC 1821 48 Cochlicella acuta (O.F. MÜLLER 1774) 48 Cochlicella barbara (LINNAEUS 1759) 51 Xerocrassa MoNTEROSATO 1829 52 Xerocrassa cretica (A. -
Grekland-Oar.Pdf
ädret V ● på Utflykterna 10 egen hand egen ✔ + + PUBLICERAD I MARS 2003 ÖAR ÖAR ÖAR ÖAR ÖAR ÖAR ÖAR ÖAR ÖAR ÖAR ÖAR Fler guider ● charter Sevärdheterna Sevärdheterna Senaste nytt ✔ ● 27 Stränderna Stränderna Skriv ut – och res! ✔ www.aftonbladet.se ● GREKLAND Sommarens Bästa: Vik här dddddddddddddddddddddddddddd dddddddddddddddddddddddddddd dddddddddddddddddddddddddddd dddddddddddddddddddddddddddd dd dddddddddddddddddddddddddddd dddddddddddddddddddddddddddd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd - dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd ädret dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd V dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd dd ● dd dd dd dd dd dd dd dd dd dd dd dd dd -
Role of LDB1 in the Transition from Chromatin Looping to Transcription Activation
Downloaded from genesdev.cshlp.org on September 28, 2021 - Published by Cold Spring Harbor Laboratory Press Role of LDB1 in the transition from chromatin looping to transcription activation Ivan Krivega, Ryan K. Dale, and Ann Dean1 Laboratory of Cellular and Developmental Biology, National Institutes of Diabetes and Digestive and Kidney Diseases, National Institutes of Health, Bethesda, Maryland 20892, USA Many questions remain about how close association of genes and distant enhancers occurs and how this is linked to transcription activation. In erythroid cells, lim domain binding 1 (LDB1) protein is recruited to the b-globin locus via LMO2 and is required for looping of the b-globin locus control region (LCR) to the active b-globin promoter. We show that the LDB1 dimerization domain (DD) is necessary and, when fused to LMO2, sufficient to completely restore LCR–promoter looping and transcription in LDB1-depleted cells. The looping function of the DD is unique and irreplaceable by heterologous DDs. Dissection of the DD revealed distinct functional properties of conserved subdomains. Notably, a conserved helical region (DD4/5) is dispensable for LDB1 dimerization and chromatin looping but essential for transcriptional activation. DD4/5 is required for the recruitment of the coregulators FOG1 and the nucleosome remodeling and deacetylating (NuRD) complex. Lack of DD4/5 alters histone acetylation and RNA polymerase II recruitment and results in failure of the locus to migrate to the nuclear interior, as normally occurs during erythroid maturation. These results uncouple enhancer–promoter looping from nuclear migration and transcription activation and reveal new roles for LDB1 in these processes. -
T.C Istanbul Üniversitesi Sosyal Bilimler Enstitüsü Coğrafya Anabilim Dali
T.C İSTANBUL ÜNİVERSİTESİ SOSYAL BİLİMLER ENSTİTÜSÜ COĞRAFYA ANABİLİM DALI DOKTORA TEZİ KUŞADASI, BODRUM VE PİRE(YUNANİSTAN) YAT LİMANLARININ TURİZM COĞRAFYASI AÇISINDAN KARŞILAŞTIRILMASI OLCAY ŞEMİEOĞLU 2502918894 DANIŞMAN: DOÇ.DR.SÜHEYLA BALCI AKOVA İSTANBUL 2006 TEZ ONAY SAYFASI II ÖZ Kuşadası, Bodrum ve Pire (Yunanistan) yat limanlarının turizm coğrafyası açısından karşılaştırılması adındaki bu çalışmada, ülkemizde yat turizminin başlıca merkezleri olan Bodrum, Kuşadası bölgelerinin ve yat turizminde daha gelişmiş olarak kabul edilen Pire bölgesinin doğal çekicilikleri, zengin tarihi ve yat limanları incelenmektedir. Çalışmamızda araştırılan Bodrum (Karada-Milta) ve Kuşadası (Setur) Marinaları, modern alt yapıları ve uygun ücretleri ile Akdeniz’de seyir halinde olan yerli ve yabancı yatlara birinci sınıf hizmet veren marinalardır. Kuşadası, Bodrum ve Pire yat limanları dünyanın çeşitli bölgelerinden gelen turistleri coğrafi şartlarının sağladığı avantajlardan dolayı etkilemektedirler. Bodrum ve Kuşadası bölgesi tüm dünyadaki diğer tarihi ve arkeolojik yöreler içinde en tanınmış ve bilinen eserlere ve yerlere sahiptir. Yatlarıyla gelen ziyaretçiler Bodrum Milta Marina ve Kuşadası Setur Marina’da gereksindikleri her tür hizmeti almaktadırlar. Bu yüzden tez konumuz olan marinalar Ege ve Akdeniz’de yelken açanlar tarafından tercih edilmektedir. Yat turizminin daha üst noktalara ulaşması için gerekli önlemler alındığında, Kuşadası Setur ve Bodrum Milta Marinalarının gelişen Akdeniz Yat turizmi dünyasında en önde kabul edilen İspanya, Fransa ve İtalya’daki marinalardan daha fazla ilerleyerek, her geçen yıl turizm alanında dünya pazarındaki payını artırarak bir çekim merkezi haline gelen Türkiye’nin en popüler marinaları olarak kabul edileceklerdir. ABSTRACT In the study ‘Comparison of Kuşadası, Bodrum and Piraeus (Greece) Marinas in terms of Tourism Geography’ the natural beauty, rich history and marinas of Bodrum, Kuşadası, accepted as the yacht tourism centers in Turkey, and Piraeus which is considered more developed in yacht tourism is analysed.