Building Connections for Global Geoconservation
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Nazik Gölü (Bitlis, Türkiye) Güneybatısından Alınan N3 Karotunun Palinolojik İlk Bulguları
Yüzüncü Yıl Üniversitesi Fen Bilimleri Enstitüsü Dergisi/ Journal of the Institute of Natural & Applied Sciences 23 (3): 291-296, 2018 Geliş Tarihi: 12.11.2018 Araştırma Makalesi / Research Article Kabul Tarihi: 23.11.2018 Nazik Gölü (Bitlis, Türkiye) Güneybatısından Alınan N3 Karotunun Palinolojik İlk Bulguları Güldem Kamar Van Yüzüncü Yıl Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü, Van, Türkiye e-posta: [email protected] Özet: Bu çalışma, Nazik Gölü (Bitlis) N3 sediman karotunun palinolojik ilk bulgularını içermektedir. Karot, gölün güneybatı bölümünden, 9 m su derinliğinden gravite karotiyer kullanılarak alınmıştır. 55 cm uzunluğundaki bu karottan alınan örneklerden elde edilen palinolojik verilere göre, göl çevresinde, çökelme süresince otsu bir paleoflora hakim olmuştur. Büyük oranda Poaceae familyasına ait polenlerin baskın olduğu gözlenmiştir. Elde edilen flora, günümüzdeki bitki örtüsü ile benzer olup çökelim süresince göl çevresinde step vejetasyonunun baskın olduğunu göstermektedir. Anahtar kelimeler: Nazik Gölü, Bitlis, Palinoloji, Holosen. Preliminary Palynological Findings of theN3 Core from Southwest of Lake Nazik (Bitlis, Turkey) Abstract: This study includes preliminarily palynological findings of the N3 sedimentcore from Lake Nazik (Bitlis). The core was taken from 9 m water depth by using gravity corer from the southwestern side of Lake Nazik. According to palynological data from the samples of this core, 55 cm in length, herbaceous palaeoflora was been dominated during the deposition surroundings of the lake. The palaeoflora was mainly dominated by Poaceae pollen grains are similar to the recent flora and points out the dominance of steppe vegetation around the lake. Key words: Lake Nazik, Bitlis, Palynology, Holocene. Giriş buzularası dönemlerde, toplam otsu ve odunsu polen yüzdeleri sürekli olarak Göller, organik malzeme içeriği değişmektedir (Litt ve ark., 2014). -
Environmental, Socioeconomic and Cultural Heritage Baseline Page 2 of 382 Area Comp
ESIA Albania Section 6 – Environmental, Socioeconomic and Cultural Heritage Baseline Page 2 of 382 Area Comp. System Disc. Doc.- Ser. Code Code Code Code Type No. Project Title: Trans Adriatic Pipeline – TAP AAL00-ERM-641-Y-TAE-1008 ESIA Albania Section 6 - Environmental, Document Title: Rev.: 03 Socioeconomic and Cultural Heritage Baseline TABLE OF CONTENTS 6 ENVIRONMENTAL, SOCIOECONOMIC AND CULTURAL HERITAGE BASELINE 11 6.1 Introduction 11 6.2 Offshore Biological and Physical Environment 11 6.2.1 Introduction 11 6.2.2 Geographical Scope of the Baseline 13 6.2.3 Methodology and Sources of Information 13 6.2.3.1 Video Methodology 13 6.2.3.2 Environmental Survey Methodology 13 6.2.4 Legislation 15 6.2.4.1 Designated Sites 15 6.2.4.2 Sensitive and Protected Habitats / Biocenoses 16 6.2.5 Regional Overview 16 6.2.5.1 Introduction 16 6.2.5.2 Physical Environment 16 6.2.5.3 Biological Baseline 33 6.2.6 Albanian Nearshore Study Area 56 6.2.6.1 Physical Baseline 56 6.2.6.2 Biological Baseline 69 6.3 Offshore Socioeconomic Environment 73 6.3.1 Introduction 73 6.3.2 Harbours 75 6.3.2.1 Durrës Harbour 75 6.3.2.2 Vlorë Port 76 6.3.3 Marine Traffic 76 6.3.3.1 Ferry Traffic 79 6.3.4 Fishing 80 6.3.4.1 National Overview 80 6.3.5 Cultural Heritage 87 6.3.6 Marine Ammunition / Unexploded Ordnances (UXO) 88 6.4 Onshore Physical Environment 89 6.4.1 Climate and Ambient Air Quality 89 6.4.1.1 Overview 89 6.4.1.2 Climate 89 6.4.1.3 Wind 99 6.4.1.4 Ambient Air Quality 103 6.4.1.5 Key Findings and Conclusions 107 6.4.1.6 Limitations 108 6.4.2 Acoustic Environment 108 6.4.2.1 Acoustic Environment along the Pipeline Route 108 6.4.2.2 Acoustic Environment at CS03 112 6.4.2.3 Acoustic Environment at CS02 116 6.4.2.4 Limitations 120 6.4.3 Surface Water 120 6.4.3.1 Introduction 120 6.4.3.2 River Hydro-Morphology 121 6.4.3.3 Water Quality 127 6.4.3.4 Sediment Quality 137 6.4.3.5 Key Findings and Conclusions 141 Page 3 of 382 Area Comp. -
Program Program
ODTÜ Kültür ve Kongre Merkezi 70th GEOLOGICAL CONGRESS OF TURKEY CULTURAL GEOLOGY AND GEOLOGICAL HERITAGE 10-14 Nisan / April 2017 / Ankara PROGRAM PROGRAM Birleşmiş Milletler UNESCO Eğitim, Bilim ve Kültür Türkiye Kurumu Millî Komisyonu Katkılarıyla... With contribution of... United Nations Turkish Educational, Scientific and National Commission Hatay Sokak No: 21 Kocatepe/ANKARA Cultural Organization for UNESCO www.jmo.org.tr - www.jeolojikurultayi.org Organisation Commission des Nations Unies nationale turque pour l'éducation, pour l'UNESCO la science et la culture ODTÜ Kültür ve Kongre Merkezi Nizamettin KAZANCI Başkan/President - Ankara Unv. Nazire ÖZGEN ERDEM Yüksel ÖRGÜN II. Başkan/Vice Presidents II. Başkan/Vice Presidents Cumhuriyet Unv. İstanbul Teknik Unv. Sadettin KORKMAZ Melahat BEYARSLAN II. Başkan/Vice Presidents II. Başkan/Vice Presidents Karadeniz Teknik Unv. Fırat Unv. Levent KARADENİZLİ Sonay BOYRAZ ASLAN Sekreter/Secretary Sekreter/Secretary İ. Nejla ŞAYLAN Düzgün ESİNA Sosyal ve Kültürel Etkinlikler Sosyal ve Kültürel Etkinlikler Social and Cultural Activities Social and Cultural Activities Ümit UZUNHASANOĞLU Deniz IŞIK GÜNDÜZ Sosyal ve Kültürel Etkinlikler Sosyal ve Kültürel Etkinlikler Social and Cultural Activities Social and Cultural Activities Malik BAKIR H. İbrahim YİĞİT Sayman/ Treasury Sayman/ Treasury Murat AKGÖZ Zeynep Yelda CUMA Basın ve Halkla İlişkiler Basın ve Halkla İlişkiler Public Relations Public Relations İlhan ULUSOY Basın ve Halkla İlişkiler Public Relations Levent KARADENİZLİ - Sonay BOYRAZ ASLAN 70. Türkiye Jeoloji Kurultayı Sekreteryası TMMOB Jeoloji Mühendisleri Odası Hatay Sokak No: 21 Kocatepe/ANKARA www.jmo.org.tr [email protected] Tel: + 90 312 434 36 01 - Fax: +90 312 434 23 88 PB 1 ODTÜ Kültür ve Kongre Merkezi Hüseyin ALAN Başkan (President) Yüksel METİN II. -
V2-1 中 Main English.Ai
Final Report, December 2012 The Project for Tirana Thematic Urban Planning 7.6 Enhancement of On-going Project and Expansion for Sewerage System The consulting services for Greater Tirana Sewerage Improvement Project commenced in February 2010 based on the contract made in October 2009 between MOPWT and the Consultant. Their work includes the following nine components. Review of Basic Design, Existing Studies and Preparation of Necessary Materials; Detailed Design (D/D) for First Stage project; Assistance of Tender and Contract Procedures; Construction Supervision; Development and Implementation of Environmental Management and Monitoring Plan; Training for Sewerage Sectors’ O&M and Other Technical and Institutional Training; Awareness Raising and Education Campaign to promote house connections; Feasibility Study for Second Stage project; and Institutional Capacity Building of DPUK (and/or Project Implementation Unit: PIU). Through the review of Consultants’ design report and discussion with them, the following 11 points are notably described to enhance the on-going project and also the next stage plan. (1) Development of Self-financed Construction of the Sewer Pipes The branch sewer in the on-going loan project was shortened from the original 27.6 km in 2007 JICA Report to 8.85 km in pre-qualification public notice following discussions with DPUK and UKT. To secure the inflow volume at the first stage, it is required that UKT self-finance construction of the branch sewer defined as out of scope of the loan project within priority project area. (2) Assistance to Phase II of the Kashar SD Japanese ODA loan consultant is required to prepare the Feasibility Study Report of Phase II of Kashar SD before the end of Phase I construction work so that a series of processes from financial arrangements to the contract will be smoothly executed. -
The Apennines, the Dinarides, and the Adriatic Sea: Is the Adriatic Microplate a Reality?
Geogr. Fis. Dinam. Quat. 32 (2009), 167-175, 13 figg. CLIFF D. OLLIER (*) & COLIN F. PAIN (**) THE APENNINES, THE DINARIDES, AND THE ADRIATIC SEA: IS THE ADRIATIC MICROPLATE A REALITY? ABSTRACT: OLLIER C.D. & PAIN C.F., The Apennines, the Dinarides, here called the Dinaride Mountains (which is sometimes and the Adriatic Sea: is the Adriatic Microplate a reality?. (IT ISSN 0391- split into different ranges in different countries, such as the 9838, 2009). Albanides in Albania) as shown in fig. 1. Structurally both The Apennines and the Dinarides consist of nappes thrust towards the Apennines and the Dinarides are thrust towards the the Adriatic Sea, which is underlain by largely undisturbed rocks. Plate tectonic reconstructions are very varied, with supposed subduction in Adriatic. The tectonic position of this area is problematic. many different directions. Besides this there is an over-ruling concept In plate tectonic terms the Dinaride Mountains are that a plate called the Adriatic (or Adria) Plate moved north from Africa usually explained as a result of subduction of a plate under to Europe where its collision helped to create the Alps. Some think the plate is still moving. The total tectonic setting, together with palaeonto- the Dinarides. Similarly the Apennines are commonly ex- logical and seismic data, suggests that the older model of two converging nappe belts meeting a common foreland best fits the observed facts. KEY WORDS: Adriatic, Apennines, Dinarides, Plates, Arcs. RIASSUNTO: OLLIER C.D. & PAIN C.F., Gli Appennini, le Dinaridi e il mare Adriatico: la Microplacca Adriatica è una realtà?. (IT ISSN 0391- 9838, 2009). -
Abstract Keywords Distribution and Impacts of Carassius Species
ISSN 1989‐8649 Manag. Biolog. Invasions, 2011, 2 Abstract Distribution and impacts of Carassius species (Cyprinidae) in Turkey: a review Biological invasions have caused considerable disruption to native Deniz INNAL ecosystems throughout the world through predation, habitat alteration, competition and hybridisation with Introduction, Hypotheses and species have been introduced in native species and introduction of Problems for Management Turkey as eggs, fry or fingerlings for diseases or parasites. Species of the different purposes over the last five genus Carassius [C. auratus (Linnaeus, In Europe, three species of the decades. Some of these fish have 1758), C. carassius (Linnaeus, 1758) and genus Carassius Nilsson 1832, are been used only in closed systems C. gibelio (Bloch, 1782)] were known; the goldfish, Carassius while others have been released transported to numerous inland water auratus (Linnaeus, 1758), the into open inland waters throughout bodies throughout Turkey. Species are crucian carp, Carassius carassius the country (Innal & Erk’akan 2006). now considered a threat factor for (Linnaeus, 1758) and the prusian Freshwater fish introductions may native species. The purpose of this (gibel) carp, Carassius gibelio (Bloch, result in impacts as a result of one study is to review the current 1782) (Ozulug et al. 2004). or many undesirable characteristics, distribution and ecological impacts of including: competition, habitat species in the inland waters of Turkey. Whereas C. carassius is alteration, parasitism, predation, native to Turkey, the other two hybridisation, alteration of habitat Keywords species of the genus Carassius were quality and/or ecosystem function, introduced to inland waters of host of pests or parasites (Copp et Carassius carassius, C. -
Environmental Impact Assessment Report Albania
. Wz W ~~~E986 t ~~~~VOL. 4 Public Disclosure Authorized THE REPUBLIC OF ALBANIA THE MINISTRY OF PUBLIC WORKS, TRANSPORT AND TELECOMMUNICATIONS GENERAL ROADS DIRECTORATE ENVIRONMENTAL Public Disclosure Authorized IMPACT ASSESSMENT REPORT Public Disclosure Authorized THE DURRES - MORINE CORRIDOR Milot - Rreshen Section Public Disclosure Authorized MAY 2006 Durres-Morine Road Corridor - Milot to Rreshen Section Proposed Transport Project Environmental Impact Assessment Report Albania CONTENTS Page 0 EXECUTIVE SUMMARY 4 1 INTRODUCTION 18 2 POLICY, LEGAL AND ADMINISTRATIVE FRAMEWORK 19 2.1 POLICY 19 2.2 LEGISLATIVE BACKGROUND 20 - 2.3 INSTITUIONAL REGULATORY FRAMEWORK 24 2.4 RIGHTS OF THE CITIZEN 26 3 PROJECT DESCRIPTION 26 3.1 FUSHE-MILOT TO MILOT SECTION 26 3.2 MILOT TO RUBIK SECTION 29 3.3 RUBIK TO RRESHEN SECTION 33 4 ENVIRONMENTAL BASELINE 36 4.1 GEOLOGY, GEOMORPHOLOGY, SOIL AND HYDROLOGY 37 4.2 CLIMATE, AIR QUALITY AND NOISE 43 4.3 FLORA, FAUNA AND LANDSCAPE 48 4.4 SOCIO-ECONOMICS, NATIONAL AND CULTURAL HERITAGE 53 4.5 TRAFFIC AND ROAD SAFETY 55 5 ENVIRONMENTAL IMPACT 57 5.1 FUSHE-MILOT TO RRESHEN (ALL SECTIONS) 58 5.2 FUSHE-MILOT TO MILOT SECTION 71 5.3 MILOT TO RUBIK SECTION 74 5.4 RUBIK TO RRESHEN SECTION 75 5.5 MITIGATION MEASURES (ALL SECTIONS) 76 6 ANALYSIS OF ALTERNATIVES 82 6.1 ALTERNATIVES CONSIDERED 82 6.2 ASSESSMENT OF ALTERNATIVES 84 6.3 CUMULATIVE ASSESSMENT 89 6.4 SELECTED ALTERNATIVE 90 7 ENVIRONMENTAL MANAGEMENT PLAN (EMP) 90 7.1 ENVIRONMENTAL MITIGATION MEASURES 90 7.2 MITIGATION PROGRAMME 93 7.3 INSTITUTIONAL ARRANGEMENTS AND STRENGTHENING 93 7.4 ENVIRONMENTAL MONITORING PLAN 101 2 Durres-Morine Road Corridor - Milot to Rreshen Section Proposed Transport Project Environmental ImDact Assessment Report Albania 8 PUBLIC CONSULTATION AND INFORMATION DISCLOSURE 110 9 RESETTLEMENT ACTION PLAN 113 10 APPENDICES 114 APPENDIX 1. -
The Alpine-Carpathian-Dinaridic Orogenic System: Correlation and Evolution of Tectonic Units
1661-8726/08/010139–45 Swiss J. Geosci. 101 (2008) 139–183 DOI 10.1007/s00015-008-1247-3 Birkhäuser Verlag, Basel, 2008 The Alpine-Carpathian-Dinaridic orogenic system: correlation and evolution of tectonic units STEFAN M. SCHMID 1, DANIEL BERNOULLI 1, BERNHARD FÜGENSCHUH 2, LIVIU MATENCO 3, SENECIO SCHEFER 1, RALF SCHUSTER 4, MATTHIAS TISCHLER 1 & KAMIL USTASZEWSKI 1 Key words: tectonics, collisional Orogens, Ophiolites, alps, Carpathians, Dinarides ABSTRACT A correlation of tectonic units of the Alpine-Carpathian-Dinaridic system of geometries resulting from out-of-sequence thrusting during Cretaceous and orogens, including the substrate of the Pannonian and Transylvanian basins, is Cenozoic orogenic phases underlay a variety of multi-ocean hypotheses, that presented in the form of a map. Combined with a series of crustal-scale cross were advanced in the literature and that we regard as incompatible with the sections this correlation of tectonic units yields a clearer picture of the three- field evidence. dimensional architecture of this system of orogens that owes its considerable The present-day configuration of tectonic units suggests that a former complexity to multiple overprinting of earlier by younger deformations. connection between ophiolitic units in West Carpathians and Dinarides was The synthesis advanced here indicates that none of the branches of the disrupted by substantial Miocene-age dislocations along the Mid-Hungarian Alpine Tethys and Neotethys extended eastward into the Dobrogea Orogen. Fault Zone, hiding a former lateral change in subduction polarity between Instead, the main branch of the Alpine Tethys linked up with the Meliata- West Carpathians and Dinarides. The SW-facing Dinaridic Orogen, mainly Maliac-Vardar branch of the Neotethys into the area of the present-day In- structured in Cretaceous and Palaeogene times, was juxtaposed with the Tisza ner Dinarides. -
Isolation and Interaction in the Shala Valley of Northern Albania
READ ONLY / NO DOWNLOAD READ ONLY / NO DOWNLOAD LIGHT AND SHADOW READ ONLY / NO DOWNLOAD COTSENCOTSEN INSTITUTE INSTITUTE OF OFARCHAEOLOGY ARCHAEOLOGY PRESS PRESS MONUMENTA ARCHAEOLOGICA Volume 27 Last House on the Hill: BACH Area Reports from Çatalhöyük, Turkey edited by Ruth Tringham and Mirjana Stevanović Volume 26 The History and Archaeology of Jaffa 1 edited by Martin Peilstöcker and Aaron A. Burke Volume 24 The Early Iron Age Cemetery at Torone by John K. Papadopoulos Volume 23 The Plain of Phaistos: yclesC of Social Complexity in the Mesara Region of Crete by L. Vance Watrous, Despoina Hadzi-Vallianou, and Harriet Blitzer Volume 22 K’axob: Ritual, Work, and Family in an Ancient Maya Village edited by Patricia A. McAnany Volume 21 The Sydney Cyprus Survey Project: Social Approaches to Regional Archaeological Survey by Michael Given and A. Bernard Knapp Volume 20 Prehistoric Sitagroi: Excavations in Northeast Greece 1968–1970 Volume 2: Final Report edited by Ernestine S. Elster and Colin Renfrew READ ONLY / NO DOWNLOAD LIGHT AND SHADOW Isolation and Interaction in the Shala Valley of Northern Albania Michael L. Galaty, Ols Lafe, Wayne E. Lee, and Zamir Tafilica Editors MONUMENTA ARCHAEOLOGICA 28 COTSEN INSTITUTE OF ARCHAEOLOGY PRESS READ ONLY / NO DOWNLOAD THE COTSEN INSTITUTE OF ARCHAEOLOGY PRESS is the publishing unit of the Cotsen Institute of Archaeology at UCLA. The Cotsen Institute is a premier research organization dedicated to the creation, dissemination, and conservation of archaeological knowledge and heritage. It is home to both the Interdepartmental Archaeology Graduate Program and the UCLA/Getty Master’s Program in the Conservation of Archaeological and Ethnographic Materials. -
Archives of Petroleum & Environmental Biotechnology
Archives of Petroleum & Environmental Biotechnology Velaj T. Arch Pet Environ Biotechnol APEB-127. Review Article DOI: 10.29011/2574-7614. 100027 About the Perspective of Exploration of the Oil and Gas in Sub- thrust of External Albanides, Albania Telo Velaj* Department of Geology, Tirana University, USA *Corresponding author: Telo Velaj, Department of Geology, Tirana University, Warrington PA 18976, USA. Tel: +1 2159096263; Email: [email protected] Citation: Velaj T (2018) About the Perspective of Exploration of the Oil and Gas in Subthrust of External Albanides, Albania. Arch Pet Environ Biotechnol APEB-127. DOI: 10.29011/2574-7614. 100027 Received Date: 22 January, 2018; Accepted Date: 6 February, 2018; Published Date: 12 February, 2018 Abstract The Albanides are part of the Alpine Orogenic belt and represent one most significant of fields in SE Europe. They are located between the Hellendes of Greece and Dina rides of Montenegro, which together form the Southern branch of Mediterranean Alpine belt. During the Jurassic and most of the Cretaceous the Adriatic-Apulia sub-plate moved in the east and northeast direction, relative to Euro Asia. At this time, it was mainly affected by the extensional tectonics, thus forming a series of parallel ridges and forrous. Owing to the different depositional environments, these alterations of horst and graben units structures formed a series of tectonic zones with alternating deep and shallow marine lithofacies. As result of a further Adriatic-Apulia sub-plate movement towards SE during the Late Cretaceous the tectonic style changed from extensional to compression. During the Neogene’s the northwards movement of the African Plate, enhanced compression, leading to a large scale folding and thrusting in the SW direction in Albania and NW of Greece. -
From the Middle Bronze to the Middle Iron Age (Urartu)
TÜBA-AR 20/2017 HIGHLAND FORTRESSES-CEMETERIES AND SETTLEMENT COMPLEXES OF MT SÜPHAN-MUŞ PLAINS IN THE LAKE VAN BASIN: FROM THE MIDDLE BRONZE TO THE MIDDLE IRON AGE (URARTU) VAN GÖLÜ HAVZASI SÜPHAN DAĞI-MUŞ OVALARI YÜKSEK YAYLA KALELERİ-MEZARLIKLARI VE YERLEŞİM KOMPLEKSLERİ: ORTA TUNÇ ÇAĞI’NDAN ORTA DEMİR ÇAĞI’NA (URARTU) Aynur ÖZFIRAT *1 Makale Bilgisi Article Info Başvuru: 5 Aralık 2016 Received: December 5, 2016 Hakem Değerlendirmesi: 5 Ocak 2017 Peer Review: Jenuary 5, 2017 Kabul: 17 Şubat 2017 Accepted: February 17, 2017 Keywords: Muş Plains, Mt Süphan, Middle Bronze Age, Late Bronze-Early Iron Age, Urartu, Lake Van Basin Anahtar Kelimeler: Muş Ovaları, Süphan Dağı, Orta Tunç Çağ, Son Tunç-Erken Demir Çağ, Urartu, Van Gölü Havzası ABSTRACT Fortresses-cemeteries and settlement complexes situated in the high plateau on the western slope of Mt Süphan which were studied in the basin of Lake Van survey is discussed in this article. In many archaeological sites located on Mt Süphan and the surrounding foothills in the Murat Valley-Muş Plains, fortresses and cemeteries, situated on the western slope of the mountain, are in large quantities. The most remarkable sites of our survey are settlement complexes. It seems that highlands, which had been very limitedly used in Early Bronze Age-Kura Araxes, were highly densely populated from Middle Bronze to the Early Iron Age. The cemeteries of Middle Bronze Age, found widespread on the highlands of Mt Süphan, imply the existence of a considerable population, no related settlements is observed. Settlement pattern again changed in the Late Bronze-Early Iron Age, as shown by the highland fortresses- cemeteries. -
Archaeobotanical Studies at the Urartian Site of Ayanis in Van Province, Eastern Turkey
Turkish Journal of Botany Turk J Bot (2013) 37: 282-296 http://journals.tubitak.gov.tr/botany/ © TÜBİTAK Research Article doi:10.3906/bot-1204-3 Archaeobotanical studies at the Urartian site of Ayanis in Van Province, eastern Turkey Tuğba SOLMAZ, Emel OYBAK DÖNMEZ* Department of Biology, Faculty of Science, Hacettepe University, 06800 Beytepe, Ankara, Turkey Received: 03.04.2012 Accepted: 18.09.2012 Published Online: 15.03.2013 Printed: 15.04.2013 Abstract: Archaeobotanical macro remains recovered from the Ayanis fortress and the outer town of the Urartian period of the Iron Age (685–645 BC), located in the area of Van (Turkey), were investigated. Most of the remains were charred due to fire. Large quantities of Hordeum vulgare L. (hulled barley), Panicum miliaceum L. (broomcorn millet), and Setaria italica (L.) P.Beauvois (foxtail millet) were found at the study site, indicating the storage of agricultural surplus. Other types of cereal remains were also recorded, including Triticum aestivum L. (bread wheat) and Secale cereale L. (rye). Ground wheat grains were also recovered and their starch microstructure under scanning electron microscope suggests that these remains represent a bulgur-like food preparation. The data suggest that in the area of Ayanis plant-based agricultural activities were based mainly on cereals in the Iron Age. The findings also include fruits of Carum carvi L. (caraway, Persian cumin), Coriandrum sativum L. (coriander), and Petroselinum crispum (Mill.) Fuss (parsley). In view of the folkloric use of these plants, it is thought that the material from Ayanis represents condiments and/or medicinal herbs used by the Urartians in Anatolia about 2600 years ago.