Forensic Palynology
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Forensic Palynology: Why Do It and How It Works
Forensic Science International 163 (2006) 163–172 www.elsevier.com/locate/forsciint Editorial Forensic palynology: Why do it and how it works Abstract Forensic palynology has been a law enforcement tool for over 50 years. Forensic palynology is the application of pollen and spores in solving legal issues, either civil or criminal. Pollen and spores can be obtained from an extremely wide range of items, including bodies. Pollen and spores provide clues as to the source of the items and the characteristics of the environments from which the material on them is sourced. Their usefulness lies in a combination of their abundance, dispersal mechanisms, resistance to mechanical and chemical destruction, microscopic size, and morphology. Their often complex morphology allows identification to an individual parent plant taxon that can be related to a specific ecological habitat or a specific scene. Pollen and spore assemblages characterise different environments and scenes and can easily be picked up and transported away from scenes of interest without providing any visual clue to a suspect as to what has occurred. With so many publications and high-profile cases involving forensic palynology and environmental analysis now receiving publicity, the future of this branch of forensic science is assured. Furthermore, with the development of multi-disciplinary approaches to environmental analyses of crime scenes, far more detailed information is now available to law enforcement agencies, enabling them to determine with greater accuracy what may have happened during the commission of criminal activities. # 2006 Elsevier Ireland Ltd. All rights reserved. Keywords: Forensic science; Forensic palynology; Pollen; Spores; Environmental analysis; Trace evidence 1. -
AASP – the Palynological Society Promoting the Scientific Understanding of Palynology Since 1967
AASP – The Palynological Society Promoting the Scientific Understanding of Palynology since 1967 December 2018 NEWSLETTER Volume 51, Number 4 Published Quarterly AASP – TPS NEWSLETTER Published Quarterly by AASP – The Palynological Society December 2018, Volume 51, Number 4 CONTENTS Page 3 | List of AASP-TPS awardees Page 4 | Board of Directors and upcoming deadlines Page 5 | A Message from our President Page 6 | Managing Editor’s Report Page 8 | Candidates to the Board of Directors 2019 Page 12 | Overview of AASP-TPS Awards and Research Grants Page 15 | In Memoriam... Page 18 | News from... Page 20 | Book Reviews Page 21 | Meetings Report Page 28 | Call to Serve - Newsletter open positions Page 29 | AASP Foundation Century Club Page 30 | Upcoming AASP-TPS Meetings Page 31 | 52nd AASP-TPS Annual Meeting - Second Circular Page 33 | Other Meetings and Workshops of Interest AASP The Palynological Society The American Association of Stratigraphic Palynologists, Inc. - AASP - The Palynological Society - was established in 1967 by a group of 31 founding members to promote the science of palynology. Today AASP has a world-wide membership of about 800 and is run by an executive comprising an elected Board of Directors and subsidiary boards and committees. AASP welcomes new members. The AASP Foundation publishes the journal Palynology (quarterly), the AASP Newsletter (quarterly), and the AASP Contributions Series (mostly monographs, issued irregularly), as well as several books and miscellaneous items. AASP organises an Annual Meeting which usually includes a field trip, a business luncheon, social events, and technical sessions where research results are presented on all aspects of palynology. AASP Scientific Medal recipients AASP Board of Directors Award recipient Professor William R. -
Palynology and Its Relation to the Exploration for Oil
The Mountain Geologist v.1, 1964 PALYNOLOGY AND ITS RELATION TO THE EXPLORATION FOR OIL (R. M. A. C. Evening Meeting, February 3, 1964) AUREAL T. CROSS: Michigan State University ABSTRACT: Palynology is one of the branches of paleontology, and more particularly, paleobotany. It deals with the study of pollen, spores, and dissociated degradation detritus of higher plants; spores, fruiting structures and other fragments of algae and fungi; and often includes some entities of similar size belonging to the protozoans or to groups of uncertain affinity. The principal common factor in these. diverse organisms is their small size which requires study under magnifications of from 50 to 1500 diameters. In a restricted sense we consider palynology to be the study of spores, pollen, algae and similar-sized entities and their significance in life, time, space and energy. Pollen and spores were long recognized in sediments and rocks before clear application and significance of their presence was studied. The first major studies in various fields of geological sciences are: a. Pleistocene and Post-pleistocene studies -- analysis of peats, bogs, marshes, etc. for determination of glacial history and history of recent vegetation. Principally introduced by von Post in Northern Europe; later widely developed in U. S. b. Identification and correlation of coal seams and coal-bearing rocks. Firet introduced in Germany 1928-31 and almost immediately in U.S. Widely expanded in U. S. during 1930- 1945. c. Application to various problems in exploration for oil commenced at almost the same tlme in three companies, 1945-47. Fossil plants range from Precambrian (algae) onwards. -
Palynological Interpretation of the Palaeoenvironments of Miocene Strata of the Well Igbomotoru-1, Niger Delta
Palynological interpretation of the palaeoenvironments of Miocene strata of the well Igbomotoru-1, Niger delta F.E. OBOH M.B. SALAMI ~~ J.L. CHAPMAN De~~nrtrneiifof GecJ/Ogynrrd Geophysics, fipnrtincwt of Geoli& De~mtrtrerrtof Enrtlr Scieirc~s, Uriir1ersity of Missoirri, Obofriiii Azt~olorcwUirim7rsit!y, Uiriz~ersityof Cninbrirfp,, Rollr?, IIe-lfr, Nigrrin. Dozor?ii~gStrcrt, Missoriri 65401, U.S.A. Cnttrbridgr, CB2 3EQ, U.K. ABSTRACT Palynological and lithologicalresults have been employed in interpreting the depositional environment of strata penetrated by the Igbomotoru-1 well at the interval 1123-3583 metres. The environment of deposition is largely transitional with marine influence occurring only at the base of the studied sequence. Zonocostitesramonae is frequent to abundant in most samples: this indicates a high influence of mangrove swamp vegetation in the environmentat the time of deposition.The absence or rarity of this species at some horizons within the studied interval is taken as evidence of deposition in a more continental environment or of a swamp forest area composed of non-Rhizophora type trees. The nature of the organic matter points to a source area near the basin of deposition for the sediments. I. ttiicropalaeoritol., 11 (1): 1-6, June 1992. INTRODUCTION SAMPLE SITE AND PREPARATION Studies on various aspects of the structure, sedimentology, Well Igbomotoru-1 is located at latitude 431'40.3"N and stratigraphy and petroleum geology of the Niger delta have longitude 603'29.6"E within the Niger delta (Fig. 1). It was been published by several workers including Allen (1964,1965), drilled to a total depth of 4325 metres by the Shell Petroleum Frank1 & Cordry (1967), Short&Stauble(1967),Adegoke(1969), Development Company of Nigeria. -
About the AAFS
American Academy of Forensic Sciences 410 North 21st Street Colorado Springs, Colorado 80904 Phone: (719) 636-1100 Email: [email protected] Website: www.aafs.org @ AAFS Publication 20-2 Copyright © 2020 American Academy of Forensic Sciences Printed in the United States of America Publication Printers, Inc., Denver, CO Typography by Kathy Howard Cover Art by My Creative Condition, Colorado Springs, CO WELCOME LETTER Dear Attendees, It is my high honor and distinct privilege to welcome you to the 72nd AAFS Annual Scientific Meeting in Anaheim, California. I would like to thank the AAFS staff, the many volunteers, and everyone else who have worked together to create an excellent program for this meeting with the theme Crossing Borders. You will have many opportunities to meet your colleagues and discuss new challenges in the field. There are many workshops and special sessions that will be presented. The Interdisciplinary and Plenary Sessions will provide different views in forensic science—past, present, and future. The Young Forensic Scientists Forum will celebrate its 25th Anniversary and is conducting a workshop related to the meeting theme. More than 1,000 presentations are scheduled that will provide you with more insight into the developments in forensic science. The exhibit hall, always interesting to explore, is where you will see the latest forensic science equipment, technology, and literature. The theme Crossing Borders was chosen by me and my colleagues at the Netherlands Forensic Institute (NFI). We see many definitions of crossing borders in forensic science today. For the 2020 meeting, six words starting with the letters “IN” are included in the theme. -
Optimization of the Pollen Extraction Processfor Improvement of Identification
OPTIMIZATION OF THE POLLEN EXTRACTION PROCESSFOR IMPROVEMENT OF IDENTIFICATION Anja Zlatanović Ana Branković, PhD1 University of Criminal Investigation and Police Studies, Belgrade, Serbia Abstract: Forensic palynology uses microscopic evidence that is resistant to external influences and displacement from the scene. Most suspects may overlook pollen as evidence because they do not know its importance. Pollen provides a myriad of opportunities in forensics: determining the time of year, locality, primary and secondary event venue, connecting participants in a single criminal event, etc. Pollen analysis consists of determining the species and estimating the percentage that each plant species represents in the evidence sample. All methods require preliminary preparation (pollen extraction). A couple of methods for pollen extraction are used, but they are usually either suitable for large samples or require expensive equipment. We tried to optimize some of the existing methods to improve yield. Best results have been achieved using water incubated samples combined with modified acetolysis. Further development and implementation of forensic palynology depend on the simplified procedure and involvement of forensic botanists. Keywords: forensic palynology, identification, extraction optimization, microscopy INTRODUCTION It has been established that trace evidence can be very important in forensic investigations and pollen evidence in particular since it can provide valuable temporal information. Most of the time, the cases where pollen evidence was used represent cases of identification of a crime scene based on the pol- len assemblages present on a suspect or victim or refuting an alibi. Palynology, which is the study of pollen and spores in an archaeological or geological context, has become a well-established research tool leading to many significant scientific developments. -
Sedimentology, Mineralogy, Palynology
Sedimentology, Mineralogy, Palynology, and Depositional History of Some Uppermost Cretaceous and Lowermost Tertiary Rocks along the Utah Book and Roan Cliffs East of the Green ·River U.S. GEOLOGICAL SURVEY BULLETIN 1787-N Chapter N Sedimentology, Mineralogy, Palynology, and Depositional History of Some Uppermost Cretaceous and Lowermost Tertiary Rocks along the Utah Book and Roan Cliffs East of the Green River By KAREN J. FRANCZYK, JANET K. PITMAN, and DOUGlAS J. NICHOLS A multidisciplinary approach to research studies of sedimentary rocks and their constituents and the evolution of sedimentary basins, both ancient and modern l . U.S. GEOLOGICAL SURVEY BULLETIN 1787 ~ EVOLUTION OF SEDIMENTARY BASINS-UINTA AND PICEANCE BASINS ) DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary • U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. UNITED STATES GOVERNMENT PRINTING OFFICE: 1990 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 Library of Congress Cataloging-In-Publication Data Franczyk, Karen J. Sedimentology, mineralogy, palynology, and depositional history of some uppermost Cretaceous and lowermost Tertiary rocks along the Utah Book and Roan Cliffs east of the Green River I by Karen J. Franczyk, Janet K. Pitman, and Douglas J. Nichols. p. em. - (Evolution of sedimentary basins-Uinta and Piceance Basins : ch. N) (U.S. Geological Survey bulletin; 1787) "A multidisciplinary approach to research studies of sedimentary rocks and their constituents and the evolution of sedimentary basins, both ancient and modem." Includes bibliographical references. -
The Terminal Paleozoic Fungal Event: Evidence of Terrestrial Ecosystem Destabilization and Collapse HENK VISSCHER*, HENK BRINKHUIS*, DAVID L
Proc. Natl. Acad. Sci. USA Vol. 93, pp. 2155-2158, March 1996 Ecology The terminal Paleozoic fungal event: Evidence of terrestrial ecosystem destabilization and collapse HENK VISSCHER*, HENK BRINKHUIS*, DAVID L. DILCHERt, WILLIAM C. ELSIKt, YORAM ESHET§, CINDY V. LOOY*, MICHAEL R. RAMPINO1, AND ALFRED TRAVERSEII *Laboratory of Palaeobotany and Palynology, Utrecht University, Heidelberglaan 2, 3584 CS Utrecht, The Netherlands; tPaleobotany Laboratory, Florida Museum of Natural History, University of Florida, Gainesville, FL 32611; tThe MycoStrat Connection, P.O. Box 549, Snook, TX 77878; §Geological Survey of Israel, 30 Malkhe Israel Street, Jerusalem 95 501, Israel; IDepartment of Earth System Science, New York University, 34 Stuyvesant Street, New York, NY 10003; and IlDepartment of Geosciences, Pennsylvania State University, 435 Deike Building, University Park, PA 16802 Contributed by David L. Dilcher, November 20, 1995 ABSTRACT Because of its prominent role in global bio- in the wood of land plants rather than in aquatic organisms. mass storage, land vegetation is the most obvious biota to be Sustained stability of this single largest biotic carbon reservoir investigated for records of dramatic ecologic crisis in Earth is basically determined by a functional equilibrium between history. There is accumulating evidence that, throughout the primary productivity and decomposition in arboreous ecosys- world, sedimentary organic matter preserved in latest Per- tems. Apart from bacteria, saprophytic fungi represent a mian deposits is characterized by unparalleled abundances of prominent category of decomposers; they are particularly fungal remains, irrespective of depositional environment (ma- efficient in the rapid degradation of woody tissue under rine, lacustrine, fluviatile), floral provinciality, and climatic aerobic conditions. -
Palynology.Pdf
762 Palynology Physical properties of palladium 0.03 to 0.11 in. (0.7 to 3 mm) in length, that live under stones, in caves, and in other moist, dark Property Value places. The elongate body terminates in a slender multisegmented flagellum set with setae. In a curi- Atomic weight 106.4 Naturally occurring isotopes 102 (0.96) ous reversal of function, the pedipalps, the second (percent abundance) pair of head appendages, serve as walking legs. The 104 (10.97) first pair of true legs, longer than the others and set 105 (22.23) 106 (27.33) with sensory setae, has been converted to tactile ap- 108 (26.71) pendages which are vibrated constantly to test the 110 (11.81) substratum. See ARACHNIDA. Willis J. Gertsch Crystal structure Face-centered cubic Thermal neutron capture cross 8.0 section, barns Density at 25 C (77 F), g/cm3 12.01 Melting point, C ( F) 1554 (2829) Palynology Boiling point, C ( F) 2900 (5300) Specific heat at 0 C (32 F), cal/g 0.0584 The study of pollen grains and spores, both extant Thermal conductivity, 0.18 and extinct, as well as other organic microfossils. (cal cm)(cm2 s C) Although the origin of the discipline dates back to Linear coefficient of thermal 11.6 expansion, (µin./in./)/ C the seventeenth century, when modern pollen was Electrical resistivity at 0 C (32 F), 9.93 first examined microscopically, the term palynology µΩ-cm was not coined until 1944. Young’s modulus, lb/in.2, static, at 16.7 106 20 C (68 F) The term palynology is used by both geologists Atomic radius in metal, nm 0.1375 and biologists. -
Non-Pollen Palynomorphs Notes: 2
Non-pollen palynomorphs notes: 2. Holocene record of Megalohypha aqua - dulces , its relation to the fossil form genus Fusiformisporites and association with lignicolous freshwater fungi Lyudmila Shumilovskikh, Astrid Ferrer, Frank Schlütz To cite this version: Lyudmila Shumilovskikh, Astrid Ferrer, Frank Schlütz. Non-pollen palynomorphs notes: 2. Holocene record of Megalohypha aqua - dulces , its relation to the fossil form genus Fusiformisporites and association with lignicolous freshwater fungi. Review of Palaeobotany and Palynology, Elsevier, 2017, 246, pp.167-176. 10.1016/j.revpalbo.2017.07.002. hal-01790616 HAL Id: hal-01790616 https://hal-amu.archives-ouvertes.fr/hal-01790616 Submitted on 14 May 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Review of Palaeobotany and Palynology 246 (2017) 167–176 Contents lists available at ScienceDirect Review of Palaeobotany and Palynology journal homepage: www.elsevier.com/locate/revpalbo Review papers Non-pollen palynomorphs notes: 2. Holocene record of Megalohypha aqua-dulces, its relation to the -
CHAPTER (24): Allied Forensic Specialties CHAPTER (23):PRINCIPLES of FORENSIC SCIENCE Locard’S Exchange Principle: ‘Every Contact Leaves a Trace
• CHAPTER (23):PRINCIPLES OF FORENSIC SCIENCE Lecture 4: • CHAPTER (24): Allied Forensic Specialties CHAPTER (23):PRINCIPLES OF FORENSIC SCIENCE Locard’s exchange principle: ‘every contact leaves a trace. Scene examination : (Aim : to secure, identify and preserve evidence ) - A crime scene is a zone is cordoned off, within which all people accessing or leaving are entered into (and have to sign) a ‘scene log’. - Crime Scene Manager (CSM) is in overall charge of the scene and controls the personnel that assist in the examination . - Scene of Crime Officers (SOCOs) is in charge of evidence gathering - Police Search Advisory (POLSA) staff in charge of ‘fingertips’. If there are human remains at crime scenes, examinations are focused on the - immediate area around the remains so that they can Be removed for a post- mortem examination (why?) à remains are prone to rapid changes, especially during the first few weeks of decomposition. Packaging differ based on the evidence: Evidence recovery : Paper sacks For clothing because, if item is slightly damp, this allows moisture to pass through. 1- Evidence assigned an Plastic bags Used for items such as cigarette ends. exhibit number. 2- Photographed before removed Plastic tubes Used for sharp items such as knives or screwdrivers . 3- Packaged. / known as weapons tubes Cardboard With plastic ties to secure the item in place. boxes Chain of custody: • Once an exhibit has been created, each time it is transferred from one place to another, the details need to be recorded. • Continuity forms, tells that the exhibit has been passed from one person to another. • Once examinations of an exhibit have been concluded, it is retained for a period of time before it is destroyed or, on occasion, returned. -
Application of Palynology to the Study of Tertiary Rocks of the Coastal Plain of Arkansas Eugene L
Journal of the Arkansas Academy of Science Volume 14 Article 9 1960 Application of Palynology to the Study of Tertiary Rocks of the Coastal Plain of Arkansas Eugene L. Jones Arkansas Tech University Follow this and additional works at: http://scholarworks.uark.edu/jaas Part of the Geology Commons, Paleontology Commons, and the Stratigraphy Commons Recommended Citation Jones, Eugene L. (1960) "Application of Palynology to the Study of Tertiary Rocks of the Coastal Plain of Arkansas," Journal of the Arkansas Academy of Science: Vol. 14 , Article 9. Available at: http://scholarworks.uark.edu/jaas/vol14/iss1/9 This article is available for use under the Creative Commons license: Attribution-NoDerivatives 4.0 International (CC BY-ND 4.0). Users are able to read, download, copy, print, distribute, search, link to the full texts of these articles, or use them for any other lawful purpose, without asking prior permission from the publisher or the author. This Article is brought to you for free and open access by ScholarWorks@UARK. It has been accepted for inclusion in Journal of the Arkansas Academy of Science by an authorized editor of ScholarWorks@UARK. For more information, please contact [email protected], [email protected]. Journal of the Arkansas Academy of Science, Vol. 14 [1960], Art. 9 APPLICATION OF PALYNOLOGY TO THE STUDY OF TERTIARY ROCKS OF THE COASTAL PLAINOF ARKANSAS Eugene L. Jones Arkansas Polytechnic College INTRODUCTION Tertiary rocks representing the Eocene series of the Tertiary sys- crop out over large areas of the Coastal Plain in Arkansas . Of Klesser areal extent are rocks of the Paleocene series.