1,785 research outputs found
RoMEO Studies 4: An analysis of Journal publishers' Copyright Agreements
No full textThis article is the fourth in a series of six emanating from the UK JISC-funded RoMEO Project (Rights Metadata for Open archiving). It describes an analysis of 80 scholarly journal publishers’ copyright agreements with a particular view to their effect on author self-archiving. 90% of agreements asked for copyright transfer and 69% asked for it prior to refereeing the paper. 75% asked authors to warrant that their work had not been previously published although only two explicitly stated that they viewed self-archiving as prior publication. 28.5% of agreements provided authors with no usage rights over their own paper. Although 42.5% allowed self-archiving in some format, there was no consensus on the conditions under which self-archiving could take place. The article concludes that author-publisher copyright agreements should be reconsidered by a working party representing the needs of both partie
A Scalable Architecture for Harvest-Based Digital Libraries - The ODU/Southampton Experiments
No full textThis paper discusses the requirements of current and emerging applications based on the Open Archives Initiative (OAI) and emphasizes the need for a common infrastructure to support them. Inspired by HTTP proxy, cache, gateway and web service concepts, a design for a scalable and reliable infrastructure that aims at satisfying these requirements is presented. Moreover it is shown how various applications can exploit the services included in the proposed infrastructure. The paper concludes by discussing the current status of several prototype implementations
Gentle Harvest of Potatoes in Storage Boxes
No full textRosana G. Moreira, Editor-in-Chief; Texas A&M UniversityThis is a paper from International Commission of Agricultural Engineering (CIGR, Commission Internationale du Genie Rural) E-Journal Volume 7 (2005): Gentle Harvest of Potatoes in Storage Boxes by P. Maly, T. Hoffmann and Ch. Fu
Fallout and Environmental Radionuclides for Estimation of Recent Environmental Changes in Maly Azau Glacier Area (Central Caucasus)
No full text1 .pdf copy (1 Pag.)
of the abstract published by the Organization. © Author(s) 2019. CC Attribution 4.0 license.Over the last decades, glaciers of Central Caucasus are undergoing intensive retreat in response to recent climate
change. Fallout radionuclides (FRN’s) and environmental radionuclides (ERN’s) both are useful instruments in
studies of soils and sediments on glacial landforms that can help to define the direction of the sedimentation
process and relative age of moraines as well as the lithological difference between different landforms.
The study area is situated on the South-Western slope of the Elbrus mountain - between the tongues of Maly Azau
and Bolshoy Azau glaciers near Maly Azau proglacial lake.Peer reviewe
Complete mitochondrial genome of a woolly mammoth (Mammuthus primigenius) from Maly Lyakhovsky Island (New Siberian Islands, Russia) and its phylogenetic assessment
No full textWe present a complete sequence and an annotation of the mitochondrial genome of the woolly mammoth (Mammuthus primigenius) found in 2012 on Maly Lyakhovsky Island (North-Eastern Siberia, Russia). The genome was 16,851 bp long and contained 13 protein-coding, 22 tRNA, and 2 rRNA genes. It was AT reach (61.3%) with A = 32.9%, T = 28.4%, C = 25.3%, and G = 13.4%. © 2018 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group
Thurzova L., Kresanek J., Marecek S. & Mika K. — Maly Atlas Liecivych Rastlin
No full textBarrau Jacques. Thurzova L., Kresanek J., Marecek S. & Mika K. — Maly Atlas Liecivych Rastlin. In: Journal d'agriculture tropicale et de botanique appliquée, vol. 22, n°7-9, Juillet-août-septembre 1975. p. 294
Log-ratio magnitude of <i>a</i> and <i>b</i> for each signatures in BRCA (I) and MALY (II).
No full textLog-ratio magnitude of a and b for each signatures in BRCA (I) and MALY (II).</p
Outburst floods of the Maly Yenisei. Part I
No full text<div><p>ABSTRACT</p><p>The Yenisei, the largest river flowing to the Arctic Ocean, repeatedly hosted cataclysmic floods during the Pleistocene. The largest of the known floods likely originated from palaeolakes in northern Mongolia, at the headwaters of the Little, or Maly, Yenisei. These ancient floods are among the greatest known globally. They left giant gravel dunes and wide abandoned channels in the Kyzyl basin, and high terraces in the gorges upstream. However, few detailed field studies of the flood deposits and no measurements of their ages have been made thus far. The largest palaeolakes were impounded during major glaciations by outlet glaciers from the East Sayan ice field in southern Siberia. The shorelines suggest four distinct palaeolake depths of 290, 175, 145, and 65 m. The timing and location of the glacier impounding the deepest lakes are uncertain but at its maximum, the Tengis outlet glacier was likely capable of impounding the 175 m lake. The dating of glacial deposits in and around the basin reveals that the maximum late Pleistocene glaciers were during Marine Oxygen Isotope Stage (MIS) 3. The ages for deep-lake sediments exposed in the basin behind the dam’s location support this finding. During MIS 2 the Tengis glacier was large enough to impound at least the 145 m lake. However, the existence of a deep MIS 2 palaeolake in the basin has been challenged, because no evidence has been published of MIS 2 lake sediments from the cutbank outcrops and deep drilling cores. Additionally, the end moraines of the Tengis glacier, separated from the deeply eroded lateral moraines by the Maly Yenisei, remain undated; therefore it is uncertain exactly when this glacier crossed the river. This review is part I of a two-part article; Part II presents new age data to constrain the ages of the glacial dam.</p></div
Complete mitochondrial genome of a woolly mammoth (<i>Mammuthus primigenius</i>) from Maly Lyakhovsky Island (New Siberian Islands, Russia) and its phylogenetic assessment
No full textWe present a complete sequence and an annotation of the mitochondrial genome of the woolly mammoth (Mammuthus primigenius) found in 2012 on Maly Lyakhovsky Island (North-Eastern Siberia, Russia). The genome was 16,851 bp long and contained 13 protein-coding, 22 tRNA, and 2 rRNA genes. It was AT reach (61.3%) with A = 32.9%, T = 28.4%, C = 25.3%, and G = 13.4%.</p
Outburst floods of the Maly Yenisei. Part I
No full textThe Yenisei, the largest river flowing to the Arctic Ocean, repeatedly hosted cataclysmic floods during the Pleistocene. The largest of the known floods likely originated from palaeolakes in northern Mongolia, at the headwaters of the Little, or Maly, Yenisei. These ancient floods are among the greatest known globally. They left giant gravel dunes and wide abandoned channels in the Kyzyl basin, and high terraces in the gorges upstream. However, few detailed field studies of the flood deposits and no measurements of their ages have been made thus far. The largest palaeolakes were impounded during major glaciations by outlet glaciers from the East Sayan ice field in southern Siberia. The shorelines suggest four distinct palaeolake depths of 290, 175, 145, and 65 m. The timing and location of the glacier impounding the deepest lakes are uncertain but at its maximum, the Tengis outlet glacier was likely capable of impounding the 175 m lake. The dating of glacial deposits in and around the basin reveals that the maximum late Pleistocene glaciers were during Marine Oxygen Isotope Stage (MIS) 3. The ages for deep-lake sediments exposed in the basin behind the dam’s location support this finding. During MIS 2 the Tengis glacier was large enough to impound at least the 145 m lake. However, the existence of a deep MIS 2 palaeolake in the basin has been challenged, because no evidence has been published of MIS 2 lake sediments from the cutbank outcrops and deep drilling cores. Additionally, the end moraines of the Tengis glacier, separated from the deeply eroded lateral moraines by the Maly Yenisei, remain undated; therefore it is uncertain exactly when this glacier crossed the river. This review is part I of a two-part article; Part II presents new age data to constrain the ages of the glacial dam.</p
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