scholarly journals The tadpole of the Narrow-mouthed Frog Microhyla fissipes from Vietnam (Anura: Microhylidae)

Zootaxa ◽  
2008 ◽  
Vol 1675 (1) ◽  
pp. 67
Author(s):  
RALF HENDRIX ◽  
ANNA GAWOR ◽  
MIGUEL VENCES ◽  
THOMAS ZIEGLER
Keyword(s):  
Southeast Asia ◽  
Southern China ◽  
External Morphology ◽  
Type Locality ◽  
Mountain Range ◽  
Malay Peninsula ◽  
The North ◽  
Central Vietnam

Based on recent mtDNA analyses, Microhyla fissipes Boulenger was removed from the synonymy  with M. ornata (Duméril & Bibron) by Matsui et al. (2005),where previously it had been placed by Parker (1934). M. fissipes inhabits southern China (type locality: Taiwan) and large parts of Southeast Asia, including the north-ern Malay Peninsula (Matsui et al. 2005). As a contribution to future comprehensive revisions of larval mor-phology of Microhyla Tschudi, we here provide a detailed description of external morphology of reliably identified tadpoles recently collected from the Truong Son mountain range, central Vietnam.

The ‘Indianization’ of Southeast Asia: Reflections on the Historical Sources

1977 ◽  
Vol 8 (2) ◽  
pp. 143-161 ◽  
Author(s):  
I. W. Mabbett
Keyword(s):  
Southeast Asia ◽  
Historical Record ◽  
Convincing Evidence ◽  
Second Century ◽  
Malay Peninsula ◽  
Indian Languages ◽  
Historical Sources ◽  
Indian Culture ◽  
The North ◽  
Influence Spread

From about the second century onwards, principalities (“empires” is probably the wrong word in all the earlier cases) began to appear in Southeast Asia, first along the isthmus of the Malay Peninsula, round the coast of the Gulf of Siam and of the southern part of Vietnam, later in the archipelago and eventually spreading throughout the area now known as Southeast Asia except for the north of Vietnam and parts of the archipelago in the east. These principalities are assigned to the historical record by inscriptions using Indian languages and scripts, stone remains attesting Hindu and Buddhist cults, and foreign accounts, mostly Chinese, indicating various features of Indian culture. Two of the questions which underlie historical studies of this evidence are: how did Indian influence spread through Southeast Asia? and, how far did Indian influence dominate Southeast Asia? In principle, these questions may be answered independently of each other, the first being chiefly concerned with the “Indianization I” discussed in an earlier article, the second with “Indianization II”. Attention will be directed here chiefly to the first, and to the second primarily only to the extent that is entailed by examination of the first. Various conflicting views have been advanced by historians; the purpose here is to suggest that, in the absence of convincing evidence for any one of them, an eclectic interpretation is not only legitimate but cogent.

V. Britain and the Siamese Malay States, 1892–1904: a Comment

1972 ◽  
Vol 15 (3) ◽  
pp. 471-492
Author(s):  
J. Chandran
Keyword(s):  
Southeast Asia ◽  
Critical Analysis ◽  
Considerable Extent ◽  
The Other ◽  
Political Control ◽  
Malay Peninsula ◽  
The North ◽  
Form Part ◽  
History Of ◽  
Basic Facts

THIS is an attempt to provide a broad and critical analysis of British policy towards the Siamese Malay States which lay to the north of the British possessions and protectorates in the Malay Peninsula. Four of them, Perlis, Kedah, Kelantan and Trengganu, were transferred to British suzerainty in 1909 and now form part of Malaysia. The period under examination was one of unusually keen rivalry between Britain and France in the whole of mainland Southeast Asia and one of its unique features was the preservation of the independence of the Kingdom of Siam. Apart from the other needs of imperialism, the policies of die two Powers in Siam were to a considerable extent influenced by the presence of their vast colonial possessions in the periphery of Siam. These basic facts of the history of the region have, not unnaturally, led to a variety of approaches to the problem of the extension of British political control in the Malay Peninsula.

An annotated checklist of mesoplodont whale species (Cetacea, Ziphiidae) discovered during the nineteenth century

2015 ◽  
Vol 42 (2) ◽  
pp. 226-235 ◽  
Author(s):  
G. N. H. Waller
Keyword(s):  
Nineteenth Century ◽  
Additional Data ◽  
Original Description ◽  
Type Specimen ◽  
External Morphology ◽  
Type Locality ◽  
Type Material ◽  
Beaked Whale ◽  
Registration Number ◽  
Annotated Checklist

Eight species of mesoplodont whales (genus Mesoplodon Gervais, 1850) named during the nineteenth century are based on valid descriptions. A checklist with the original description and type material for each of these species is provided. Additional data given may include type locality and illustrative sources, type material holding institution and type registration number(s). The only type specimen for which a record of external morphology was published relates to the 1803 stranding of Sowerby's beaked whale (Mesoplodon bidens).

New data on the tribe Ducetiini from Vietnam (Orthoptera: Tettigoniidae: Phaneropterinae)

2010 ◽  
Vol 19 (1) ◽  
pp. 29-34
Author(s):  
A.V. Gorochov
Keyword(s):  
Systematic Position ◽  
Type Locality ◽  
Northern Vietnam ◽  
Central Vietnam ◽  
Erroneous Data

Prohimerta (Anisotima) laocai sp. nov. from Northern Vietnam and Paraducetia cruciata gialai subsp. nov. from Central Vietnam are described. Corrected are some erroneous data on systematic position of Prohimerta (Anisotima) vieta, P. (Prohimerta) maculosa, and Paraducetia cruciata, as well as those on the type locality of P. maculosa.

Centroceras gasparrinii subsp. minor subsp. nov. (Ceramiaceae, Rhodophyta) in the North Adriatic Sea (Mediterranean): molecular and morphological characterization

Phytotaxa ◽  
2019 ◽  
Vol 415 (4) ◽  
pp. 233-239
Author(s):  
MARION A. WOLF ◽  
ALESSANDRO BUOSI ◽  
ABDUL-SALAM F. JUHMANI ◽  
ADRIANO SFRISO
Keyword(s):  
Morphological Characterization ◽  
Type Locality ◽  
Correct Identification ◽  
Cortical Cells ◽  
Western Atlantic ◽  
Gland Cells ◽  
The North ◽  
Red Algal ◽  
Long Time ◽  
The 19Th Century

Centroceras Kützing is a small red algal genus with 18 currently accepted species (Guiry & Guiry 2019), characterized by simple filamentous thalli with erect axes arising from a prostrate system and di-trichotomous branching (Hommersand 1963). The characters used to distinguish species are primarily cortical filament morphology: shape and number of the acropetal cortical cells, shape of gland cells, and shape of spines (Won et al. 2009). The generitype C. clavulatum (C. Agardh) Montagne has been viewed for a long time as a highly variable and cosmopolitan species (Hommersand 1963). Molecular and detailed morphological analyses brought Barros-Barreto et al. (2006) to report that C. clavulatum may consist of a species complex and Won et al. (2009) confirmed this hypothesis identifying eight taxonomic entities phylogenetically segregated from genuine C. clavulatum. Seven of these entities were assigned to the following species: C. gasparrinii (Meneghini) Kützing, C. hommersandii Won, T.O. Cho & Fredericq, C. hyalacanthum Kützing, C. micracanthum Kützing, C. natalensis Won, T.O. Cho & Fredericq, C. rodmanii Won, T.O. Cho & Fredericq, and C. tetrachotomum Won, T.O. Cho & Fredericq, (Won et al. 2009). Centroceras gasparrinii, C. hyalacanthum, and C. micracanthum are three western Atlantic species listed as synonyms of C. clavulatum since the middle of the 19th century and resurrected from the ‘C. clavulatum complex’ by Won et al. (2009). In particular, two of these taxa were described from specimens of the Mediterranean Sea: C. gasparrinii (as Ceramium gasparrinii Meneghini, type locality Palermo, Italy) and C. micracanthum (reported with the synonym Centroceras leptacanthum Kützing, type locality Genoa, Italy). Therefore, the numerous Mediterranean records of C. clavulatum (e.g., Gómez Garreta et al. 2001; Verlaque 2001; Sfriso & Curiel 2007; Taşkýn et al. 2013) most probably belong to one of these two species and have to be re-examined for a correct identification and to understand the spatial distribution of the different taxa (Tsiamis et al. 2010). For this reason, in the last years in Greece (Tsiamis et al. 2010), Spain (Gallardo et al. 2016) and Morocco (Hassoun et al. 2018) accurate sampling and morphological analyses of specimens previously identified as C. clavulatum were conducted to determine their correct taxonomic identities. In all cases the recognized species was C. gasparrinii, which can be distinguished morphologically from the other ones previously known as C. clavulatum by the presence of ovoid gland cells and ovoid terminal acropetal cortical cells (Won et al. 2009). As reported by Tsiamis et al. (2010), Greek samples differed from those described by Won et al. (2009), in the smaller number of periaxial cells (10–12 against 13–19).

In the Service of World Revolution: Vietnamese Communists’ Radical Ambitions through the Three Indochina Wars

2019 ◽  
Vol 21 (4) ◽  
pp. 4-30
Author(s):  
Tuong Vu
Keyword(s):  
Cold War ◽  
Southeast Asia ◽  
Local Politics ◽  
International System ◽  
The North ◽  
Local Actors ◽  
The 1950S

The terms “decolonization” and “Cold War” refer to specific processes and periods in the international system, but they do not capture the full agency of local actors such as Vietnamese Communists. Based on recently available archival materials from Hanoi, this article maps those terms onto Vietnamese Communist thinking through four specific cases. The declassified materials underscore the North Vietnamese leaders’ deep commitment to a radical worldview and their occasional willingness to challenge Moscow and Beijing for leadership of world revolution. The article illuminates the connections (or lack thereof) between global, regional, and local politics and offers a more nuanced picture of how decolonization in Southeast Asia in the 1950s–1980s sparked not only a Cold War confrontation but also a regional war.

scholarly journals Human Impacts on Estuarine Erosion-Deposition in Southern Central Vietnam: Observation and Hydrodynamic Simulation

2021 ◽  
Vol 13 (15) ◽  
pp. 8303
Author(s):  
Vu Tuan Anh ◽  
Pham Ba Trung ◽  
Kim-Anh Nguyen ◽  
Yuei-An Liou ◽  
Minh-Thu Phan
Keyword(s):  
Deposition Process ◽  
Southwest Monsoon ◽  
North Coast ◽  
Northeast Monsoon ◽  
Southern Coast ◽  
Erosion Processes ◽  
The North ◽  
Central Vietnam ◽  
Southern Central ◽  
Deposition Processes

This paper aims to identify the causes and sources of erosion and deposition at small estuaries in southern central Vietnam under human intervention. The jetty built at the Tam Quan river mouth (Binh Dinh Province, Vietnam) serves as the base for the study. After its completion at the end of 2009, the hydrodynamic and erosion-deposition processes in the region have been significantly altered. Inside the estuary, the waves are not influenced, but the currents are increased during the ebb tide period and decreased during the flood tide timeframe. During the southwest monsoon, the jetty could cause an increase in the deposition process in both frequency and area, whereas the erosion process tends to narrow the area and increase the frequency on the north coast. In contrast, both deposition and erosion processes are increased on the southern coast. About 5859 m3 of sediments are deposited in the channel gate mainly by local sources. During the northeast monsoon, both deposition and erosion processes are located over a narrow area with frequency increased on the north coast, whereas the deposition process is narrowed with higher frequency on the southern coast. The total amount of sediment deposited at the estuary is 56,446 m3, of which 74.2% is from the onsite erosion material, 15.8% from the river and 10% from the longshore transportation. Generally, due to mainly erosion-deposition processes, sediment volume is accumulated during the northeast monsoon with amount 9.6 times more than that the southwest monsoon. The erosion-deposition processes are contributed to by poor practical management and local human activities inland and in the coastal regions, as well as the natural situation, resulting in serious impacts on society, the economy and the environment. Hence, the governance of the erosion-deposition processes and sediment load in small estuaries appear to contribute to the master plan for the local sustainable development of society and the economy.

Trends and Variability of North American Cool-Season Extratropical Cyclones: 1979–2019

2021 ◽  
Author(s):  
Robert Fritzen ◽  
Victoria Lang ◽  
Vittorio A. Gensini
Keyword(s):  
North American ◽  
Research Question ◽  
Weather Conditions ◽  
Extratropical Cyclones ◽  
Mountain Range ◽  
Cool Season ◽  
The North ◽  
Primary Driver ◽  
Regional Reanalysis ◽  
Log Linear

AbstractExtratropical cyclones are the primary driver of sensible weather conditions across the mid-latitudes of North America, often generating various types of precipitation, gusty non-convective winds, and severe convective storms throughout portions of the annual cycle. Given ongoing modifications of the zonal atmospheric thermal gradient due to anthropogenic forcing, analyzing the historical characteristics of these systems presents an important research question. Using the North American Regional Reanalysis, boreal cool-season (October–April) extratropical cyclones for the period 1979–2019 were identified, tracked, and classified based on their genesis location. Additionally, bomb cyclones—extratropical cyclones that recorded a latitude normalized pressure fall of 24 hPa in 24-hr—were identified and stratified for additional analysis. Cyclone lifespan across the domain exhibits a log-linear relationship, with 99% of all cyclones tracked lasting less than 8 days. On average, ≈ 270 cyclones were tracked across the analysis domain per year, with an average of ≈ 18 year−1 being classified as bomb cyclones. The average number of cyclones in the analysis domain has decreased in the last 20 years from 290 year−1 during the period 1979–1999 to 250 year−1 during the period 2000–2019. Spatially, decreasing trends in the frequency of cyclone track counts were noted across a majority of the analysis domain, with the most significant decreases found in Canada’s Northwest Territories, Colorado, and east of the Graah mountain range. No significant interannual or spatial trends were noted with bomb cyclone frequency.

The Invasion of Plague in Early Modern Italy

2019 ◽  
pp. 23-50
Author(s):  
John Henderson
Keyword(s):  
Early Modern ◽  
Preventive Measures ◽  
Northern Italy ◽  
Reggio Emilia ◽  
Health Board ◽  
Mountain Range ◽  
Physical Barrier ◽  
The North ◽  
Early Modern Italy ◽  
The Dead

This chapter discusses the origins and spread of plague in northern Italy. Plague arrived in Italy in 1629 with French and German troops. It is no accident that the initial cases of plague identified in October of 1629 were first in Piedmont in the Val di Susa, west of Turin and near the border with France, and secondly in the Valtellina in Lombardy, subsequently travelling to Lake Como to the north of Milan. Other cities in northern Italy soon became infected and on May 6, 1630, the authorities as far south as Bologna announced the official outbreak of plague. Judging by the rapidity with which plague spread between these northern urban centres, one would have expected the epidemic to have arrived in Tuscany by early May, given that Bologna is only 65 miles north of Florence, but it was delayed by both natural and man-made factors. Tuscany is separated from Reggio-Emilia by the Apennine mountain range, which provided a physical barrier and facilitated the control of traffic coming from the north. The chapter then traces the preventive measures adopted by the health board as the plague approached Tuscany, including cordons sanitaires along frontiers, the removal of the sick to quarantine centres, and the rapid burial of the dead.

scholarly journals Temporal and Spatial Heterogeneity of PM2.5 Related to Meteorological and Socioeconomic Factors across China during 2000–2018

2022 ◽  
Vol 19 (2) ◽  
pp. 707
Author(s):  
Xiangxue Zhang ◽  
Changxiu Cheng
Keyword(s):  
Socioeconomic Factors ◽  
Southern China ◽  
Yangtze River Delta ◽  
Socioeconomic Factor ◽  
Factors Affecting ◽  
The North ◽  
The Status ◽  
Risk Areas ◽  
Future Direction ◽  
Q Values

In recent years, air pollution caused by PM2.5 in China has become increasingly severe. This study applied a Bayesian space–time hierarchy model to reveal the spatiotemporal heterogeneity of the PM2.5 concentrations in China. In addition, the relationship between meteorological and socioeconomic factors and their interaction with PM2.5 during 2000–2018 was investigated based on the GeoDetector model. Results suggested that the concentration of PM2.5 across China first increased and then decreased between 2000 and 2018. Geographically, the North China Plain and the Yangtze River Delta were high PM2.5 pollution areas, while Northeast and Southwest China are regarded as low-risk areas for PM2.5 pollution. Meanwhile, in Northern and Southern China, the population density was the most important socioeconomic factor affecting PM2.5 with q values of 0.62 and 0.66, respectively; the main meteorological factors affecting PM2.5 were air temperature and vapor pressure, with q values of 0.64 and 0.68, respectively. These results are conducive to our in-depth understanding of the status of PM2.5 pollution in China and provide an important reference for the future direction of PM2.5 pollution control.

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