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This paper aims to compile an exhaustive list of the behavioral patterns exhibited by the chimpanzees of the Mahale Mountains National Park, Tanzania. The compilation is based on the glossary compiled by Goodall (1989), but a substantial numbers of new terms have been added. Thus, we list 316 simple anatomical terms, 81 complex anatomical terms, 37 simple functional terms, and 81 complex functional terms, in addition to 116 synonyms. The behavioral patterns are divided into eight categories on the basis of degree of universality: (1) commonly seen in both Homo and two species of Pan, (1?) commonly seen in Homo and only one species of Pan, (2) patterns common to the genus Pan but not to Homo, (3) patterns common to the chimpanzee Pan troglodytes but not the bonobo Pan paniscus, (4) patterns common to eastern (P.t. schweinfurthii) and central (P.t. troglodytes) but not western (P.t. vents) chimpanzees, (5) patterns unique to the eastern chimpanzees, P.t. schweinfurthii, (6) patterns unique to the population of Mahale, (7) patterns unique to many individuals (at least most members of an age/sex class) of M group chimpanzees, (8) patterns limited to a single (idiosyncrasy) or a few individuals of M group. It is most likely that the behavior patterns of the last common ancestor of Homo and Pan are found in Categories 1 and I? and less likely in Categories 2 and 3. It is possible that behavior patterns belonging to Categories 5, 6 or 7 are cultures.
During the 1930s through the 1940s and into the 1950s, Spanish and German presentations in opposition to ardent nationalism share strikingly common aesthetic and ideological strategies supporting claims to a transnational, international space. Specific examples of common geography, identity and language in German and Spanish presentations (theater, short stories, reports, essays, speeches and poetry) in Spain and Latin America by German (Regler, Renn, Uhse), Spanish (J. Bergamin, R. Alberti, M. Aub) and Latin American (D. Rivera, P. Neruda, C. Vallejo) intellectuals, artists and activists during the 1930s through the 1950s will be explored. For example, German-speaking audiences and artists in Spain and Mexico shared a common lived and aesthetic space as Spanish-speaking audiences and artists. Further, many German presentations were translated into Spanish and visa versa. Here, presentations in “Das Wort” and “El Mono Azul” in Spain as well as “Freies Deutschland/Alemania libre” in Mexico will be referenced in developing a sense of re-definition of the concept of ‘foreign’ and ‘commonness’ beyond simply nationality (tradition, history and geography) and language. The impetus for an alternative, international and even revolutionary ‘space’ (as defined by Henri Lefebvre in The Production of Space) was produced in and through common Spanish and German strategies and realizations in their presentations. This Spanish-German example from the early/mid-part of the 20th century is a significant contribution to contemporary interdisciplinary discussions in the 21st century.
The shape of the facial carina in Altastreplia is discussed. Although taxonomically useful, the protrudent form probably occurs by convergence in different species groups. Two species groups in which the carina is usually produced are revised. The belljamini species group includes: belljamini Lima (from southeastern Brazil), gigantea Stone (from Panama), magna, n. sp. (from Colombia and Venezuela), and superj1ua Stone (from Panama). Host data for this group are limited to only one record of benjamilli from a species of Pouteria (Sapotaceae). The pallidipennis complex, which is included in the pseudoparallela species group, is recognized to include: amnis Stone (from southern Brazil and possibly Trinidad), curitis Stone (from Colombia, Peru, and northern Brazil), pallida, n. sp. (from Panama), pallidipennis Greene (from Colombia and Venezuela), and vele::i, n. sp. (from Colombia). These species breed in fruit of Passij10ra (Passifloraceae) (P. ambigua Hems., ligularis Juss., Idtida H.B.K., quadrallgularis L., and seemannii Griseb.). The relationships of these Anastrepliaspecies are discussed, and diagnoses and ill ustrations are provided to permit their identification. A neotype is designated for A. consobrina (Loew), and the identity of this species is clarified.
Extremely short verbs can be found in various Genn::.,nic languages and dialects; the sterns of these verbs do not have a fInal consonant «C-)C-V), and they always have a monosyllabic infinitive and usually monosyllabic fInite forms as weIl. Examples for these 'kinds of short verbs are Swiss Gennan hä 'to have', gö 'to go', g~ 'to give', n~ 'to take' which correspond to the Swedish verbs ha, gä, ge and tao The last example shows that such short verb formations also occur with verbs having (nearly) identical meanings but which do not share the same etymology. Apart from their shortness, these verbs are characterized by a high degree of irregularity, often even by suppletion, which sometimes develops contrary to regular sound laws. Furthermore they are among the most-used verbs and often tend towards grammaticalization. The present paper compares the short verbs of seven Germanic languages; in addition, it describes their various ways of development and strategies of differentiation. Moreover, it examines the question of why some languages and dialects (e.g. Swiss German, Frisian, Swedish, Norwegian) have many short verbs while others (New High German, Icelandic, Faroese) only have few, the paper discusses the contribution of short verbs to questions concerning linguistic change and the morphological organization of languages.
In order to understand the specific structures and features of the German surnames the most important facts about their emergence and history should be outlined and, at the same time, be compared with the Swedish surnames because there are considerable differences (for further details cf. Nubling 1997 a, b). First of all, surnames in Germany emerged rather early, with the first instances occurring in the 11th century in southern Germany; by the 16th century surnames were common all over Germany. Differences are related to geography (from south to north), social class (from the upper to the lower classes) und urban versus rural areas.
German linking elements are sometimes classified as inflectional affixes, sometimes as derivational affixes, and in any case as morphological units with at least seven realisations (e.g. -s-, -es-, -(e)n-, -e-). This article seeks to show that linking elements are hybrid elements situated between morphology and phonology. On the one hand, they have a clear morphological status since they occur only within compounds (and before a very small set of suffixes) and support the listener in decoding them. On the other hand, they also have to be analysed on the phonological level, as will be shown in this article. Thus, they are marginal morphological units on the pathway to phonology (including prosodics). Although some alloforms can sometimes be considered former inflectional endings and in some cases even continue to demonstrate some inflectional behaviour (such as relatedness to gender and inflection class), they are on their way to becoming markers of ill-formed phonological words. In fact, linking elements, above all the linking -s-, which is extremely productive, help the listener decode compounds containing a bad phonological word as their first constituent, such as Geburt+s+tag ‘birthday’ or Religion+s+unterricht ‘religious education’. By marking the end of a first constituent that differs from an unmarked monopedal phonological word, the linking element aids the listener in correctly decoding and analysing the compound. German compounds are known for their length and complexity, both of which have increased over time—along with the occurrence of linking elements, especially -s-. Thus, a profound instance of language change can be observed in contemporary German, one indicating its typological shift from syllable language to word language.
The (mis)management of rapport amongst groups in Niger Delta (ND) communities has become a significant issue, which Ahmed Yerima's Hard Ground (HG) depicts as having the capacity to aid or control the conflicts in the region. Linguistic studies on Yerima's drama from the perspective of pragmatics have tended to use pragmatic acts to identify the discourse value of proverbs and functions of characters' utterances but have not accounted for the politeness strategies utilised for rapport management, especially in conflict situations. This article, drawing on a rapport management model of politeness and aspects of speech act discourse, identifies the face, sociality rights, and interactional goals that characterise the conflict-motivated dialogues sampled in HG, and reveals the rapport management (RM) strategies through which these are managed in the text. Three conflict situations can be observed as prompting different RM strategies: cause-effect identification (CEI), militancy support (MSP), and disagreement (DSG) situations. CEI is marked by incriminating (involving eliciting and informing acts) and exonerating (including complimenting and acknowledging acts) strategies; MSP is indexed by strategies of persuasion (realised with face-enhancing/threatening acts), whereas DSG is typified by requesting (featuring explicit head acts and alerters) and blaming strategies (including insulting and threatening, aggravating moves). Generally, the requesting, blaming, and exonerating strategies are largely used by the ND youth in HG to probe, threaten, or disagree on specific issues, while the incriminating and persuasion strategies are mainly employed by the women to indict, influence, and predict future actions. The study of RM in the conflict situations depicted in the play sheds light on the often neglected cause of conflicts in contemporary Africa.
The subfamily Epiphloeinae is defined to include fourteen genera as follows: Epiphloeus Spinola; Pilosirus, new genus; Plocamocera Spinola; Iontoclerus, new genus; Arenaria, new genus; Ichnea Laporte; Diapromeces, new genus; Pyticeroides Kuwert; Ellipotoma Spinola; J{atamyurus, new genus; Megatrachys, new genus; Madoniella Pic; Hapsidopteris, new genus; and Teutonia, new genus. The following type-species are described: Pilosirus brunoi, new species; Arenaria chiapas, new species; Diapromeces aclydis, new species; Katamyurus paxillus, new species; Megatrachys paniculus, new species; Hapsidopteris diastenus, new species; and Teutonia nova, new species. Elloplium humerale Klug is designated as the typespecies of Iontoclerus. The genus Madolliella is removed from the subfamily Korynetinae andis declared a senior synonym of Phlogistosternus Wolcott. Neiclmea is synonymized with Pyticeroides. This treatise includes a key to the genera of Epiphloeinae, descriptions of the genera and new type-species, and distribution map for each genus.
A three-dimensional gridded climatology of carbon monoxide (CO) has been developed by trajectory mapping of global MOZAIC-IAGOS in situ measurements from commercial aircraft data. CO measurements made during aircraft ascent and descent, comprising nearly 41 200 profiles at 148 airports worldwide from December 2001 to December 2012 are used. Forward and backward trajectories are calculated from meteorological reanalysis data in order to map the CO measurements to other locations, and so to fill in the spatial domain. This domain-filling technique employs 15 800 000 calculated trajectories to map otherwise sparse MOZAIC-IAGOS data into a quasi-global field. The resulting trajectory-mapped CO dataset is archived monthly from 2001–2012 on a grid of 5° longitude × 5° latitude × 1 km altitude, from the surface to 14 km altitude.
The mapping product has been carefully evaluated, by comparing maps constructed using only forward trajectories and using only backward trajectories. The two methods show similar global CO distribution patterns. The magnitude of their differences is most commonly 10 % or less, and found to be less than 30 % for almost all cases. The trajectory-mapped CO dataset has also been validated by comparison profiles for individual airports with those produced by the mapping method when data from that site are excluded. While there are larger differences below 2 km, the two methods agree very well between 2 and 10 km with the magnitude of biases within 20 %.
Maps are also compared with Version 6 data from the Measurements Of Pollution In The Troposphere (MOPITT) satellite instrument. While agreement is good in the lowermost troposphere, the MOPITT CO profile shows negative biases of ∼ 20 % between 500 and 300 hPa. These upper troposphere biases are not related to the
mapping procedure, as almost identical differences are found with the original in situ MOZAIC-IAGOS data. The total CO trajectory-mapped MOZAIC-IAGOS climatology column agrees with the MOPITT CO total column within ±5 %, which is consistent with previous reports.
The maps clearly show major regional CO sources such as biomass burning in the central and southern Africa and anthropogenic emissions in eastern China. The dataset shows the seasonal CO cycle over different latitude bands and altitude ranges that are representative of the regions as well as long-term trends over latitude bands. We observe a decline in CO over the Northern Hemisphere extratropics and the tropics consistent with that reported by previous studies.
Similar maps have been made using the concurrent O3 measurements by MOZAICIAGOS, as the global variation of O3–CO correlations can be a useful tool for the evaluation of ozone sources and transport in chemical transport models. We anticipate use of the trajectory-mapped MOZAIC-IAGOS CO dataset as an a priori climatology for satellite retrieval, and for air quality model validation and initialization.
A three-dimensional gridded climatology of carbon monoxide (CO) has been developed by trajectory mapping of global MOZAIC-IAGOS in situ measurements from commercial aircraft data. CO measurements made during aircraft ascent and descent, comprising nearly 41 200 profiles at 148 airports worldwide from December 2001 to December 2012, are used. Forward and backward trajectories are calculated from meteorological reanalysis data in order to map the CO measurements to other locations and so to fill in the spatial domain. This domain-filling technique employs 15 800 000 calculated trajectories to map otherwise sparse MOZAIC-IAGOS data into a quasi-global field. The resulting trajectory-mapped CO data set is archived monthly from 2001 to 2012 on a grid of 5° longitude × 5° latitude × 1 km altitude, from the surface to 14 km altitude.
The mapping product has been carefully evaluated, firstly by comparing maps constructed using only forward trajectories and using only backward trajectories. The two methods show similar global CO distribution patterns. The magnitude of their differences is most commonly 10 % or less and found to be less than 30 % for almost all cases. Secondly, the method has been validated by comparing profiles for individual airports with those produced by the mapping method when data from that site are excluded. While there are larger differences below 2 km, the two methods agree very well between 2 and 10 km with the magnitude of biases within 20 %. Finally, the mapping product is compared with global MOZAIC-IAGOS cruise-level data, which were not included in the trajectory-mapped data set, and with independent data from the NOAA aircraft flask sampling program. The trajectory-mapped MOZAIC-IAGOS CO values show generally good agreement with both independent data sets.
Maps are also compared with version 6 data from the Measurements Of Pollution In The Troposphere (MOPITT) satellite instrument. Both data sets clearly show major regional CO sources such as biomass burning in Central and southern Africa and anthropogenic emissions in eastern China. While the maps show similar features and patterns, and relative biases are small in the lowermost troposphere, we find differences of ∼ 20 % in CO volume mixing ratios between 500 and 300 hPa. These upper-tropospheric biases are not related to the mapping procedure, as almost identical differences are found with the original in situ MOZAIC-IAGOS data. The total CO trajectory-mapped MOZAIC-IAGOS column is also higher than the MOPITT CO total column by 12–16 %.
The data set shows the seasonal CO cycle over different latitude bands and altitude ranges as well as long-term trends over different latitude bands. We observe a decline in CO over the northern hemispheric extratropics and the tropics consistent with that reported by previous studies using other data sources.
We anticipate use of the trajectory-mapped MOZAIC-IAGOS CO data set as an a priori climatology for satellite retrieval and for air quality model validation and initialization.
Intrinsic motivation, the causal mechanism for spontaneous exploration and curiosity, is a central concept in developmental psychology. It has been argued to be a crucial mechanism for open-ended cognitive development in humans, and as such has gathered a growing interest from developmental roboticists in the recent years. The goal of this paper is threefold. First, it provides a synthesis of the different approaches of intrinsic motivation in psychology. Second, by interpreting these approaches in a computational reinforcement learning framework, we argue that they are not operational and even sometimes inconsistent. Third, we set the ground for a systematic operational study of intrinsic motivation by presenting a formal typology of possible computational approaches. This typology is partly based on existing computational models, but also presents new ways of conceptualizing intrinsic motivation. We argue that this kind of computational typology might be useful for opening new avenues for research both in psychology and developmental robotics.
Background: The interferon-inducible immunity-related GTPases (IRG proteins/p47 GTPases) are a distinctive family of GTPases that function as powerful cell-autonomous resistance factors. The IRG protein, Irga6 (IIGP1), participates in the disruption of the vacuolar membrane surrounding the intracellular parasite, Toxoplasma gondii, through which it communicates with its cellular hosts. Some aspects of the protein's behaviour have suggested a dynamin-like molecular mode of action, in that the energy released by GTP hydrolysis is transduced into mechanical work that results in deformation and ultimately rupture of the vacuolar membrane. Results: Irga6 forms GTP-dependent oligomers in vitro and thereby activates hydrolysis of the GTP substrate. In this study we define the catalytic G-domain interface by mutagenesis and present a structural model, of how GTP hydrolysis is activated in Irga6 complexes, based on the substrate-twinning reaction mechanism of the signal recognition particle (SRP) and its receptor (SRalpha). In conformity with this model, we show that the bound nucleotide is part of the catalytic interface and that the 3'hydroxyl of the GTP ribose bound to each subunit is essential for trans-activation of hydrolysis of the GTP bound to the other subunit. We show that both positive and negative regulatory interactions between IRG proteins occur via the catalytic interface. Furthermore, mutations that disrupt the catalytic interface also prevent Irga6 from accumulating on the parasitophorous vacuole membrane of T. gondii, showing that GTP-dependent Irga6 activation is an essential component of the resistance mechanism. Conclusions: The catalytic interface of Irga6 defined in the present experiments can probably be used as a paradigm for the nucleotide-dependent interactions of all members of the large family of IRG GTPases, both activating and regulatory. Understanding the activation mechanism of Irga6 will help to explain the mechanism by which IRG proteins exercise their resistance function. We find no support from sequence or G-domain structure for the idea that IRG proteins and the SRP GTPases have a common phylogenetic origin. It therefore seems probable, if surprising, that the substrate-assisted catalytic mechanism has been independently evolved in the two protein families.
A new family (Macronicophilidae) is established for Macronicophilus Silvestri, 1909, currently placed in Geophilidae. Seven new species of Neotropical Geophilomorpha are described: Ilyphilus saudus n.sp. and I. sensibilis n.sp. (Baliophilidae), Hyphydrophilus projeclUs n.sp. and Ribautia onycophaena n.sp. (Geophilidae), Macronicophilus abbrevialus n.sp., M. unguiseta n.sp. and M. venezolanus n.sp. (Macronicophilidae). The hitherto unknown male of Schendylops marchantariae (PEREIRA, MINELLI & BARBIERI, 1995) is described and two species (Pectiniunguis geayi (BROLEMANN & RIBAUT, 1911) and Ityphilus calinus CHAMBERLIN, 1957 are redescribed from the type and new material. A key to the species of Macronicophilus is provided.
A new genus is proposed within the family Geophilidae: Hyphydrophilus n. gen., for H. adisi n.sp. Four additional new species are described, i.e. the ballophilids ltyphilus crabilli n.sp. and Taeniolinllm arborum n.sp. and the schendylids Pecfiniunguis ascendens n.sp. and Schendyluflls amazonicl/s n.sp. The geophilid species Ribautia centralis (SILVESTRI, 1907) is redescribed, after material from Brazil compared with the holotype. The ballophilid Thalthybil/s perrieri BROLEMANN, 1909 is transferred to the genus ltyphi/us COOK, 1889 and a lectotype is designated here for it.
In AD 79 the town of Herculaneum was suddenly hit and overwhelmed by volcanic ash-avalanches that killed all its remaining residents, as also occurred in Pompeii and other settlements as far as 20 kilometers from Vesuvius. New investigations on the victims' skeletons unearthed from the ash deposit filling 12 waterfront chambers have now revealed widespread preservation of atypical red and black mineral residues encrusting the bones, which also impregnate the ash filling the intracranial cavity and the ash-bed encasing the skeletons. Here we show the unique detection of large amounts of iron and iron oxides from such residues, as revealed by inductively coupled plasma mass spectrometry and Raman microspectroscopy, thought to be the final products of heme iron upon thermal decomposition. The extraordinarily rare preservation of significant putative evidence of hemoprotein thermal degradation from the eruption victims strongly suggests the rapid vaporization of body fluids and soft tissues of people at death due to exposure to extreme heat.
The classifications of the Hystricomorpha in English text-books of Zoology are based upon the one proposed by Alston in 1876 (P.Z.S. 1876, pp. 90-97), which was itself an amplification and in some particulars a modification of the arrangement suggested by Waterhouse in 1848. Alston added to the group the family Dinomyidae, which, following Peters, he placed between the Dasyproctidae and Caviidae; and the Otenodactylinae, which he ranked as a subfamily of Octodontidae. He also transferred Petromys from the Echymyina (Echinomyinae), where it was placed by Waterhouse, to the Octodontinae. ...