A new species of freshwater amphipod, Paracalliope larai, is described, the first description of a species of the genus Paracalliope from Tasmania. P. larai is found in the Dip River, north-western Tasmania. The distribution of the genus in Tasmania is briefly discussed.
{"title":"A new species of freshwater amphipod, Paracalliope larai, (Family Eusiridae) from Tasmania","authors":"B. Knott","doi":"10.26749/rstpp.109.39","DOIUrl":"https://doi.org/10.26749/rstpp.109.39","url":null,"abstract":"A new species of freshwater amphipod, Paracalliope larai, is described, the first description of a species of the genus Paracalliope from Tasmania. P. larai is found in the Dip River, north-western Tasmania. The distribution of the genus in Tasmania is briefly discussed.","PeriodicalId":35513,"journal":{"name":"Papers and Proceedings - Royal Society of Tasmania","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"1975-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69101562","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
A well-exposed middle Late Cambrian to Early Ordovician clastic sequence, herein referred to as the Denison Subgroup, unconformably overlies Middle Cambrian rocks on the Denison Range and is conformably overlain by Ordovician limestone. Four formations are recognized. The basal Singing Creek Formation (720 m) consists of interbedded siltstone, quartzwacke turbidites, siliceous fine conglomerate, and slump sheets, and contains an abundant Franconian trilobite-brachiopod fauna. It grades upwards into the Great Dome Sandstone (510 m), a shallow marine-deltaic-fluvial sequence of crossbedded quartz sandstone, siltstone and fine conglomerate, with a sparse fauna of probable Late Cambrian age. Above this the Reeds Conglomerate (1560 m) comprises largely non-marine pink siliceous conglomerate and cross-bedded sandstone, probably deposited on alluvial fans. This grades into the marine Squirrel Creek Formation, comprising a lower sandstone member (150 m) with worm burrows and gastropods, a siltstone- limestone member (150 m) with an abundant Early Ordovician shelly fauna, and an upper sandstone member (300 m). The Denison Subgroup is approximately equivalent to the pre-limestone part of the Junee Group in the 'original area of Lewis, and to the Owen Conglomerate of western Tasmania.
{"title":"The Late Cambrian to Early Ordovician sequence on the Denison Range, southwest Tasmania","authors":"K. Corbett","doi":"10.26749/rstpp.109.111","DOIUrl":"https://doi.org/10.26749/rstpp.109.111","url":null,"abstract":"A well-exposed middle Late Cambrian to Early Ordovician clastic sequence, herein referred to as the Denison Subgroup, unconformably overlies Middle Cambrian rocks on the Denison Range and is conformably overlain by Ordovician limestone. Four formations are recognized. The basal Singing Creek Formation (720 m) consists of interbedded siltstone, quartzwacke turbidites, siliceous fine conglomerate, and slump sheets, and contains an abundant Franconian trilobite-brachiopod fauna. It grades upwards into the Great Dome Sandstone (510 m), a shallow marine-deltaic-fluvial sequence of crossbedded quartz sandstone, siltstone and fine conglomerate, with a sparse fauna of probable Late Cambrian age. Above this the Reeds Conglomerate (1560 m) comprises largely non-marine pink siliceous conglomerate and cross-bedded sandstone, probably deposited on alluvial fans. This grades into the marine Squirrel Creek Formation, comprising a lower sandstone member (150 m) with worm burrows and gastropods, a siltstone- limestone member (150 m) with an abundant Early Ordovician shelly fauna, and an upper sandstone member (300 m). The Denison Subgroup is approximately equivalent to the pre-limestone part of the Junee Group in the 'original area of Lewis, and to the Owen Conglomerate of western Tasmania.","PeriodicalId":35513,"journal":{"name":"Papers and Proceedings - Royal Society of Tasmania","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"1975-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69101488","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
The relationship between the areas and plant species number of sixteen small islands in a Tasmanian subalpine lake is described. The nature of the island area species diversity curve seems to be strongly affected by island area rather than habitat heterogeneity, and by differences in species diversity in the vegetation zones found on the island.
{"title":"Plant species diversity of the Lake Dora Islands, Tasmania","authors":"J. Kirkpatrick","doi":"10.26749/rstpp.109.33","DOIUrl":"https://doi.org/10.26749/rstpp.109.33","url":null,"abstract":"The relationship between the areas and plant species number of sixteen small islands in a Tasmanian subalpine lake is described. The nature of the island area species diversity curve seems to be strongly affected by island area rather than habitat heterogeneity, and by differences in species diversity in the vegetation zones found on the island.","PeriodicalId":35513,"journal":{"name":"Papers and Proceedings - Royal Society of Tasmania","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"1975-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69101557","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
A new species of freshwater isopod, Heterias petrensis (Family Janiridae, tribe Asellota) is described. The species is found in Lake Crescent, Tasmania. A revised description is given of the genus Heterias.
{"title":"Heterias petrensis, a new species of freshwater isopod from Tasmania (Family Janiridae, Tribe Asellota)","authors":"P. Roberts","doi":"10.26749/rstpp.109.21","DOIUrl":"https://doi.org/10.26749/rstpp.109.21","url":null,"abstract":"A new species of freshwater isopod, Heterias petrensis (Family Janiridae, tribe Asellota) is described. The species is found in Lake Crescent, Tasmania. A revised description is given of the genus Heterias.","PeriodicalId":35513,"journal":{"name":"Papers and Proceedings - Royal Society of Tasmania","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"1975-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69101552","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
The vegetation of the Lagoon Beach area is mapped and described. Classification and ordination of thirty-five randomly located quadrats, and central chi-squared distribution analysis of association between species, reveal three main species/stand groups. The wombat-grazed closed-herbfields dominated by Samolus repens and Schoenus nitens form one strong group associated with the lagoonal flats. A second group consists of stands which include characteristic heath species such as Casuarina monilifera and Hypolaena fastigiata. A third, less well-defined group consists mainly of Eucalyptus viminalis open forests with an understory characteristically dominated by pteridium esculentum. The factors that could be responsible for the differentiation of the vegetation of the area are discussed, and a species list is appended.
{"title":"Phytosociological analysis of the vegetation of Lagoon Beach, Tasmania","authors":"J. Kirkpatrick","doi":"10.26749/rstpp.109.53","DOIUrl":"https://doi.org/10.26749/rstpp.109.53","url":null,"abstract":"The vegetation of the Lagoon Beach area is mapped and described. Classification and ordination of thirty-five randomly located quadrats, and central chi-squared distribution analysis of association between species, reveal three main species/stand groups. The wombat-grazed closed-herbfields dominated by Samolus repens and Schoenus nitens form one strong group associated with the lagoonal flats. A second group consists of stands which include characteristic heath species such as Casuarina monilifera and Hypolaena fastigiata. A third, less well-defined group consists mainly of Eucalyptus viminalis open forests with an understory characteristically dominated by pteridium esculentum. The factors that could be responsible for the differentiation of the vegetation of the area are discussed, and a species list is appended.","PeriodicalId":35513,"journal":{"name":"Papers and Proceedings - Royal Society of Tasmania","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"1975-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69101590","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
An important Late Middle Cambrian fossil locality occurs 2 km west of St. Valentines Peak in north-western Tasmania. The Cambrian rocks to the north and west of St. Valentines Peak are exposed in the core of the north-south trending St. Valentines Peak Anticline. In the best exposed section (3 km north of the main fossil locality), the oldest Cambrian unit is a massive, cherty, pyritic meta-sandstone and meta-siltstone at least 100 m thick. This is overlain by 100 m of rhyolitic welded tuff, 75 to 100 m of meta-sandstones and meta-siltstones, 100 m of a possible contact metasomatic rock and 230 to 375 m of a pale grey chert which in turn is overlain by about 17 m of fine breccia and poorly fossiliferous siltstone. This sequence is overlain with probable disconformity by the basal chert conglomerate of the essentially Ordovician Junee Group. It is suggested that the sediments of the main fossiliferous locality occur stratigraphically below the section noted above. The Cambrian and Ordovician rocks are intruded by Devonian granite and partly overlain by Tertiary basalt.
{"title":"Cambrian stratigraphy of the St. Valentines Peak area, north-western Tasmania","authors":"J. Jago, G. Pike, D. Mills","doi":"10.26749/rstpp.109.85","DOIUrl":"https://doi.org/10.26749/rstpp.109.85","url":null,"abstract":"An important Late Middle Cambrian fossil locality occurs 2 km west of St. Valentines Peak in north-western Tasmania. The Cambrian rocks to the north and west of St. Valentines Peak are exposed in the core of the north-south trending St. Valentines Peak Anticline. In the best exposed section (3 km north of the main fossil locality), the oldest Cambrian unit is a massive, cherty, pyritic meta-sandstone and meta-siltstone at least 100 m thick. This is overlain by 100 m of rhyolitic welded tuff, 75 to 100 m of meta-sandstones and meta-siltstones, 100 m of a possible contact metasomatic rock and 230 to 375 m of a pale grey chert which in turn is overlain by about 17 m of fine breccia and poorly fossiliferous siltstone. This sequence is overlain with probable disconformity by the basal chert conglomerate of the essentially Ordovician Junee Group. It is suggested that the sediments of the main fossiliferous locality occur stratigraphically below the section noted above. The Cambrian and Ordovician rocks are intruded by Devonian granite and partly overlain by Tertiary basalt.","PeriodicalId":35513,"journal":{"name":"Papers and Proceedings - Royal Society of Tasmania","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"1975-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69101602","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
The region of the anterior dorsal fin of the elephant-fish (CalZorhinchus callorhynchus (L.) has been examined by dissection, by injection of radio-opaque material and in serial sections. Particular attention has been paid to the venous system in the region. A large venous sinus lies below the basal plate of the fin skeleton and has connections running anteriorly and posteriorly in the midline. Anteriorly, the sinus is connected with the left posterior cardinal vein by a large communicating vein which lies close against the left side of the vertebral column. This arrangement is generally similar to that found in the Selachii, but in the latter group two venae circulares are found instead of the median dorsal sinus of Callorhinchus and other Holocephali.
{"title":"Some notes on the anterior dorsal fin and venous drainage in Callorhinchus (Holocephali)","authors":"N. Plomley, N. Dilly","doi":"10.26749/rstpp.109.175","DOIUrl":"https://doi.org/10.26749/rstpp.109.175","url":null,"abstract":"The region of the anterior dorsal fin of the elephant-fish (CalZorhinchus callorhynchus (L.) has been examined by dissection, by injection of radio-opaque material and in serial sections. Particular attention has been paid to the venous system in the region. A large venous sinus lies below the basal plate of the fin skeleton and has connections running anteriorly and posteriorly in the midline. Anteriorly, the sinus is connected with the left posterior cardinal vein by a large communicating vein which lies close against the left side of the vertebral column. This arrangement is generally similar to that found in the Selachii, but in the latter group two venae circulares are found instead of the median dorsal sinus of Callorhinchus and other Holocephali.","PeriodicalId":35513,"journal":{"name":"Papers and Proceedings - Royal Society of Tasmania","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"1975-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69101546","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
CARCHARHINIDAE. Carcharhinus greyi greyi, second recorded specimen from Tasmania (first recorded as C. brachyurus); head in plan, mouth parabolic curves, orthogonal polynomials fitted; girth of head an exponential function of length from snout tip; notes on dentition, coloration; key to Tasmanian carcharhinids. SPHYRNIDAE. Sphyrna zygaena, second recorded Tasmanian example, female, compared with first, male; logarithmic lengths to seven morphological landmarks yield a linear graph when plotted on logarithms of seven natural numbers (similar formulations in other sharks). SYNGNATHIDAE. Syngnathus phillipi, study of two samples (meristic and morphometric data, variation within and between samples, supposed sexual dimorphism, pouch, coloration, depth range): Syngnathus caretta (apparently known only from type-specimens) reported from Tasmania; current knowledge of species extended: IchthyocaIlzpus runa noted as a Tasmanian species: Syngnathus poecilolaemus, metrical data. LAMPRIDAE. Lampris regius, new and old local records. SCORPIDAE. Scorpis aequipinnis, morphometry and coloration in a juvenile sample; comparison with adult material, yielding data on regional relative growth. LEPTOSCOPIDAE. Crapatalus arenarius, new subspecies described and figured. TRIPTERYGIIDAE. General review of Tasmanian representatives, with key; Tripterygium clarkei (later placed in Gillias and Norfolkia) here referred to Helcogramma: specimen noted in R.M. Johnston's memoranda, identified as T. clarkei by Whitley, now described as a new species: Gillias macleayana, new material, table of dimensions: two new species of Forsterygion (New Zealand genus new to Australia) described and figured: Brachynectes fasciatus retained in that genus; size classes. ECHENEIDAE. Remora remora, observations on two Tasmanian examples (host, Luth); outline of disc fitted with second degree polynomial; lengths of transverse ridges of disc an exponential function of their serial numbers; unusual white markings in one specimen. SYNANCEJIDAE. Glyptauchen insidiator mirandus, habits; first detailed account of the subspecies; length-number patterns of spines and rays; taxonomic status discussed.
{"title":"Observations on some Tasmanian fishes. Part XXI","authors":"E. Scott","doi":"10.26749/RSTPP.115.101","DOIUrl":"https://doi.org/10.26749/RSTPP.115.101","url":null,"abstract":"CARCHARHINIDAE. Carcharhinus greyi greyi, second recorded specimen from Tasmania (first recorded as C. brachyurus); head in plan, mouth parabolic curves, orthogonal polynomials fitted; girth of head an exponential function of length from snout tip; notes on dentition, coloration; key to Tasmanian carcharhinids. SPHYRNIDAE. Sphyrna zygaena, second recorded Tasmanian example, female, compared with first, male; logarithmic lengths to seven morphological landmarks yield a linear graph when plotted on logarithms of seven natural numbers (similar formulations in other sharks). SYNGNATHIDAE. Syngnathus phillipi, study of two samples (meristic and morphometric data, variation within and between samples, supposed sexual dimorphism, pouch, coloration, depth range): Syngnathus caretta (apparently known only from type-specimens) reported from Tasmania; current knowledge of species extended: IchthyocaIlzpus runa noted as a Tasmanian species: Syngnathus poecilolaemus, metrical data. LAMPRIDAE. Lampris regius, new and old local records. SCORPIDAE. Scorpis aequipinnis, morphometry and coloration in a juvenile sample; comparison with adult material, yielding data on regional relative growth. LEPTOSCOPIDAE. Crapatalus arenarius, new subspecies described and figured. TRIPTERYGIIDAE. General review of Tasmanian representatives, with key; Tripterygium clarkei (later placed in Gillias and Norfolkia) here referred to Helcogramma: specimen noted in R.M. Johnston's memoranda, identified as T. clarkei by Whitley, now described as a new species: Gillias macleayana, new material, table of dimensions: two new species of Forsterygion (New Zealand genus new to Australia) described and figured: Brachynectes fasciatus retained in that genus; size classes. ECHENEIDAE. Remora remora, observations on two Tasmanian examples (host, Luth); outline of disc fitted with second degree polynomial; lengths of transverse ridges of disc an exponential function of their serial numbers; unusual white markings in one specimen. SYNANCEJIDAE. Glyptauchen insidiator mirandus, habits; first detailed account of the subspecies; length-number patterns of spines and rays; taxonomic status discussed.","PeriodicalId":35513,"journal":{"name":"Papers and Proceedings - Royal Society of Tasmania","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"1975-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69101688","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
The sequence of interbedded mudstone, siltstone and very fine sandstone in the Strahan Quadrangle, correlated with the Bell Shale is at least 500 m thick. Two broad associations can be defined. The ratio of very fine sand to mud in the lower association is between 3:2 and 2:3 whereas in the upper association only occasional thin sandstone beds occur. Sedimentary structures such as lenticular bedding, symmetrical ripple marks and the lack of deep water sedimentary features suggest that deposition took place in shallow water. This is supported by palaeontological evidence. Some scouring and upward fining beds suggest that deposition from waning currents occurred sporadically within this environment. The Bell Shale correlate has been folded during two phases. The first phase produced folds plunging between 300 and 900 NW and the second phase produced folds plunging shallowly WNW or ESE. Cleavage was developed only locally during each phase. Folds of both phases produced a primary axial surface cleavage and the second phase produced crenulation cleavage in some areas. The amplitude of folds produced during the first phase decreases towards the centre of the basin. The locus of strain during the second phase of deformation was along the Firewood Siding Fault. The existence and timing of these deformation events demonstrates the uniformity in orientation of Tabberabberan structures throughout north and western Tasmania.
{"title":"Sedimentary and structural features of the Bell shale correlate (Early Devonian), Strahan quadrangle, western Tasmania","authors":"P. Baillie, Pr Williams","doi":"10.26749/rstpp.109.1","DOIUrl":"https://doi.org/10.26749/rstpp.109.1","url":null,"abstract":"The sequence of interbedded mudstone, siltstone and very fine sandstone in the Strahan Quadrangle, correlated with the Bell Shale is at least 500 m thick. Two broad associations can be defined. The ratio of very fine sand to mud in the lower association is between 3:2 and 2:3 whereas in the upper association only occasional thin sandstone beds occur. Sedimentary structures such as lenticular bedding, symmetrical ripple marks and the lack of deep water sedimentary features suggest that deposition took place in shallow water. This is supported by palaeontological evidence. Some scouring and upward fining beds suggest that deposition from waning currents occurred sporadically within this environment. The Bell Shale correlate has been folded during two phases. The first phase produced folds plunging between 300 and 900 NW and the second phase produced folds plunging shallowly WNW or ESE. Cleavage was developed only locally during each phase. Folds of both phases produced a primary axial surface cleavage and the second phase produced crenulation cleavage in some areas. The amplitude of folds produced during the first phase decreases towards the centre of the basin. The locus of strain during the second phase of deformation was along the Firewood Siding Fault. The existence and timing of these deformation events demonstrates the uniformity in orientation of Tabberabberan structures throughout north and western Tasmania.","PeriodicalId":35513,"journal":{"name":"Papers and Proceedings - Royal Society of Tasmania","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"1975-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69101483","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Spartina anglica was introduced into the Tamar Estuary, Tasmania, in 1947. Initially spread was slow but subsequently rapid. It is capable of colonizing all rock types and sediments available in the estuary but fine sediments provide the most and basalt the least suitable substrate. It colonises all available slopes (10 degrees -28 degrees). As a result of the introduction, mud banks become stabilized and the navigable channel thereby safeguarded. The spread of Spartina has, however, adversely affected some beaches and private jetties.
{"title":"The establishment of Spartina in the Tamar Estuary, Tasmania","authors":"A. W. Phillips","doi":"10.26749/rstpp.109.65","DOIUrl":"https://doi.org/10.26749/rstpp.109.65","url":null,"abstract":"Spartina anglica was introduced into the Tamar Estuary, Tasmania, in 1947. Initially spread was slow but subsequently rapid. It is capable of colonizing all rock types and sediments available in the estuary but fine sediments provide the most and basalt the least suitable substrate. It colonises all available slopes (10 degrees -28 degrees). As a result of the introduction, mud banks become stabilized and the navigable channel thereby safeguarded. The spread of Spartina has, however, adversely affected some beaches and private jetties.","PeriodicalId":35513,"journal":{"name":"Papers and Proceedings - Royal Society of Tasmania","volume":null,"pages":null},"PeriodicalIF":0.0,"publicationDate":"1975-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69101594","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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