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Journal articles on the topic 'Lardeer'

Author: Grafiati

Published: 4 June 2021

Last updated: 5 February 2022

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1

Rodríguez, Rafael L., Robb C. Kolodziej, and Gerlinde Höbel. "Memory of prey larders in golden orb-web spiders, Nephila clavipes (Araneae: Nephilidae)." Behaviour 150, no. 12 (2013): 1345–56. http://dx.doi.org/10.1163/1568539x-00003099.

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Nephila clavipes spiders accumulate prey larders on their webs. We conducted a field experiment to ask if the spiders search for larders that have been pilfered (experimentally mimicking the potential effect of kleptoparasites), and to ask if the spiders vary their search efforts according to the size of the larder. All spiders searched for larders removed from their web, and spiders that lost larger larders (i.e., consisting of more prey items) searched for longer intervals. We thus suggest that N. clavipes form memories of the size of the larders they have accumulated, and that they use those memories to regulate recovery efforts when the larders are pilfered. The content of those memories may include discrete prey counts or the accumulation of a continuous variable correlated with counts, such as the total mass of captured prey. We discuss the adaptive significance of this ability in the framework of costs related to kleptoparasites and the ecology of food hoarding.

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2

Kissack, Gardner. "Recommended: Ring Lardner." English Journal 74, no. 1 (1985): 81. http://dx.doi.org/10.2307/816520.

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3

Goheen, Jacob R., and Robert K. Swihart. "Food-hoarding behavior of gray squirrels and North American red squirrels in the central hardwoods region: implications for forest regeneration." Canadian Journal of Zoology 81, no. 9 (2003): 1636–39. http://dx.doi.org/10.1139/z03-143.

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The North American red squirrel (Tamiasciurus hudsonicus) has expanded its geographic range into the state of Indiana concurrently with a decline in populations of gray squirrels (Sciurus carolinensis) throughout portions of the central hardwoods region of the United States that have been converted to intensive agriculture. Red squirrels construct larder hoards and function as seed predators throughout much of their geographic range. In contrast, gray squirrels construct scatter hoards and thus function as seed dispersers in addition to eating seeds. We conducted field observations to discern whether hoarding behavior differed between the two species in a deciduous forest stand near the southern limit of the range of red squirrels. Red squirrels were more likely to hoard walnuts and acorns in larders or trees, whereas gray squirrels were more likely to scatter-hoard mast items. We present a simple model to illustrate the potential impact of interspecific differences in hoarding on germination success of black walnut. Our results suggest that red squirrels are unable to compensate completely for the loss of gray squirrels as seed dispersers in portions of the central hardwoods region that have been transformed by agriculture.

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4

Petrick, Gabriella M. "Larding the Larder." Senses and Society 5, no. 3 (2010): 382–87. http://dx.doi.org/10.2752/174589210x12753842356160.

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5

Kalliokoski, J. "The Pontiac problem, Quebec–Ontario, in the light of gravity data." Canadian Journal of Earth Sciences 24, no. 9 (1987): 1916–19. http://dx.doi.org/10.1139/e87-181.

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A belt of Archean quartzose metasedimentary gneisses with minor mafic volcanic rocks (the Pontiac Group) lies south of the Blake River and older Archean mafic volcanic rocks of the Abitibi Greenstone Belt, and is separated from them by the Larder Lake – Cadillac Break. To the west of the Pontiac Group, on strike, is the Archean Larder Lake Group of turbidite conglomerate, argillite, limestone, and iron formation with abundant mafic flows and intrusions. These strata also lie south of the Larder Lake – Cadillac Break and south of the Blake River and older Archean mafic volcanic rocks. The western contact between the Pontiac and Larder Lake groups is covered by a narrow north–south strip of Proterozoic Cobalt sedimentary rocks. On the basis of gravity work that compares the Bouguer gravity anomaly gradient across the Cadillac Break with that across the west margin of the Pontiac Group, it is proposed that the Larder Lake and Pontiac groups are separated by a north–south fault and that the Pontiac Group represents a lithologically distinct uplifted block. The Pontiac block may be an Archean terrane.

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6

Harrison, S. L. "Field, F.P.A. & Lardner." American Journalism 14, no. 3-4 (1997): 520–29. http://dx.doi.org/10.1080/08821127.1997.10731939.

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7

Zhang, Hongmao, Haiyang Gao, Zheng Yang, Zhenzhen Wang, Yang Luo, and Zhibin Zhang. "Effects of interspecific competition on food hoarding and pilferage in two sympatric rodents." Behaviour 151, no. 11 (2014): 1579–96. http://dx.doi.org/10.1163/1568539x-00003201.

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Food hoarding and pilferage in rodents may be regulated by intense competition between sympatric species that have similar habitats, diets and activity, but studies exploring this remain rare. Here, we used semi-natural enclosures to investigate food-hoarding and cache pilferage interactions between sympatric Korean field mice (KFM) (Apodemus peninsulae) and Chinese white-bellied rats (CWR) (Niviventer confucianus). KFM and CWR have similar diets, habitat and nocturnal activity, but the smaller KFM larder and scatter hoards and larger CWR larder hoard only. We found that KFM harvest, larder-hoard and eat seeds at a greater intensity when CWR are present as an audience (present but cannot pilfer). KFM ate 11.5%, re-larder-hoarded 17.9% and re-scatter-hoarded 1.3% of their scatter-hoarded seeds, and ate 29.3% of their larder-hoarded seeds when CWR were present as pilferers. A total of 12.8% of the seeds scatter-hoarded and 50% of seeds directly put on the ground by KFM were pilfered by CWR. CWR did not alter hoarding intensity in the presence of KFM and their stores cannot be pilfered by KFM. These results indicate that large-sized rodent species (more dominant) significantly increase the hoarding intensity of small-sized species and show a unidirectional pilferage of seeds cached by small-sized species. The behavioural differences between these two species may reduce competition for resources and promote coexistence between sympatric rodents.

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8

Gullason, Thomas A., Douglas Robinson, and Ellen Gardiner. "Ring Lardner and the Other." American Literature 65, no. 4 (1993): 810. http://dx.doi.org/10.2307/2927321.

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9

James, Martin. "Edwin (Ted) Lardner: an appreciation." Powder Metallurgy 47, no. 3 (2004): 234. http://dx.doi.org/10.1179/pom.2004.47.3.234.

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10

Zhang, Hongmao, and Yu Wang. "Differences in hoarding behavior between captive and wild sympatric rodent species." Current Zoology 57, no. 6 (2011): 725–30. http://dx.doi.org/10.1093/czoolo/57.6.725.

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Abstract In hand reared birds and mammals, it is generally considered that the development of hoarding behavior is the result of an interaction between the development and maturation of the nervous system and learning from individual experience. However, few studies have been done on wild animals. We tested differences in hoarding behavior between captive reared and wild individuals of two sympatric small rodents, Korean field mice Apodemus peninsulae and Chinese white-bellied rats Niviventer confucianus. Our aim was to identify if lack of experience from the wild would result in poorly developed hoarding behavior. The Korean field mice perform scatterand larder-hoarding behaviors whereas Chinese white-bellied rats hoard food in larders only. Within outdoor enclosures we compared seed-hoarding behavior in reared juveniles (RJ, 40-50 d old, pregnant mothers were captured in the wild), wild juveniles (WJ, as young as the RJ) and wild adults (WA, over-winter animals). We found that a lack of experience from the wild had significant effects on seed-hoarding behavior for both species. The RJ-group removed and hoarded fewer seeds than the WJand WA-groups. The two latter groups hoarded seeds in a similar way. In the Korean filed mouse the RJ-group placed more seeds on the ground surface than other groups. These findings suggest that wild experience is important for the acquisition of an appropriate food-hoarding behavior (especially for scatter-hoarding) in these species.

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11

Smith, Moira T., and George E. Gehrels. "Structural geology of the Lardeau Group near Trout Lake, British Columbia: implications for the structural evolution of the Kootenay Arc." Canadian Journal of Earth Sciences 29, no. 6 (1992): 1305–19. http://dx.doi.org/10.1139/e92-104.

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The Lardeau Group is a heterogeneous assemblage of lower Paleozoic eugeoclinal strata present in the Kootenay Arc in southeastern British Columbia. It is in fault contact with lower Paleozoic miogeoclinal strata for all or some of its length along a structure termed the Lardeau shear zone. The Lardeau Group was deformed prior to mid-Mississippian time, as manifested by layer-parallel faults, folds, and evidence for early greenschist-facies metamorphism. Regional constraints indicate probable Devono-Mississippian timing of orogeny, and possible juxtaposition of the Lardeau Group over miogeoclinal strata along the Lardeau shear zone at this time. Further ductile deformation during the Middle Jurassic Columbian orogeny produced large folds with subhorizontal axes, northwest-striking foliation and faults, and orogen-parallel stretching lineations. This deformation was apparently not everywhere synchronous, and may have continued through Late Jurassic time northeast of Trout Lake. This was followed by Cretaceous(?) dextral strike-slip and normal movement on the Lardeau shear zone and other parallel faults. While apparently the locus of several episodes of faulting, the Lardeau shear zone does not record the accretion of far-travelled tectonic fragments, as sedimentological evidence ties the Lardeau Group and other outboard units to the craton.

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12

Ferré, John P. "The Lost Journalism of Ring Lardner." American Journalism 34, no. 2 (2017): 242–44. http://dx.doi.org/10.1080/08821127.2017.1309236.

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13

Garner, Lynne. "What we find in nature's larder." Child Care 15, no. 7 (2018): 6–7. http://dx.doi.org/10.12968/chca.2018.15.7.6.

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14

Sharma, Aditya, Mayora Varshney, Weon Cheol Lim, et al. "Mechanistic insights on the electronic properties and electronic/atomic structure aspects in orthorhombic SrVO3 thin films: XANES–EXAFS study." Physical Chemistry Chemical Physics 19, no. 9 (2017): 6397–405. http://dx.doi.org/10.1039/c6cp08301c.

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15

Smith, Moira T., and George E. Gehrels. "Stratigraphic comparison of the Lardeau and Covada groups: implications for revision of stratigraphic relations in the Kootenay Arc." Canadian Journal of Earth Sciences 29, no. 6 (1992): 1320–29. http://dx.doi.org/10.1139/e92-105.

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The Lardeau Group is a heterogeneous assemblage of lower Paleozoic, outer continental margin strata present in the Kootenay Arc in southeastern British Columbia. From east to west, structurally lowest to highest, and what has been previously interpreted as stratigraphically lowest to highest, it consists of green and grey phyllite, argillite, limestone, and rare pillow flows (Index Formation); siliceous argillite and phyllite (Triune Formation); grey massive quartzite (Ajax Formation); siliceous argillite and phyllite (Sharon Creek Formation); alkalic(?) pillow basalt, breccia, and tuff (Jowett Formation); and quartzo-feldspathic wacke and phyllite (Broadview Formation).We propose a correlation between the Lardeau Group and the Covada Group and Bradeen Hill assemblage, both in north eastern Washington. The latter contain the same stratigraphic elements, in the same structural order, as those of the Lardeau Group. These include, from east to west, black and grey argillite and slate, chert, chert–quartz sandstone, limestone, and rare tuff, pillow flows, and quartz arenite (Bradeen Hill assemblage); alkalic(?) pillow basalt, breccia, tuff, and limestone (Butcher Mountain Formation); and quartzo-feldspathic wacke and slate (Daisy Formation). However, the sense of facing, and hence the stratigraphie sequence in the Covada Group and Bradeen Hill assemblage, is reversed in relation to the Lardeau Group, with the quartzo-feldspathic wacke unit the oldest and slate and argillite the youngest. Because the degree of preservation (and consequently the evidence for facing and age) of the units in northeastern Washington is superior to that of the Lardeau Group, we suggest that (1) the Lardeau Group may be inverted relative to the sequence as originally defined; (2)the Lardeau Group may range from Late Cambrian (Broadview Formation) to Devonian (Index Formation) in age; and (3)further work is warranted to test this hypothesis. This correlation unites lower Paleozoic stratigraphic units along several hundred kilometres of the ancient continental margin.

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16

Wilkinson, Lori, Alexander R. Cruden, and Thomas E. Krogh. "Timing and kinematics of post-Timiskaming deformation within the Larder Lake - Cadillac deformation zone, southwest Abitibi greenstone belt, Ontario, Canada." Canadian Journal of Earth Sciences 36, no. 4 (1999): 627–47. http://dx.doi.org/10.1139/e99-015.

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The Larder Lake - Cadillac deformation zone is one of several anastomosing zones of high strain within the Abitibi greenstone belt. In the Kirkland Lake area, Ontario, the Larder Lake - Cadillac deformation zone is characterized by extensive carbonate and chlorite alteration, strong south-dipping foliations, and steep lineations. These features formed during two ductile deformation increments, D2 and D3, that occurred after deposition of Timiskaming assemblage sediments. D2 strain accumulation and greenschist facies metamorphism and alteration were localized within the deformation zone, facilitated by channelling of hydrothermal fluids within a preexisting structure, possibly formed during early D1 terrane accretion. During D2 north-south shortening, east-west-trending sectors of the deformation zone accumulated bulk coaxial strains, while southeast- and northeast-trending sectors experienced, respectively, dextral and sinistral transpressive deformations. Preservation of Timiskaming assemblage sediments in the footwall of the deformation zone indicates a component of south-over-north (reverse) displacement that is not recorded by D2 fabrics. Northwest-southeast D3 compression resulted in the formation of a regional, northeast-striking cleavage formed under regional greenschist facies conditions, and local dextral reactivation of suitably oriented sections of the Larder Lake - Cadillac deformation zone. The Murdoch Creek and Lebel stocks abut the Larder Lake - Cadillac deformation zone. Their internal structure and emplacement are interpreted to be a consequence of D2 north-south shortening. Magmatic zircon and titanite in the Murdoch Creek and Lebel stocks yield U-Pb geochronology ages of 2672 ± 2 and 2673 ± 2 Ma, providing a maximum age for D2 deformation. Hydrothermal titantite associated with S3 foliation in the Murdoch Creek stock gives an U-Pb age of 2665 ± 4 Ma, the maximum age of D3 deformation. Pluton emplacement, deformation, and coincident metamorphism occurred over a span of 1 Ma (from 2670 to 2669 Ma) to over 14 Ma (from 2675 to 2661 Ma), during a regime of north-south, followed by northwest-southeast, regional shortening.

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17

Lankevich, George J., and Ellen D. Langill. "Foley & Lardner: Attorneys at Law, 1842-1992." Journal of American History 81, no. 1 (1994): 275. http://dx.doi.org/10.2307/2081064.

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18

Powell, W. G., C. J. Hodgson, J. A. Hanes, D. M. Carmichael, S. Mcbride, and E. Farrar. "40Ar/39Ar geochronological evidence for multiple postmetamorphic hydrothermal events focused along faults in the southern Abitibi greenstone belt." Canadian Journal of Earth Sciences 32, no. 6 (1995): 768–86. http://dx.doi.org/10.1139/e95-066.

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Thermal histories in the Abitibi and Pontiac subprovinces vary for three general domains: (1) zones of impermeable rock with cooling rates of >8 °C/Ma; (2) zones of impermeable rock that are spatially associated with monzogranite plutons, with apparent cooling rates of 1–2 °C/Ma; and (3) permeable high-strain zones with apparent cooling rates of <l °C/Ma. Evidence for multiple hydrothermal events in fault zones includes (1) most age spectra having a disturbed form; (2) concave-down spectra for samples from subgreenschist-facies faults, indicating multiple episodes of white mica growth; (3) Cr-muscovite from a greenschist-facies segment of the Larder Lake–Cadillac fault yielding a plateau age of 2543 ± 8 Ma, postdating regional metamorphism by 120 Ma; (4) two discrete ages for postmetamorphic amphibole from the Larder Lake–Cadillac fault (2578 ± 10, 2421 ± 15 Ma); and (5) two discrete dates for white mica (2414 ± 9, >2594 Ma) from the volcanogenic massive sulphide-related sericite alteration, with the coarser mica yielding the younger date. Based on radiometric dating, impermeable rocks were affected weakly by postmetamorphic hydrothermal events. Minerals in zones of higher permeability were reset during the intrusion of monzogranite plutons. Highly permeable zones, such as the Larder Lake–Cadillac and Porcupine–Destor faults, were overprinted repeatedly. This produces a drawn-out series of dates from minerals with varying closure temperatures. Radiometric ages from fault zones, or ore deposits, cannot be used to interpret the cooling history and evolution of the Abitibi belt as a whole.

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19

Shirai, Yasuhiro. "The Aspect Hypothesis, the comparative fallacy and the validity of obligatory context analysis: a reply to Lardiere, 2003." Second Language Research 23, no. 1 (2007): 51–64. http://dx.doi.org/10.1177/0267658307071602.

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Lardiere (2003), in her reply to Lakshmanan and Selinker (2001), justifies the use of suppliance in obligatory contexts as a method of analysis in the investigation of the second language (L2) acquisition of past tense, and claims that such a method is characteristic of previous studies that have proposed the Aspect Hypothesis. It is argued here that this is a misrepresentation of research on the Aspect Hypothesis which, contra Lardiere, takes seriously the problem of the ‘comparative fallacy’ and the autonomous nature of interlanguage. Lardiere also argues that the Aspect Hypothesis studies suffer from a different kind of comparative fallacy, to which I reply by discussing the importance of refining methods of analysis in verb aspectual classification of learner data.

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20

McGaw, Judith A. "Food for Thought in Philadelphia: "The Larder Invaded"." Technology and Culture 29, no. 2 (1988): 266. http://dx.doi.org/10.2307/3105526.

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21

Staudohar, Paul D. "Baseball short stories: From Lardner to Asinof to Kinsella." Culture, Sport, Society 3, no. 2 (2000): 44–55. http://dx.doi.org/10.1080/14610980008721869.

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22

Gerhardt, Fritz. "FOOD PILFERING IN LARDER-HOARDING RED SQUIRRELS (TAMIASCIURUS HUDSONICUS)." Journal of Mammalogy 86, no. 1 (2005): 108–14. http://dx.doi.org/10.1644/1545-1542(2005)086<0108:fpilrs>2.0.co;2.

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23

Meredith, Jill. "The Wedding Feast: Frans Snyders's Larder with a Maidservant." Gastronomica 3, no. 3 (2003): 10–12. http://dx.doi.org/10.1525/gfc.2003.3.3.10.

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24

Sherratt, Andrew, and J. Clutton-Brock. "The Walking Larder: Patterns of Domestication, Pastoralism, and Predation." Man 24, no. 4 (1989): 685. http://dx.doi.org/10.2307/2804296.

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25

Smith, A. F. "The Larder: Food Studies Methods from the American South." Journal of American History 101, no. 4 (2015): 1231–32. http://dx.doi.org/10.1093/jahist/jav145.

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26

Wang, Zhenyu, Bo Wang, Xianfeng Yi, Chuan Yan, Lin Cao, and Zhibin Zhang. "Scatter-hoarding rodents are better pilferers than larder-hoarders." Animal Behaviour 141 (July 2018): 151–59. http://dx.doi.org/10.1016/j.anbehav.2018.05.017.

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27

Murphy, Paul V. "Midwesterners Swallow the World: Lardner, Shirer, Terkel, and American Journalism." Middle West Review 4, no. 1 (2017): 193–98. http://dx.doi.org/10.1353/mwr.2017.0080.

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28

Limón-Priego, Yensen, Ismael Everardo Bárcenas-Patiño, Edgard Iván Benítez-Guerrero, Guillermo Gilberto Molero-Castillo, and Alejandro Velazquez-Mena. "Mu-Calculus Satisfiability with Arithmetic Constraints." Proceedings of the Institute for System Programming of the RAS 33, no. 2 (2021): 191–200. http://dx.doi.org/10.15514/ispras-2021-33(2)-12.

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The propositional modal μ-calculus is a well-known specification language for labeled transition systems. In this work, we study an extension of this logic with converse modalities and Presburger arithmetic constraints, interpreted over tree models. We describe a satisfiability algorithm based on breadth-first construction of Fischer-Lardner models. An implementation together several experiments are also reported. Furthermore, we also describe an application of the algorithm to solve static analysis problems over semi-structured data.

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29

Donald, Jenna L., and Stan Boutin. "Intraspecific cache pilferage by larder-hoarding red squirrels (Tamiasciurus hudsonicus)." Journal of Mammalogy 92, no. 5 (2011): 1013–20. http://dx.doi.org/10.1644/10-mamm-a-340.1.

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30

Matheny, Gaverick, and Kai M. A. Chan. "Human Diets and Animal Welfare: the Illogic of the Larder." Journal of Agricultural and Environmental Ethics 18, no. 6 (2005): 579–94. http://dx.doi.org/10.1007/s10806-005-1805-x.

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31

Charabidze, D., T. Colard, A. Becart, and V. Hedouin. "Use of larder beetles (Coleoptera: Dermestidae) to deflesh human jaws." Forensic Science International 234 (January 2014): 162–64. http://dx.doi.org/10.1016/j.forsciint.2013.10.041.

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32

Dillon, Mike. "Book Review: Ron Rapoport, ed., The Lost Journalism of Ring Lardner." Newspaper Research Journal 39, no. 2 (2018): 245–46. http://dx.doi.org/10.1177/0739532918775700.

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33

Kupfer, Charles A. "Ring Lardner's You Know Me Al: Up from Popularity." Prospects 30 (October 2005): 487–504. http://dx.doi.org/10.1017/s0361233300002143.

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Ring Lardner's position in American literature suffers more from the praise he gains than the criticism he receives. His reputation as an acerbic journalist, mordant satirist, master dialectician, and popular sportswriter still draws clouds of suspicion across the minds of highbrow critics weighing his stature as a serious writer.Lardner himself did nothing to debunk the notion that he was at heart a pulp author, never tearing away from his journalistic roots as did other authors who started their careers in the newspaper business. It may have been comfort with his preferred environment, or a reverse snobbery, but Lardner always disdained self-conscious artfulness, instead preening his image as a wordsmith and copy-slave. Max Perkins, his Scribner's editor, noted this self-defined lowbrow posture: “He always thought of himself as a newspaperman, anyhow. He had a sort of provincial scorn for literary people.”Provincial scorn notwithstanding, Lardner was a prominent member of Perkins's stable. Contemporaries at Scribner's included Thomas Wolfe, Ernest Hemingway, and F. Scott Fitzgerald. Perkins, a literary talent scout with a knack for coaxing maximum output from mercurial writers, devoted ample time and attention to cultivating Lardner's work. Few writers of any stripe could boast more lustrous friends and colleagues, and, in his lifetime, Lardner's proper place in the American literary pantheon was accorded with scant complaint. It was only after his death in 1933 that the diminishing process began.

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34

Cartwright, Caroline R. "Grapes or raisins? An early Bronze Age larder under the microscope." Antiquity 77, no. 296 (2003): 345–48. http://dx.doi.org/10.1017/s0003598x00092322.

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The sudden conflagration of an Early Bronze Age room at Tell es-Sa'idiyeh in the Jordan valley resulted in the preservation of a remarkable assemblage of plant remains. Using microscopy and experiment, the author was able to detect fruits previously sun dried for preservation. Grapes, figs, pomegranate, olives, cereals, legumes and capers provided the most conclusive evidence for the drying and preservation of food.

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35

SOMANATHAN, Hema, Subhash MALI, and Renee M. BORGES. "Arboreal larder-hoarding in the tropical Indian giant squirrel Ratufa indica." Ecoscience 14, no. 2 (2007): 165–69. http://dx.doi.org/10.2980/1195-6860(2007)14[165:alitti]2.0.co;2.

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36

Moro, Alfredo. "Extraños compañeros de viaje: Cervantes y Mary Shelley." Anales Cervantinos 49 (November 21, 2017): 325. http://dx.doi.org/10.3989/anacervantinos.2017.013.

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Miguel de Cervantes y Mary Shelley parecen, a priori, dos extraños compañeros de viaje. Pese a las evidentes divergencias entre la narrativa de ambos autores, la autora inglesa mostró un notable interés por la vida y obra de Miguel de Cervantes a lo largo de toda su carrera. Este artículo pretende ofrecer un retrato preciso de los intereses cervantinos de la autora de Frankenstein, rastreando con este fin la correspondencia personal de la autora inglesa, su producción narrativa, y finalmente, su contribución al cervantismo: la Life of Cervantes (1837) que Shelley publicaría en la Cabinet Cyclopaedia de Dyonisius Lardner.

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37

Dryer, Christy. "An interview with nursing education champion and national compliance expert Greg Lardner." Teaching and Learning in Nursing 16, no. 1 (2021): A1—A2. http://dx.doi.org/10.1016/j.teln.2020.10.003.

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38

Muroya, Akiko. "L1 Transfer in L2 Acquisition of English Verbal Morphology by Japanese Young Instructed Learners." Languages 4, no. 1 (2018): 1. http://dx.doi.org/10.3390/languages4010001.

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Inflectional morphology has been considered as a particularly difficult area in second language (L2) acquisition (Lardiere 2008; Slabakova 2008). This paper reports on an empirical study investigating the L2 acquisition of English verbal morphology by Japanese young instructed learners. The aim of this study is to explore how the first language (L1) plays a role in the L2 acquisition of inflectional morphology, by applying the Feature Reassembly Hypothesis (FRH, Lardiere 2008, 2009) to a Japanese−English pairing. An elicited production task was administered to Japanese junior high school aged 12–15 (n = 102) and university students aged 19–20 (n = 30). The results show a difference with respect to accuracy rates and error types from previous L2 English studies, in terms of tense−aspect morphology. The findings provide evidence for the FRH’s prediction that attributes morphological variability to L1−L2 contrasts in reassembly of feature matrices for morpholexical items.

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39

Corfu, F., S. L. Jackson, and R. H. Sutcliffe. "U–Pb ages and tectonic significance of late Archean alkalic magmatism and nonmarine sedimentation: Timiskaming Group, southern Abitibi belt, Ontario." Canadian Journal of Earth Sciences 28, no. 4 (1991): 489–503. http://dx.doi.org/10.1139/e91-043.

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The paper presents U–Pb ages for zircons of the calc-alkalic to alkalic igneous suite and associated alluvial–fluvial sedimentary rocks of the Timiskaming Group in the late Archean Abitibi greenstone belt, Superior Province. The Timiskaming Group rests unconformably on pre-2700 Ma komatiitic to calc-alkalic volcanic sequences and is the expression of the latest stages of magmatism and tectonism that shaped the greenstone belt. An age of 2685 ± 3 Ma for the Bidgood quartz porphyry, an age of about 2685–2682 Ma for a quartz–feldspar porphyry clast in a conglomerate, and ages ranging from 2686 to 2680 Ma for detrital zircons in sandstones appear to reflect an early stage in the development of the Timiskaming Group. The youngest detrital zircons in each of three sandstones at Timmins, Kirkland Lake, and south of Larder Lake define maximum ages of sedimentation at about 2679 Ma; the latter sandstone is cut by a porphyry dyke dated by titanite at [Formula: see text], identical to the 2677 ± 2 Ma age for a volcanic agglomerate of the Bear Lake Formation north of Larder Lake. Similar ages have previously been reported for syenitic to granitic plutons of the region. The dominant period of Timiskaming sedimentation and magmatism was thus 2680–2677 Ma. Xenocrystic zircons found in a porphyry and a lamprophyre dyke have ages of 2750–2720 Ma, which correspond to the ages of the oldest units in the belt, predating the volumetrically dominant ca. 2700 Ma greenstone sequences. The presence of these xenocrysts and the onlapping of the Timiskaming Group on all earlier lithotectonic units of the southern Abitibi belt support the concept that the 2700 Ma ensimatic sequences were thrust onto older assemblages during a phase of compression that culminated with the generation of tonalite and granodiorite at about 2695–2688 Ma. Published geochemical data for the Timiskaming igneous suite, notably the enrichments in large-ion lithophile elements and light rare-earth elements and the relative depletion of Nb, Ta, and Ti compare with the characteristics of suites at modern convergent settings such as the Eolian and the Banda arcs and are consistent with generation of the melts from deep metasomatized mantle in the final stages of, or after cessation of, subduction. Late- and post-Timiskaming compression caused north-directed thrusting and folding. Turbiditic sedimentary units of the Larder Lake area which locally structurally overly the alluvial–fluvial sequence and were earlier thought to be part of the Timiskaming Group, appear to be older "flyschoid" sequences, possibly correlative with sedimentary rocks deposited in the Porcupine syncline at Timmins between 2700 and 2690 Ma.

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40

Fitzgerald, John. "Increased Disunity: The Politics and Finance of Guangdong Separatism, 1926–1936." Modern Asian Studies 24, no. 4 (1990): 745–75. http://dx.doi.org/10.1017/s0026749x0001057x.

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There are two lemons in the larder of Modern China's history. Stalin's, dating from April 1927, is certainly the better known:Chiang Kaishek is submitting to discipline. The Kuomintang is a bloc, a sort of revolutionary parliament, with the Right, the Left and the Communists. Why make a coup d'etat? Why drive away the Right when we have the majority and the Right listens to us?… Also, they have connections with the rich merchants and can raise money from them. So they have to be utilized to the end, squeezed out like a lemon, and then flung away.

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41

Bramall, Rebecca. "The austerity larder: Mapping food systems in a new age of austerity." Journal of Consumer Culture 15, no. 2 (2013): 183–201. http://dx.doi.org/10.1177/1469540513493208.

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42

Peterson, Scott D. "Finding the "Real" in 1922: Dixon, Lardner, Broun, and the "Great Cultural Divide"." NINE: A Journal of Baseball History and Culture 26, no. 1-2 (2017): 51–67. http://dx.doi.org/10.1353/nin.2017.0018.

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43

Rosenbloom, Richard S. "Fast Forward: Hollywood, the Japanese, and the Onslaught of the VCR. James Lardner." Isis 78, no. 4 (1987): 624–25. http://dx.doi.org/10.1086/354589.

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44

Lafrance, Bruno. "Geology of the orogenic Cheminis gold deposit along the Larder Lake – Cadillac deformation zone, Ontario." Canadian Journal of Earth Sciences 52, no. 12 (2015): 1093–108. http://dx.doi.org/10.1139/cjes-2015-0067.

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The Larder Lake – Cadillac deformation zone (LLCDZ) is one of two major, auriferous, deformation zones in the southern Abitibi subprovince of the Archean Superior Province. It hosts the Cheminis and the giant Kerr Addison – Chesterville deposits within a strongly deformed band of Fe-rich tholeiitic basalt and komatiite of the Larder Lake Group (ca. 2705 Ma). The latter is bounded on both sides by younger, less deformed, Timiskaming turbidites (2674–2670 Ma). The earliest deformation features are F1 folds affecting the Timiskaming rocks, which formed either during D1 extensional faulting or during early D2 north–south shortening related to the opening and closure, respectively, of the Timiskaming basin. Continued shortening during D2 imbricated the older volcanic rocks and turbidites and produced regional F2 folds with an axial planar S2 cleavage. D2 deformation was partitioned into the weaker band of volcanic rocks, producing the strong S2 foliation, L2 stretching lineation, and south-side-up shear sense indicators, which characterize the LLCDZ. Gold is present in quartz–carbonate veins in deformed fuchsitic komatiites (carbonate ore) and turbiditic sandstone (sandstone-hosted ore), and in association with disseminated pyrite in altered Fe-rich tholeiitic basalts (flow ore). All host rocks underwent strong mass gains in CO2, S, K2O, Ba, As, and W, during sericitization, carbonatization, and sulphidation of the host rocks, suggesting that they interacted with the same hydrothermal fluids. Textural relationships between alteration minerals and S2 cleavage indicate that mineralization is syn-cleavage. Thus, gold was deposited as hydrothermal fluids migrated upward along the LLCDZ during contractional, D2 south-side-up shearing. The gold zones were subsequently modified during D3 reactivation of the LLCDZ as a dextral transcurrent fault zone.

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45

Kurek, P., D. Dobrowolska, B. Wiatrowska, and L. Dylewski. "What if Eurasian jay Garrulus glandarius would larder acorns instead of scatter them?" iForest - Biogeosciences and Forestry 11, no. 5 (2018): 685–89. http://dx.doi.org/10.3832/ifor2793-011.

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46

BOWER, JOHN. "The Walking Larder: Patterns of Domestication, Pastoralism, and Predation. JULIET CLUTTON-BROCK, ed." American Ethnologist 17, no. 4 (1990): 802–3. http://dx.doi.org/10.1525/ae.1990.17.4.02a00160.

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47

Korada, Rajasekhara Rao, and Frans C. Griepink. "Aggregation pheromone compounds of the black larder beetle Dermestes haemorrhoidalis Kuster (Coleoptera: Dermestidae)." Chemoecology 19, no. 3 (2009): 177–84. http://dx.doi.org/10.1007/s00049-009-0020-z.

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48

Sorkin, Adam J. "Politics, Privatism and the Fifties: Ring Lardner Jrs.'s "The Ecstasy of Owen Muir"." Journal of American Culture 8, no. 3 (1985): 59–73. http://dx.doi.org/10.1111/j.1542-734x.1985.0803_59.x.

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49

Bogaard, Amy, Michael Charles, Katheryn C. Twiss, et al. "Private pantries and celebrated surplus: storing and sharing food at Neolithic Çatalhöyük, Central Anatolia." Antiquity 83, no. 321 (2009): 649–68. http://dx.doi.org/10.1017/s0003598x00098896.

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In the Neolithic megasite at Çatalhöyük families lived side by side in conjoined dwellings, like a pueblo. It can be assumed that people were always in and out of each others' houses – in this case via the roof. Social mechanisms were needed to make all this run smoothly, and in a tour-de-force of botanical, faunal and spatial analysis the authors show how it worked. Families stored their own produce of grain, fruit, nuts and condiments in special bins deep inside the house, but displayed the heads and horns of aurochs near the entrance. While the latter had a religious overtone they also remembered feasts, episodes of sharing that mitigated the provocations of a full larder.

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Suhonen, Jukka, Matti Halonen, Tapio Mappes, and Erkki Korpimäki. "Interspecific competition limits larders of pygmy owls Glaucidium passerinum." Journal of Avian Biology 38, no. 5 (2007): 630–34. http://dx.doi.org/10.1111/j.0908-8857.2007.03960.x.

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