129,809 research outputs found
Letter from Alvan Coe to James B. Finley
No full textAlvan Coe, Presbyterian missionary, writes to Finley (from Venice on Sandusky Bay?), where he is running an Indian school under the care of the Western Missionary Society of Pittsburgh. The school was originally located in Greenfield. Alexander Clark, one of Coe\u27s scholars, spent time with him last winter, and as he is acquainted with the Ottaways (Ottawa Indians), he was invited to stay and help in Coe\u27s school. Coe is sending Clark to Malvern to get new Ottawa Indian students. He would like the Wyandot children to attend Finley\u27s school. He hopes that what has taken place will cause Finley no hard feelings. Coe ends his letter as follows -- Pray for us. The Wyandots appear civilized compared to these poor creatures. Abstract Number - 689https://digitalcommons.owu.edu/finley-letters/1783/thumbnail.jp
Coe, B K, 2789945
No full textThis record was harvested from a previous catalogue system and will be withdrawn in 2025. Information in this record may be superseded or incomplete. Visit this record in UMA's new catalogue at: https://archives.library.unimelb.edu.au/nodes/view/377859Surname: COE
Given Name(s) or Initials: B K
Military Service Number or Last Known Location: 2789945
Missing, Wounded and Prisoner of War Enquiry Card Index Number: SEA-4540191674
Item: [2016.0049.10155] "Coe, B K, 2789945
Naturalization record of Phillips Coe, Henry
No full textThe naturalization affidavits for Henry Phillips Coe of the Cayman Islands. Signed by Judge Joseph B. Wall
Going Beyond Counting First Authors in Author Co-citation Analysis
No full textThe present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation
counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings
are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that
only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into
account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed
Dispelling the Myths Behind First-author Citation Counts
No full textWe conducted a full-scale evaluative citation analysis study of scholars in the XML research field to explore just how different from each other author rankings resulting from different citation counting methods actually are, and to demonstrate the capability of emerging data and tools on the Web in supporting more realistic citation counting methods. Our results contest some common arguments for the continued
use of first-author citation counts in the evaluation of scholars, such as high correlations between author rankings by first-author citation counts and other citation
counting methods, and high costs of using more realistic citation counting methods that are not well-supported by the ISI databases. It is argued that increasingly available digital full text research papers make it possible for citation analysis studies to go beyond what the ISI databases have directly supported and to employ more
sophisticated methods
Cerebratulus lineolatus Coe 1905
No full text<i>Cerebratulus</i> cf. <i>lineolatus</i> Coe, 1905 <p>(Figure 2 [4])</p> <p> <i>Cerebratulus lineolatus</i> Coe, 1905: 196, pl. 4, fig. 44; Coe, 1940: 275; MacGinitie & MacGinitie, 1949: 163, textfig. 44; Corrêa, 1961: 14; Gibson, 1995: 337.</p> <p> <b>Material examined.</b> One specimen (115 mm, after preservation), MZUSP 0 0 0 13, Brazil, Ceará, Paracuru, Praia da Pedra Rachada, 3°23.95' S 39°0.85' W, under rock, on sand, coll. Cecili Mendes, 28.VIII.2011.</p> <p>One specimen (39 mm, after preservation), MZUSP 0 0 0 14, Brazil, Ceará, Caucaia, Praia do Pacheco, 3°41.11' S 38°37.91' W, under rock, coll. Cecili Mendes, 18.VI.2011.</p> <p>Two specimens (30 mm, 73 mm, after preservation), MZUSP 0 0 0 15, Brazil, Ceará, Paracuru, Pedra Rachada beach, 3°23.95' S 39°0.85' W, under rock, on sand, coll. Cecili Mendes, 20.VIII.2012.</p> <p> <b>Field diagnosis.</b> Body beige, with posterior region reddish due to gonads; dorsal and ventral surfaces completely covered by numerous thin, interrupted, brown lines. Cephalic lobe triangular, narrowing to neck-like constriction. Body long and flat ending in short caudal cirrus; latter lost easily during collection. Cerebral ganglia visible as a reddish region in head. No eye spots evident.</p> <p> <b>Distribution.</b> Western Atlantic: USA (Florida [JLN unpublished obs] and South Carolina [Fox & Ruppert 1985]) and Brazil (Ceará [present study]).</p> <p>Eastern Pacific: California (San Pedro, Newport, San Diego), Mexico (Puerto Refugio, Angel de la Guardia, Punta Willard, Bahia San Luis Gonzaga) (Coe 1940).</p> <p> <b>Ecology.</b> This species is reported from intertidal zone to depths of 70 m (Gibson 1995). They seem to inhabit mud or muddy sand. The specimens here were found on muddy sand under rocks in the lower intertidal zone, sometimes in direct contact with the rock.</p> <p> <b>Remarks.</b> The species was first described from the North Pacific Ocean, along the southwestern coast of North America, and a morphologically identical form has been reported from the south coast of Florida (Corrêa 1961; JLN, unpublished obs). No material is available from the Pacific Coast for comparison. Though the described appearance (Coe 1905; Coe 1940) is convincingly similar, the disjunct geographic and depth distributions provide cause to question the specific identity of the Brazilian (Florida and South Carolina) worms.</p>Published as part of <i>Mendes, Cecili B., Matthews-Cascon, Helena & Norenburg, Jon L., 2016, New records of ribbon worms (Nemertea) from Ceará, Northeast Brazil, pp. 146-156 in Zootaxa 4061 (2)</i> on pages 151-152, DOI: 10.11646/zootaxa.4061.2.4, <a href="http://zenodo.org/record/263586">http://zenodo.org/record/263586</a>
Letter to Marguerite B. Coe regarding award of the Lucile Elliott Scholarship, May 20, 1976
No full textA letter from J. Lamar Woodard to Marguerite B. Coe enclosing Coe\u27s Scholarship funds
Seawater redox variations during the deposition of the Kimmeridge Clay Formation, United Kingdom (Upper Jurassic): evidence from molybdenum isotopes and trace metal ratios
No full textThe Kimmeridge Clay Formation (KCF) and its equivalents worldwide represent one of the most prolonged periods of organic carbon accumulation of the Mesozoic. In this study, we use the molybdenum (Mo) stable isotope system in conjunction with a range of trace metal paleoredox proxies to assess how seawater redox varied both locally and globally during the deposition of the KCF. Facies with lower organic carbon contents (TOC 1–7 wt %) were deposited under mildly reducing (suboxic) conditions, while organic-rich facies (TOC >7 wt %) accumulated under more strongly reducing (anoxic or euxinic) local conditions. Trace metal abundances are closely linked to TOC content, suggesting that the intensity of reducing conditions varied repeatedly during the deposition of the KCF and may have been related to orbitally controlled climate changes. Long-term variations in ?98/95Mo are associated with the formation of organic-rich intervals and are related to third-order fluctuations in relative sea level. Differences in the mean ?98/95Mo composition of the organic-rich intervals suggest that the global distribution of reducing conditions was more extensive during the deposition of the Pectinatites wheatleyensis and lower Pectinatites hudlestoni zones than during the deposition of the upper Pectinatites hudlestoni and Pectinatites pectinatus zones. The global extent of reducing conditions during the Kimmerigidan was greater than today but was less widespread than during the Toarcian (Early Jurassic) oceanic anoxic event. This study also demonstrates that the Mo isotope system in Jurassic seawater responded to changes in redox conditions in a manner consistent with its behavior in present-day sedimentary environment
Letter to Marguerite B. Coe regarding award of the Lucile Elliott Scholarship, May 7, 1976
No full textA letter from William C. Younger to Marguerite B. Coe awarding Coe with the Lucile Elliott Scholarship
XMM-Newton observation of the highly magnetised accreting pulsar Swift J045106.8-694803: evidence of a hot thermal excess
No full textSeveral persistent, low luminosity (LX ~ 1034 erg s-1), long spin period (P > 100 s) High Mass X-ray Binaries have been reported with blackbody components with temperatures > 1 keV. These hot thermal excesses have correspondingly small emitting regions (< 1 km2) and are attributed to the neutron star polar caps. We present a recent XMM-Newton target of opportunity observation of the newest member of this class, Swift J045106.8-694803. The period was determined to be 168.5 ± 0.2 s as of 17 July 2012 (MJD = 56125.0). At LX ~ 1036 erg s-1, Swift J045106.8-694803 is the brightest member of this new class, as well as the one with the shortest period. The spectral analysis reveals for the first time the presence of a blackbody with temperature kTBB = 1.8 +0.2-0.3 keV and radius RBB = 0.5 ± 0.2 km. The pulsed fraction decreases with increasing energy and the ratio between the hard (> 2 keV) and soft (< 2 keV) light curves is anticorrelated with the pulse profile. Simulations of the spectrum suggest that this is caused by the pulsations of the blackbody being ~ π out of phase with those of the power law component. Using a simple model for emission from hot spots on the neutron star surface, we fit the pulse profile of the blackbody component to obtain an indication of the geometry of the system
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