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Study site locations at Bay of Sails (77°21.911′S, 163°32.594′E) and Explorers Cove (77°34.259′S, 163°30.699′E) in McMurdo Sound, Ross Sea, Antarctica.
Published: 01 July 2014
Figure 1 Study site locations at Bay of Sails (77°21.911′S, 163°32.594′E) and Explorers Cove (77°34.259′S, 163°30.699′E) in McMurdo Sound, Ross Sea, Antarctica.
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Abundance boxplots of calcareous foraminifera from Bay of Sails and Explorers Cove. Key: Cant = C. antarcticus, Naur = Nonionella auris, Pconic = Patellinoides conica, Pcor = Patellina corrugata, Rglob = Rosalina globularis.
Published: 01 July 2014
Figure 5 Abundance boxplots of calcareous foraminifera from Bay of Sails and Explorers Cove. Key: Cant = C. antarcticus , Naur = Nonionella auris , Pconic = Patellinoides conica , Pcor = Patellina corrugata , Rglob = Rosalina globularis .
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Abundance boxplots of agglutinated foraminifera from Bay of Sails and Explorers Cove. Key: Adisc = Ammodiscus sp, Hbrad = Hemisphaerammina bradyi, Pant = Portatrochammina antarctica, Pceno = Placopsilina cenomana, Pindiv = Psammatodendron indivisum, Tglab = Trochammina glabra, Tves = Tholosina vesicularis.
Published: 01 July 2014
Figure 6 Abundance boxplots of agglutinated foraminifera from Bay of Sails and Explorers Cove. Key: Adisc = Ammodiscus sp, Hbrad = Hemisphaerammina bradyi , Pant = Portatrochammina antarctica , Pceno = Placopsilina cenomana , Pindiv = Psammatodendron indivisum , Tglab = Trochammina glabra
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Species accumulation curves for Bay of Sails (BOS) and Explorers Cove (EC); error bars are 95% confidence intervals.
Published: 01 July 2014
Figure 7 Species accumulation curves for Bay of Sails (BOS) and Explorers Cove (EC); error bars are 95% confidence intervals.
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Rarefaction curve for foraminifera on Bay of Sails (BOS) valves. Samples were rarefied to the lowest abundance of 90 individuals. Key: BV = BOS valve, 1A–4A = top valves, 1B–4B = bottom valves.
Published: 01 July 2014
Figure 8 Rarefaction curve for foraminifera on Bay of Sails (BOS) valves. Samples were rarefied to the lowest abundance of 90 individuals. Key: BV = BOS valve, 1A–4A = top valves, 1B–4B = bottom valves.
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 MgO v. SiO2 variation illustrating the relationships between the Kangaroo Island S-type complexes. Shaded envelope: local composition of Kanmantoo Group sedimentary rocks (psammo-pelites–greywackes); large shaded circles, biotite granodiorite diatexite from Vivonne Bay and Stun Sail Boom River; shaded squares, the intrusive, porphyritic granite at Vivonne Bay and Stun Sail Boom River; small shaded circles, garnet leucogranite; crossed squares, biotite melanosome rocks from Vivonne Bay. The 62% restite trend shown illustrates the extent of variation resulting from extraction of 62% of a restite composed of biotite (35%)  An35 plagioclase (37%)  quartz (28%)  minor apatite (Table 6). Large shaded square, bulk composition of this restite. R–R is the restite-controlled diatexite trend.
Published: 01 September 2002
Fig. 8.  MgO v. SiO 2 variation illustrating the relationships between the Kangaroo Island S-type complexes. Shaded envelope: local composition of Kanmantoo Group sedimentary rocks (psammo-pelites–greywackes); large shaded circles, biotite granodiorite diatexite from Vivonne Bay and Stun Sail
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 Field photograph showing detail of the biotite granodiorite diatexite at Vivonne Bay–Stun Sail Boom River. Hammer for scale (35 cm).
Published: 01 September 2002
Fig. 3.  Field photograph showing detail of the biotite granodiorite diatexite at Vivonne Bay–Stun Sail Boom River. Hammer for scale (35 cm).
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Percentages of calcareous and agglutinated foraminifera on top and bottom valves for Bay of Sails (BOS) and Explorers Cove (EC); significant differences exist between top and bottom valves and between sites (see text).
Published: 01 July 2014
Figure 4 Percentages of calcareous and agglutinated foraminifera on top and bottom valves for Bay of Sails (BOS) and Explorers Cove (EC); significant differences exist between top and bottom valves and between sites (see text).
Journal Article
Published: 23 October 2019
Journal of Foraminiferal Research (2019) 49 (4): 434–455.
..., Alaska. Forty-one ballast sediment samples were obtained during 1998–1999 from 11 oil tankers that routinely discharged their ballast in Prince William Sound after sailing from other West Coast (Los Angeles/Long Beach Harbor, San Francisco Bay, and Puget Sound) or foreign ports (Japan, Korea, and China...
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Published: 01 July 2014
Table 1 Species and abundance of calcareous and agglutinated foraminifera that encrust the valves of the Antarctic scallop Adamussium colbecki from Bay of Sails (BOS) and Explorers Cove (EC), McMurdo Sound, Antarctica. Key: Valves are labeled by site, replicate number, and top (A) or bottom (B
Journal Article
Published: 01 July 2014
Journal of Foraminiferal Research (2014) 44 (3): 255–280.
...Figure 1 Study site locations at Bay of Sails (77°21.911′S, 163°32.594′E) and Explorers Cove (77°34.259′S, 163°30.699′E) in McMurdo Sound, Ross Sea, Antarctica. ...
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Series: GSA Special Papers
Published: 01 January 1939
DOI: 10.1130/SPE7-p49
... Introduction GENERAL CONSIDERATIONS In the days when ocean commerce was borne in relatively small, shallow draft, slow moving sailing vessels, the chart needs of the mariner were limited to a narrow belt along the coast. In fact, the charts extended farther inland during this period...
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Q-mode cluster dendrogram of encrusting foraminifera based on average linkage and Bray-Curtis dissimilarity. Dotted lines indicate two clusters, one at 67% dissimilarity and one with four subclusters (denoted by A, B, C, D) below 42% dissimilarity. Key: Bay of Sails valves = BV, Explorers Cove valves = EV, 1A–4A = top valves, 1B–4B = bottom valves.
Published: 01 July 2014
Figure 11 Q-mode cluster dendrogram of encrusting foraminifera based on average linkage and Bray-Curtis dissimilarity. Dotted lines indicate two clusters, one at 67% dissimilarity and one with four subclusters (denoted by A, B, C, D) below 42% dissimilarity. Key: Bay of Sails valves = BV
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Additive partitioning of foraminifera encrusting A. colbecki habitat islands based on species richness at Bay of Sails (BOS) and Explorers Cove (EC). Alpha diversity: α1 is the average of all valves; α2, average valve diversity for top or bottom valves; α3, average diversity for each site (top and bottom valves pooled per site); and γ = global diversity (all valves pooled).
Published: 01 July 2014
Figure 12 Additive partitioning of foraminifera encrusting A. colbecki habitat islands based on species richness at Bay of Sails (BOS) and Explorers Cove (EC). Alpha diversity: α1 is the average of all valves; α2, average valve diversity for top or bottom valves; α3, average diversity for each
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Additive partitioning for A. colbecki habitat islands for Shannon H and Shannon expH at Bay of Sails (BOS) and Explorers Cove (EC). Alpha diversity: α1 is the average of all valves; α2, average valve diversity for top or bottom valves; α3, average diversity for each site (top and bottom valves pooled per site); and γ = global diversity (all valves pooled).
Published: 01 July 2014
Figure 13 Additive partitioning for A. colbecki habitat islands for Shannon H and Shannon exp H at Bay of Sails (BOS) and Explorers Cove (EC). Alpha diversity: α1 is the average of all valves; α2, average valve diversity for top or bottom valves; α3, average diversity for each site (top
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Mean densities of encrusting foraminifera/cm2 in sectors from top and bottom valves of A. colbecki at Bay of Sails (BOS) and Explorers Cove (EC). A: BOS top valve; B: EC top valve; C: BOS bottom valve; D: EC bottom valve. Asterisks (*) indicate that densities are significantly less than the lower confidence intervals for a t-distribution; arrows indicate densities that are significantly higher than the upper confidence interval for a t-distribution (see text). Total mean density/cm2: BOS top valves = 5.24, bottom valves = 4.3; EC top valves = 6.86, bottom valves = 2.56.
Published: 01 July 2014
Figure 3 Mean densities of encrusting foraminifera/cm 2 in sectors from top and bottom valves of A. colbecki at Bay of Sails (BOS) and Explorers Cove (EC). A : BOS top valve; B : EC top valve; C : BOS bottom valve; D : EC bottom valve. Asterisks (*) indicate that densities
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 Geochemical variation of ASI, V, εNd and CaO with silica. □, rhyodacites and dacites from the Cape Hart composite dykes; ♦, the mafic rocks from the Cape Hart composite dykes; ◊, dolerites from the similarly orientated and assumed age equivalent Woodside dyke complex (Fig. 2; Foden et al. 2002); shaded circles, biotite granodiorite diatexites from the Vivonne Bay–Stun Sail Boom River Complex. In the εNd v. SiO2 figure the mixing trend is that produced between the garnet leucogranite S-type melt and the most primitive Woodside dolerite (Table 3). The shaded field is that of the Kanmantoo clastic sedimentary rocks.
Published: 01 September 2002
et al . 2002 ); shaded circles, biotite granodiorite diatexites from the Vivonne Bay–Stun Sail Boom River Complex. In the ε Nd v. SiO 2 figure the mixing trend is that produced between the garnet leucogranite S-type melt and the most primitive Woodside dolerite ( Table 3 ). The shaded field
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Global non-metric multidimensional scaling plot (NMDS) for species abundance distributions on individual valves from Bay of Sails (denoted by BV) and Explorers Cove (denoted by EV). Axis 1 (NMDS1) appears to represent the number of species, with increasing species richness toward the right (e.g., valve BV1B had three species, while valve EV4B had nine species). Axis 2 (NMDS2) appears to be ordinated based on dominant species: valves with more T. glabra occur near the bottom of the plot, those in the middle have high abundances of P. antarctica and T. glabra, and valves near the top have high abundances of C. antarcticus. Key: 1A–4A = top valves, 1B–4B = bottom valves, circles indicate valves with different ranked abundance of the dominant species.
Published: 01 July 2014
Figure 10 Global non-metric multidimensional scaling plot (NMDS) for species abundance distributions on individual valves from Bay of Sails (denoted by BV) and Explorers Cove (denoted by EV). Axis 1 (NMDS1) appears to represent the number of species, with increasing species richness toward
Journal Article
Published: 13 February 2019
Seismological Research Letters (2019) 90 (2A): 475–476.
... for mitigation and preparation to improve earthquake safety in the Bay Area. Jack authored more than 90 scientific publications and a body of other writing. In the months before his death, he was writing “The Sound Before Us: Ice Sheets, Sea Level, and Sailing in Fishers Island Sound,” an essay about...
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Journal Article
Published: 01 October 2013
Earth Sciences History (2013) 32 (2): 235–251.
... and momentous hitherto undertaken by man” ( Anonymous 1819c , p. 104). Unfortunately, the polar expedition under David Buchan, like Phipps, failed to sail any farther than Spitsbergen due to heavy ice. The other ships, under John Ross, sailed around Baffin Bay but failed to discover any outlet from that body...
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