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  • 1
    Publication Date: 2023-03-25
    Keywords: AGE; Argilloecia; BJ8-03-70GGC; Bradleya; GGC; Giant gravity corer; Index; Krithe; Ostracoda, other; Species diversity
    Type: Dataset
    Format: text/tab-separated-values, 276 data points
    Location Call Number Limitation Availability
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  • 2
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    PANGAEA
    In:  Supplement to: Iwatani, Hokuto; Yasuhara, Moriaki; Rosenthal, Yair; Linsley, Braddock K (2018): Intermediate-water dynamics and ocean ventilation effects on the Indonesian Throughflow during the past 15,000 years: Ostracod evidence. Geology, https://doi.org/10.1130/G40177.1
    Publication Date: 2023-01-13
    Description: The Indonesian Throughflow (ITF) is thought to influence thermohaline circulation dynamics and is important for understanding global climate and the marine ecosystem. The physical and chemical properties of North Pacific Intermediate Water (NPIW) and the underlying deep water incorporated into the ITF appear to be the result of climate-related preconditioning in the North and South Pacific. Thus, these high-latitude source waters play an important role in the Indo-Pacific oceanography. Here, we present the results of down-core faunal analyses of fossil ostracods (Crustacea) that we argue reflect NPIW variability in the central part of the Makassar Strait in the ITF over the past 15 k.y. The results show that the warm-water and low-oxygen–water fauna, and species diversity, rapidly increased at ca. 12 ka, reaching maxima during the Younger Dryas (YD). We interpret the faunal change and the diversity maximum at ca. 12 ka as a response to the stagnation of intermediate water due to the decline in ITF intensity during the YD. After ca. 7 ka, the ostracod faunal composition clearly changed from a relatively shallower, warmer, and low-oxygen fauna to a relatively deeper, colder, and high-oxygen fauna. Our interpretation is that the ostracod fauna was responding to the deglacial–early Holocene sea-level rise and the ventilation variations due to the mixing of the NPIW and the underlying deep water. The intermediate-water environment and the ecosystem in the ITF could have been driven by the intensification of the influence of the underlying deep water, caused by changes in the southern high-latitude source due to the latitudinal displacements of the southwesterly winds.
    Keywords: BJ8-03-70GGC; GGC; Giant gravity corer
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 3
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    PANGAEA
    In:  Supplement to: Huang, Huai-Hsuan May; Yasuhara, Moriaki; Iwatani, Hokuto; Alvarez Zarikian, Carlos A; Bassetti, Maria Angela; Sagawa, Takuya (2018): Benthic Biotic Response to Climate Changes Over the Last 700,000 Years in a Deep Marginal Sea: Impacts of Deoxygenation and the Mid‐Brunhes Event. Paleoceanography and Paleoclimatology, 33(7), 766-777, https://doi.org/10.1029/2018PA003343
    Publication Date: 2023-07-10
    Description: The Sea of Japan is a marginal sea, semi-enclosed by the Eurasian Continent, Korean Peninsula, Japanese archipelago, and connected to the Pacific Ocean and adjacent seas by three shallow straits (water depths 〈 130 m). Marginal seas are ideal natural laboratories to study biotic responses to large-scale environmental changes as they are typically sensitive to glacial-interglacial and stadial-interstadial climatic cycles. However, only limited number of studies covers time periods beyond 1 to 2 glacial-interglacial cycles. Here we present a 700,000-year record of benthic biotic response to past oceanographic changes in the southern Sea of Japan, covering the past seven glacial-interglacial cycles, based on ostracode assemblages at the IODP Site U1427. The results indicate that the long-term oxygen variability has been a major control of deep marginal sea biota. Five local extirpation events were recognized as barren zones during glacial maxima (i.e., sea-level minima) immediately before terminations I, II, IV, V, and VII in MISs 2, 6, 10, 12, and 16, which are probably caused by bottom-water oxygen depletion. The results of multivariate analyses indicated clear faunal cyclicity influenced by glacial-interglacial scale oxygen variability with the succession from opportunistic species dominance through tolerant infauna dominance to barren zone during the deoxygenation processes and the opposite succession during the recovery processes. The Sea of Japan ostracode abundance and faunal composition showed distinct difference between the post- and pre-MBE (Mid-Brunhes Event at around 400-350 ka) periods, indicating the MBE as a major disturbance event of deep-sea, especially marginal-sea ecosystems. The MBE shortened the duration of the extirpation events, fostered dominance of warmer-water species, and amplified the glacial-interglacial faunal cyclicity. Our long-term biotic response study clearly indicates that deep marginal sea ecosystems are dynamic and vulnerable to climate changes.
    Keywords: 346-U1427; Acanthocythereis dunelmensis; Acanthocythereis sp.; AGE; Argilloecia sp.; Asian Monsoon; Calculated after Simpson-Index; CDRILL; Core drilling; Counting; Cytheropteron hyalinosa; DEPTH, sediment/rock; Exp346; Falsobuntonia sp.; Falsobuntonia taiwanica; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Krithe antisawanense; Krithe sawanensis; Loxoconchidea dolgoiensis; Ostracoda; Ostracoda, other; Palmenella limicola; Palmoconcha parapontica; Robertsonites hanaii; Sample code/label; Sample volume; Sea of Japan/East Sea; Simpson index of diversity
    Type: Dataset
    Format: text/tab-separated-values, 7389 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2023-07-09
    Description: This is the ostracods census data from 157 sub-samples from two marine sediment cores, JM10-10GC and JM10-12GC, from Storfjorden, Svalbard. Cores were taken in October 2010 by RV 'Jan Mayen'. JM10-10GC is 402 cm long, sampled at 5-cm intervals. JM10-12GC is 320 cm long, sampled at 4-cm intervals. The cores comprise the last 13500 years. Cores were split in two halves and one half of each core was cut up in 1 cm thick sample slices. Each sample slice at 5 cm (core JM10-10GC) and 4 cm (cores JM10-12GC) interval was wet sieved with mesh sizes of 63, 100 and 1000 μm, oven dried, and then dry sieved with mesh-size of 150 μm. The size fraction 〉150 μm was analyzed for the content of benthic ostracods. All species were identified to species level.
    Keywords: Acanthocythereis dunelmensis; Arctic Ocean; Argilloecia cf. robinwhatleyi; Argilloecia sp.; Baffinicythere howei; Bythocythere constricta; Calendar age; Cluthia cluthae; Counting 〉150 µm fraction; Cytheropteron arcuatum; Cytheropteron biconvexa; Cytheropteron carolinae; Cytheropteron champlainum; Cytheropteron dimlingtonensis; Cytheropteron discoveria; Cytheropteron hamatum; Cytheropteron inflatum; Cytheropteron irizukii; Cytheropteron laptevensis; Cytheropteron montrosiense; Cytheropteron nodosoalatum; Cytheropteron nodosum; Cytheropteron parahamatum; Cytheropteron paralatissimum; Cytheropteron pseudoinflatum; Cytheropteron pseudomontrosiense; Cytheropteron pyramidale; Cytheropteron scoresbyi; Cytheropteron tumefactum; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Elofsonella concinna; Event label; Finmarchinella angulata; Finmarchinella finmarchica; GC; Gravity corer; Hemicythere villosa; Hemicytherura clathrata; Heterocyprideis facis; Heterocyprideis sorbyana; Holocene; JM10-10GC; JM10-12GC; Krithe glacialis; Latitude of event; Longitude of event; Loxoconcha sp.; Normanicythere leioderma; Ostracoda; Palmenella limicola; Paracytherois sp.; Polycope bireticula; Pseudocythere caudata; Rabilimis mirabilis; Rabilimis septentrionalis; Robertsonites tuberculatus; Roundstonia globulifera; Roundstonia macchesneyi; Sarsicytheridea bradii; Sarsicytheridea punctillata; Sclerochilus sp.; Semicytherura complanata; Semicytherura concentrica; Semicytherura sp.; Storfjord, Svalbard, Norway; The last deglaciation
    Type: Dataset
    Format: text/tab-separated-values, 8635 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2023-07-10
    Keywords: Actinocythereis cf. levinsoni; Alataconcha pterogona; Ambostoracon sp.; Argilloecia spp.; Aurila sp.; BJ8-03-70GGC; Bradleya multicostata; Bradleya sp.; Buntonia sp.; Bythoceratina sp.; Bythocypris sp.; Callistocythere sp.; Cardobairdia balcombensis; Caudites sp.; Chejudocythere cf. higashikawai; Chejudocythere sp.; Copytus posterosulcus; Cornucoquimba sp.; Cytherella spp.; Cytherelloidea sp.; Cytherois sp.; Cytheropteron aff. miurense; Cytheropteron excism; Cytheropteron hanaii; Cytheropteron miurense; Cytheropteron sp.; Cytheropteron testudo; Cytheropteron uchioi; DEPTH, sediment/rock; Eucytherura aff. spinosa; Eucytherura sp.; Falsobuntonia ornata; Forcipicythere sp.; GGC; Giant gravity corer; Hemiparacytheridea cf. minaminipponica; Javanella sp.; Kotoracythere sp.; Krithe sp.; Lankacythere sp.; Legitimocythere sp.; Loxoconcha aff. uranouchiensis; Loxoconcha alata; Loxoconcha sp.; Loxoconchidea sp.; Loxocorniculum georgei; Macrocypris spp.; Microcythere sp.; Microcythere vittata; Miocyprideis sp.; Neomonoceratina sp.; Neonesidea spp.; Number of species; Ostracoda indeterminata; Pacambocythere aff. reticulata; Pacambocythere sp.; Paijenborchella cf. iocosa; Paijenborchella cymbula; Paijenborchella iocosa; Paijenborchella sp.; Palmoconcha semistriata; Palmoconcha sp.; Paracypris sp.; Paracytheridea echinata; Paracytherois sp.; Paradoxostoma spp.; Parahemingwayella dowingae; Parakrithella cf. oblongata; Parakrithella oblongata; Parakrithe sp.; Paranesidea sp.; Pedicythere cf. atroposopetasi; Pedicythere lachesisopetasi; Perissocytheridea sp.; Phlyctocythere hamanensis; Phlyctocythere reticulosa; Pistocythereis cf. bradyformis; Pistocythereis sp.; Polycope spp.; Pontocythere suprema; Profundobythere sp.; Propontocypris spp.; Pseudocythere caudata; Pseudocythere sp.; Rimacytheropteron sinense; Saida torresi; Semicytherura cf. minaminipponica; Semicytherura cf. prona; Semicytherura indonesiaensis; Semicytherura sp.; Tanella gracilis; Xestoleberis cf. okinawensis; Xestoleberis hanaii; Xestoleberis sp.; Xestoleberis variegata; Xylocythere sp.
    Type: Dataset
    Format: text/tab-separated-values, 6157 data points
    Location Call Number Limitation Availability
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