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  • 1
    Publication Date: 2023-02-23
    Description: Radiolarians are planktonic protozoon that play an important role in marine ecosystem and paleoenvironmental construction. The South China Sea (SCS) and Malacca Strait (MLS), strongly influenced by the East Asian monsoon, are the key gateway between the Pacific and Indian Oceans. However, a few plankton studies of radiolarians are performed during winter and spring in the SCS and MLS due to the adverse sea conditions. In this study the use of a ship-board plankton net rendered it possible to obtain shallow water samples (~5 m depth) along transects from the northern SCS to MLS during the spring of 2017 and winter of 2017-2018. The results show that partitioning among Spumellaria, Nassellaria and Collodaria radiolarians differed spatially and seasonally. The high partition of Collodaria and low partition of Nassellaria are potential indicators of the strongly stratified waters with low nutrients for paleoceanographic studies in the slope and basin SCS. The radiolarian assemblages in the MLS are quite different from those in the SCS, that is, the two communities are largely independent, suggesting that advective transport between the MLS and SCS is rare. There are obvious seasonal variations in species diversity and abundance in both the MLS and SCS, generally with higher biodiversity and maximum abundances in winter. The results of Q-mode cluster analysis showed that radiolarian assemblages during winter were grouped together in the slope and basin SCS, and their distributions had moved to the southwest relative to those in spring. The results demonstrate the East Asian monsoon has a significant controlling effect on radiolarian diversity and geographic distribution in the studied areas. We also established five candidates for weakly stratified waters with high nutrients: Archiperidium hexacantha, Acanthodesmia vinculatus, Peromelissa phalacra, Dictyocoryne muelleri, and Tetrapyle octacantha. Thus, this study increases the knowledge of radiolarian geographic distribution in the tropics as a whole, as well as revealing the sensitive response of radiolarians to the regional environments, a fact which may prove useful for reconstructing the paleoceanographic changes.
    Keywords: Acanthodesmia vinculata; Acrobotrissa cf. cribrosa; Actinomma arcadophorum; Amphispyris hertwigi; Amphispyris reticulata; Arachnocorys circumtexta; Arachnosphaera myriacantha; Archiperidium hexacantha; Astrosphaera hexagonalis; Biodiversity; Botryocyrtis scutum; Buccinosphaera invaginata; Centrocubus octostylus; Counting, radiolarians; Dictyoceras virchowii; Dictyocoryne elegans; Dictyocoryne muelleri; Dictyocoryne profunda; Dictyocoryne truncatum; Dictyocryphalus? acrostoma; Dictyocryphalus? democriti; Dictyocryphalus? variabilis; Didymocyrtis tetrathalamus tetrathalamus; East Asian monsoon; Eucyrtidium acuminatum; Event label; Flustrella perispira; Geographic distribution; Heliodiscus spp.; Identification; LATITUDE; Lipmanella prismaticum; Living radiolarians; LONGITUDE; Myelastrum lobum; Neosemantis distephanus; Perichlamydium venustum; Peromelissa phalacra; Phorticium polycladum; Plectacantha oikiskos; Plegmosphaerella spongiacea; Pseudocubus obeliscus; Pterocanium praetextum praetextum; Pterocorys fastuosa; Pterocorys sabae; Pylodiscus spinulosa; Radiolarians indeterminata; Rhizosphaera medianum; SCS/MS_1; SCS/MS_11; SCS/MS_13; SCS/MS_15; SCS/MS_16; SCS/MS_17; SCS/MS_18; SCS/MS_2; SCS/MS_20; SCS/MS_22; SCS/MS_23; SCS/MS_25; SCS/MS_27; SCS/MS_28; SCS/MS_30; SCS/MS_31; SCS/MS_4; SCS/MS_5; SCS/MS_7; SCS/MS_72; SCS/MS_74; SCS/MS_76; SCS/MS_77; SCS/MS_78; SCS/MS_80; SCS/MS_82; SCS/MS_84; SCS/MS_86; SCS/MS_88; SCS/MS_9; SCS/MS_90; SCS/MS_92; SCS/MS_94; SCS/MS_96; Siphonosphaera abyssi; South China Sea; Sphaerolarnacillium cochleatum; Sphaeropylolena spp.; Sphaerozoum bifurcum; Spirocyrtis scalaris; Spongaster pentas; Spongaster tetras tetras; Spongastriscus ellipticus; Spongocyclia cycloides; Spongodiscus heliodes; Spongodiscus resurgens; Spongosphaera streptacantha; Spongospira sp.; Stylodictya arathnia; Stylodictya cf. hertwigii; Tetrapyle circularis; Tetrapyle fruticosa; Tetrapyle octacantha; Tetrapyle spp.; Time coverage; tropics; Water sample; WS; Zygocircus acacia; Zygocircus piscicaudatus; Zygocircus productus
    Type: Dataset
    Format: text/tab-separated-values, 2142 data points
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  • 2
    Publication Date: 2024-01-09
    Keywords: 189-1172A; 189-1172D; Age, comment; Age model; Ageprofile Datum Description; Ageprofile Datum Type; Boundary description; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Error, absolute; Event label; Joides Resolution; Leg189; Ocean Drilling Program; ODP; Sample code/label; Sample code/label 2; Tasman Sea
    Type: Dataset
    Format: text/tab-separated-values, 2615 data points
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  • 3
    Publication Date: 2024-01-09
    Keywords: 189-1171; Age, comment; Age model; Ageprofile Datum Description; Ageprofile Datum Type; Boundary description; COMPCORE; Composite Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Error, absolute; Hole; Joides Resolution; Leg189; Ocean Drilling Program; ODP; Sample code/label; Sample code/label 2; South Pacific Ocean
    Type: Dataset
    Format: text/tab-separated-values, 1774 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Matsuzaki, Kenji M; Nishi, Hiroshi; Suzuki, Noritoshi; Cortese, Giuseppe; Eynaud, Frédérique; Takashima, Reishi; Kawate, Yumiko; Sakai, Toyusaburo (2014): Paleoceanographic history of the Northwest Pacific Ocean over the past 740kyr, discerned from radiolarian fauna. Palaeogeography, Palaeoclimatology, Palaeoecology, 396, 26-40, https://doi.org/10.1016/j.palaeo.2013.12.036
    Publication Date: 2024-01-09
    Description: The Northwest Pacific Ocean is characterized by a strong mixing of water masses, due to the interplay of three distinct currents, i.e., the Kuroshio, the Tsugaru, and the Oyashio. The C9001C drill core site, located east of the Shimokita Peninsula and directly influenced by the Tsugaru warm current and the Oyashio subarctic current was used here to reconstruct the paleoceanographical history of this region, especially focusing on the Mid-Brunhes Event (MBE) and its consequences. This core provides a continuous record from marine isotope stage (MIS) 18 (740 ka) to the present. Polycystine radiolarian assemblages were analyzed to highlight paleoceanographic and sea surface temperature changes at this site. Based on the radiolarian fauna, seven time periods are defined, which coincide with changes in the dynamics of the Tsugaru and Oyashio currents, respectively. The oldest time interval covered by our analysis (i.e., VII: 740-621 ka) was marked by generally sluggish ocean circulation. The Tsugaru Current influence increased during the following Interval VI (621-478 ka) which encompasses interglacials MIS 15 and 13, while the Oyashio Current strengthened during the Interval V (478-337), i.e. from glacials MIS 12 to 10. These latter intervals (VI to V) constitute a long climatic transitional period where Tsugaru Current and Oyashio Current influences are strengthened. In the time period from Interval IV to Interval I (0-337 ka), the warming intensity of interglacials (MIS 9, MIS 5) appears to be close to the modern one. However, several unusually warm glacials, associated with a relatively strong Tsugaru Current flow, were identified during this interval (e.g., MIS 8 and MIS 6). Radiolarian productivity data suggest that during Intervals VII to V, deep water masses are rich in nutrient content. However, a high vertical mixing event is recorded after Interval IV, when high nutrient concentrations appear to shift to the surface layer.
    Keywords: Acanthodesmia vinculata; Actinomma boreale; Actinomma leptodermum; Amphirhopalum virchowii; Amphisphaera spumacea; Amphisphaera tanzhiyuani; Archiperidium spp.; Axoprunum acquilonium; Bortyostrobus seriatus; Botryocampe inflata; Botryopera cf. chlamida; Botryostrobus aquilonaris; C9001C; Carpocanistrum spp.; Cenosphaera sp.; Ceratocyrtis aff. mashae; Ceratocyrtis spinosiretis; Ceratospyris borealis; Ceratospyris problematica; Cinclopyramis murrayana; Cladoccocus dentata; Cladococcus bifurcus; Cycladophora bicornis; Cycladophora davisiana; Cyrtidosphaera reticulata; DEPTH, sediment/rock; Dictyocoryne muelleri; Dictyocoryne profunda; Dictyocoryne truncatum; Didymocyrtis tetrathalamus; DRILL; Drilling/drill rig; Eucecryphalus cervus; Eucecryphalus sp.; Eucyrtidium acuminatum; Eucyrtidium frohlichi; Flustrella cf. camerina; Flustrella polygonia; Gondwanaria dogieli; Haliomma miocenica; Heliodiscus cf. tunicatus; Hexacontium pachydermum; Lamprocyclas maritalis; Lamprocyrtis sp.; Lamprotripus sp.; Larcopyle buetschlii; Larcopyle cervicone; Larcopyle spp.; Larcopyle weddellium; Lipmanella irregulare; Lithelius haeckelispiralis; Lithelius nautiloides; Lithopera bacca; Lochnosphaera boreale; Lychnocanoma sakaii; Northwestern Pacific Ocean; Ocean Drilling Program; ODP; Phorticium polycladum; Phorticium pylonium; Plagiacantha panarium; Polysolenia spinosa; Pseudodictyophimus gracilipes; Pterocanium korotnevi; Pterocanium praetextum; Pterocorys clausus; Pylodiscus triangularis; Radiolarians, other; Rizosphaera medianum; Sample code/label; Schizodiscus biconcavus; Schizodiscus japonicus; Schizodiscus sp.; Schizodiscus stylotrochoides; Siphonosphaera paraphoros; Siphonosphaera socialis; Sphaeropyle langii; Spongaster tetras irregularis; Spongaster tetras tetras; Spongodiscus resurgens; Spongoliva ellipsoides; Spongopyle osculosa; Spongosphaera boreale; Spongosphaera streptacantha; Spongotrochus helioides; Spongurus cylindricus; Stylochlamydium perichlamydium; Stylochlamydium venustrum; Stylodictya aculeata; Stylodictya validispina; Stylosphaera pyriformis; Tetrapyle octacantha group; Thaecosphaera aequora; Theocorythium trachelium; Tholomura polystyla; Zygocircus cf. piscicaudatus
    Type: Dataset
    Format: text/tab-separated-values, 14507 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Matsuzaki, Kenji M; Suzuki, Noritoshi (2018): Quaternary radiolarian biostratigraphy in the subarctic northeastern Pacific (IODP Expedition 341 Site U1417) and synchroneity of bioevents across the North Pacific. Journal of Micropalaeontology, 37(1), 1-10, https://doi.org/10.5194/jm-37-1-2018
    Publication Date: 2024-01-02
    Description: Expedition 341 of the Integrated Ocean Drilling Program (IODP) retrieved sediment cores spanning the time interval between the Pleistocene and Miocene from the southern Gulf of Alaska. Onboard Pleistocene radiolarian biostratigraphy is hereby refined by increasing the sampling resolution. The 178 core samples from the upper 190 m CCSF-B of Site U1417 contained faunal elements similar to the Northwest Pacific; for example, the three biozones in the Northwest Pacific (i.e., Eucyrtidium matuyamai, Stylatractus universus and Botryostrobus aquilonaris) were also recognized in the Gulf of Alaska, spanning 1.80-1.13 Ma, 1.13-0.45 Ma, and the last 0.45 Myr, respectively. Based on the age model that we used in this study and the shipboard paleomagnetic reversal events, the first occurrences (FOs) of Amphimelissa setosa and Schizodiscus japonicus in the Northeast Pacific were preliminarily determined to be 1.48 and 1.30 Ma, respectively. The last occurrence (LO) of Eucyrtidium matuyamai and the FO of Lychnocanoma sakaii, both well-established bioevents in the Northwest Pacific, were dated at 0.80 Ma and 1.13 Ma, respectively. The LO of E. matuyamai is a synchronous event at 1.05±0.1 Ma in the North Pacific, while the FOs of A. setosa and S. japonicus are significantly older than what found elsewhere at 1.48 Ma and 1.30 Ma, respectively.
    Keywords: 341-U1417A; 341-U1417C; Actinomma robustum; Amphimelissa setosa; Axoprunum acquilonium; Comment; Counts; DRILL; Drilling/drill rig; Eucyrtidium matuyamai; Exp341; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Lychnocanoma sakaii; Sample code/label; Schizodiscus japonicus; Southern Alaska Margin; Southern Alaska Margin: Tectonics, Climate and Sedimentation; Stylatractus universus
    Type: Dataset
    Format: text/tab-separated-values, 1668 data points
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  • 6
    Publication Date: 2024-01-09
    Keywords: 189-1168A; 189-1168B; Age, comment; Age model; Ageprofile Datum Description; Ageprofile Datum Type; Boundary description; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Error, absolute; Event label; Indian Ocean; Joides Resolution; Leg189; Ocean Drilling Program; ODP; Sample code/label; Sample code/label 2
    Type: Dataset
    Format: text/tab-separated-values, 1342 data points
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  • 7
    Publication Date: 2024-01-09
    Keywords: 189-1170A; 189-1170B; 189-1170D; Age, comment; Age model; Ageprofile Datum Description; Ageprofile Datum Type; Boundary description; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; Error, absolute; Event label; Indian Ocean; Joides Resolution; Leg189; Ocean Drilling Program; ODP; Sample code/label; Sample code/label 2
    Type: Dataset
    Format: text/tab-separated-values, 1179 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Stickley, Catherine E; Brinkhuis, Henk; McGonigal, Kristeen L; Chaproniere, George C H; Fuller, Michael D; Kelly, Daniel Clay; Nürnberg, Dirk; Pfuhl, Helen A; Schellenberg, Stephen A; Schoenfeld, Joachim; Suzuki, Noritoshi; Touchard, Yannick; Wei, Wuchang; Williams, Graham L; Lara, Jonathan; Stant, S Audra (2004): Late Cretaceous-Quaternary biomagnetostratigraphy of ODP Sites 1168, 1170, 1171, and 1172, Tasmanian Gateway. In: Exon, NF; Kennett, JP; Malone, MJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 189, 1-57, https://doi.org/10.2973/odp.proc.sr.189.111.2004
    Publication Date: 2024-01-09
    Description: Late Cretaceous (Maastrichtian)-Quaternary summary biostratigraphies are presented for Ocean Drilling Program (ODP) Leg 189 Sites 1168 (West Tasmanian Margin), 1170 and 1171 (South Tasman Rise), and 1172 (East Tasman Plateau). The age models are calibrated to magnetostratigraphy and integrate both calcareous (planktonic foraminifers and nannofossils) and siliceous (diatoms and radiolarians) microfossil groups with organic walled microfossils (organic walled dinoflagellate cysts, or dinocysts). We also incorporate benthic oxygen isotope stratigraphies into the upper Quaternary parts of the age models for further control. The purpose of this paper is to provide a summary age-depth model for all deep-penetrating sites of Leg 189 incorporating updated shipboard biostratigraphic data with new information obtained during the 3 yr since the cruise. In this respect we provide a report of work to November 2003, not a final synthesis of the biomagnetostratigraphy of Leg 189, yet we present the most complete integrated age model for these sites at this time. Detailed information of the stratigraphy of individual fossil groups, paleomagnetism, and isotope data are presented elsewhere. Ongoing efforts aim toward further integration of age information for Leg 189 sites and will include an attempt to correlate zonation schemes for all the major microfossil groups and detailed correlation between all sites.
    Keywords: 189-1168A; 189-1168B; 189-1170A; 189-1170B; 189-1170D; 189-1171; 189-1172A; 189-1172D; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Indian Ocean; Joides Resolution; Leg189; Ocean Drilling Program; ODP; South Pacific Ocean; Tasman Sea
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 9
    Publication Date: 2015-07-01
    Print ISSN: 1434-4610
    Electronic ISSN: 1618-0941
    Topics: Biology
    Published by Elsevier
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  • 10
    Publication Date: 2012-05-01
    Print ISSN: 1434-4610
    Electronic ISSN: 1618-0941
    Topics: Biology
    Published by Elsevier
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