ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Collection
Keywords
  • 11
    Publication Date: 2023-05-12
    Keywords: -; Branch_Steram; Calcium carbonate; Carbon isotope excursion; Comment; Identification; Lithology/composition/facies; Marlborough, New Zealand; OUTCROP; Outcrop sample; Sample comment; SECTION, height; δ13C, carbonate; δ18O, carbonate
    Type: Dataset
    Format: text/tab-separated-values, 1938 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 12
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Slotnick, Benjamin S; Dickens, Gerald Roy; Hollis, Christopher J; Crampton, James; Strong, C Percy; Phillips, Austin (2015): The onset of the Early Eocene Climatic Optimum at Branch Stream, Clarence River valley, New Zealand. New Zealand Journal of Geology and Geophysics, 58(3), 262-280, https://doi.org/10.1080/00288306.2015.1063514
    Publication Date: 2023-05-12
    Description: We present new lithologic, biostratigraphic and carbon isotope records for a calcareous-rich ~84m thick, early Eocene, upper continental slope section now exposed along Branch Stream, Marlborough. Decimetre-scale limestone-marl couplets comprise the section. Several marl-rich intervals correspond to carbon isotope excursions (CIEs) representing increased 13C -depleted carbon fluxes to the ocean. These records are similar to those at nearby Mead Stream, except marl-rich intervals at Branch Stream are thicker with a wider d13C range. Comparison to other sites indicates the section spans ~53.4-51.6 Ma, the onset of the Early Eocene Climatic Optimum (EECO). The most prominent CIE is correlated with the K/X event (52.9 Ma). Prominent marl-rich intervals resulted from increased fluxes of terrigenous material and associated carbonate dilution. We find multiple warming events marked lowermost EECO, each probably signaling enhanced seasonal precipitation. Branch Stream bulk isotopic records suggest 'differential diagenesis' impacted the sequence during sediment burial.
    Keywords: Branch_Steram; Marlborough, New Zealand; OUTCROP; Outcrop sample
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 13
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Hollis, Christopher J (1993): Latest Cretaceous to Late Paleocene radiolarian biostratigraphy: A new zonation from the New Zealand region. Marine Micropaleontology, 21(4), 295-327, https://doi.org/10.1016/0377-8398(93)90024-R
    Publication Date: 2023-06-27
    Description: The scarcity of records of Early Paleocene radiolarians has meant that while radiolarian biostratigraphy is firmly established as an important tool for correlation, there has been a long-standing gap between established zonations for the Cretaceous and from latest Paleocene to Recent. It has also led to considerable speculation over the level of faunal change across the Cretaceous/Tertiary (K/T) boundary. Consequently, the discovery of rich and diverse radiolarian assemblages in well-delineated K/T boundary sections within siliceous limestones of the Amuri Limestone Group in eastern Marlborough, New Zealand, is of great significance for biostratigraphy and K/T boundary research. This initial report is restricted to introducing a new latest Cretaceous to mid Late Paleocene zonation based on the radiolarian succession at four of these sections and a re-examination of faunas from coeval sediments at DSDP Site 208 (Lord Howe Rise). Three new Paleocene species are described: Amphisphaera aotea, Amphisphaera kina and Stichomitra wero. Six new interval zones are defined by the first appearances of the nominate species. In ascending order these are: Lithomelissa? hoplites Foreman (Zone RK9, Cretaceous), Amphisphaera aotea n. sp. (Zone RP1, Paleocene), Amphisphaera kina n. sp. (RP2), Stichomitra granulata Petrushevskaya (RP3), Buryellaforemanae petrushevskaya (RP4) and Buryella tetradica (RP5). Good age control from foraminifera and calcareous nannofossils permits close correlation with established microfossil zonations. Where age control is less reliable, radiolarian events are used to substantially improve correlation between the sections. No evidence is found for mass extinction of radiolarians at the end of the Cretaceous. However, the K/T boundary does mark a change from nassellarian to spumellarian dominance, due to a sudden influx of actinommids, which effectively reduces the relative abundance of many Cretaceous survivors. An accompanying influx of diatoms in the basal Paleocene of Marlborough, together with evidence for an increase of total radiolarian abundance, suggests siliceous plankton productivity increased across the K/T boundary. Possible causes for this apparently localised phenomenon are briefly discussed.
    Keywords: 21-208; Australia; Chancet_Rocks; DRILL; Drilling/drill rig; Flaxbourne_River; Glomar Challenger; HAND; Leg21; New Zealand; Sampling by hand; South Pacific/Tasman Sea/CONT RISE; Wharanui_Point; Woodside_Creek
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 14
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Lüer, Vanessa; Cortese, Giuseppe; Neil, Helen L; Hollis, Christopher J; Willems, Helmut (2009): Radiolarian-based sea surface temperatures and paleoceanographic changes during the Late Pleistocene-Holocene in the subantarctic southwest Pacific. Marine Micropaleontology, 70(3-4), 151-165, https://doi.org/10.1016/j.marmicro.2008.12.002
    Publication Date: 2023-07-10
    Description: A high-resolution record of radiolarian faunal changes from Site Y8 south of the Subtropical Front (STF), offshore eastern New Zealand, provides insight into the paleoceanographic history of the last 265 kyrs. Quantitative analysis of radiolarian paleotemperature indicators and radiolarian-based sea surface temperature (SST) estimates reveal distinct shifts during glacial-interglacial (G-I) climate cycles encompassing marine isotope stages (MIS) 8-1. Faunas at Site Y8 are abundant and diverse and consist of a mixture of species typical of the subantarctic, transitional and subtropical zones which is characteristic of subantarctic waters just south of the STF. During interglacials, diverse radiolarian faunas have increased numbers of warm-water taxa (not, vert, similar 15%) while cool-water taxa decrease to not, vert, similar 11% of the assemblage. Warmest climate conditions occurred during MIS 5.5 and the early Holocene Climatic Optimum (HCO) at the onset of MIS 1 where SSTs reach maxima of 12.8 and 12.9 °C, respectively. This suggests that temperatures during the HCO were comparable to the Eemian, one of the warmest interglacial intervals of the Late Quaternary. Glacials are characterized by less diverse radiolarian faunas with cool-water taxa increasing to 49% of the assemblage. Coolest climate conditions occurred in MIS 4 and 2 where SSTs are reduced to 5.4 °C and 4.3 °C, respectively. Radiolarian faunal changes and SST estimates clearly identify major water masses and oceanic fronts in the offshore eastern New Zealand area. During warmest MIS 5.5 and early MIS 1 substantial influence of northern-sourced Subtropical Surface Water (STW) is evident at Site Y8. This implies southward incursions of STW around the eastern crest of Chatham Rise with the STF displaced towards higher latitudes and spinning off eddies as far south as Campbell Plateau. Additionally, increased flow of the Southland Current (SC) might have enhanced the local occurrence of warm-water radiolarians derived from the subtropical Tasman Sea. Coolest glacials are marked by a strong inflow of cool, southern-sourced waters at Site Y8 indicating a more vigorous flow along the Subantarctic Front (SAF).
    Keywords: Acanthosphaera actinota; Acanthosphaera dodecastyla; Acanthosphaera pinchuda; Acanthosphaera spp.; Acrosphaera arktios; Acrosphaera cyrtodon; Acrosphaera inflata; Acrosphaera lappacea; Acrosphaera mercurius; Acrosphaera murrayana; Acrosphaera spinosa; Acrosphaera spp.; Actinomma antarcticum; Actinomma arcadophorum; Actinomma delicatulum; Actinomma leptodermum leptodermum; Actinomma leptodermum longispina; Actinomma medianum; Actinomma sol; Actinomma spp.; Actinomma trinacria; Actinommidae; Actinosphaera acanthophora; AGE; Amphiplecta acrostoma; Amphirhopalum ypsilon; Androcyclas gamphonycha; Anomalacantha dentata; Antarctissa cylindrica; Antarctissa denticulata; Antarctissa longa; Antarctissa sp. cf. denticulata; Antarctissa spp.; Antarctissa strelkovi; Anthocyrtidium ophirense; Anthocyrtidium zanguebaricum; Arachnocorallium calvata; Arachnocorys umbellifera; Archipilium macroporus; Artostrobiidae; Artostrobus annulatus; Artostrobus joergenseni; Axoprunum bispiculum; Axoprunum stauraxonium; Bathropyramis woodringi; Botryocampe cf. inflata; Botryocampe conythorax; Botryopyle dictyocephalus; Botryostrobus aquilonaris; Botryostrobus auritus/australis; Cannobotryidae; Carpocanarium papillosum group; Carpocaniidae; Carpocanistrum acutidentatum; Carpocanistrum spp.; Carposphaera sp. cf. C. capillacea; Cenosphaera cristata; Cenosphaera sp. aff. C. perforata; Cenosphaera spp.; Ceratocyrtis galeus; Ceratocyrtis histricosus; Ceratocyrtis spp.; Circodiscus microporus; Cladoscenium ancoratum; Cladoscenium sp. cf. C. tricolpium; Clathrocanium coarctatum; Clathrocorys murrayi; Coccodiscidae; Collosphaera confossa; Collosphaera huxleyi; Collosphaera macropora; Collosphaera spp.; Collosphaeridae; Cornutella bimarginata; Cornutella profunda; Corocalyptra alcmenae; Corocalyptra cervus/gegenbauri; Corocalyptra columba; Counting 〉45 µm fraction; Cromyechinus antarctica; Cubotholus spp.; Cycladophora bicornis; Cycladophora davisiana; Cyrtopera laguncula; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Dictyocoryne profunda; Dictyophimus bicornis; Dictyophimus hirundo; Dictyophimus infabricatus; Dictyophimus platicephalus; Dictyophimus spp.; Didymocyrtis sp. cf. D. tetrathalamus; Didymocyrtis tetrathalamus; Dipylissa bensoni; Disolenia zanguebarica; Druppatractus hastatus; Druppatractus irregularis; Druppatractus spp.; Druppatractus variabilis; Euchitonia elegans/furcata group; Eucyrthidium acuminatum octocolum; Eucyrtidium acuminatum acuminatum; Eucyrtidium annulatum; Eucyrtidium anomalum; Eucyrtidium hexagonatum; Eucyrtidium hexastichum; Eucyrtidium matuyamai; Eucyrtidium spp.; Eucyrtidium teuscheri; Euphysetta elegans; GeoB; Geosciences, University of Bremen; Gondwanaria dogieli; Haliometta miocenica; Heliodiscus asteriscus; Hexacontium aristarchi; Hexacontium armatum/hostile group; Hexacontium laevigatum; Hexacontium spp.; Hexastylus spp.; Hexastylus triaxonius; KAL; Kasten corer; Lamprocyclas maritalis maritalis; Lamprocyclas maritalis polypora; Lamprocyrtis nigriniae; Lampromitra cracenta; Lampromitra quadricuspis; Lampromitra schultzei; Lampromitra spp.; Larcopyle buetschlii; Larcopyle spp.; Larcospira quadrangula; Lipmanella bombus; Lipmanella dictyoceras; Lirellidae; Litharachnium tentorium; Litheliidae; Lithelius minor group; Lithelius nautiloides; Lithelius spp.; Lithocampe furcaspiculata; Lithocampe platycephala; Lithocarpium sp.; Lithomelissa borealis; Lithomelissa hystrix; Lithomelissa laticeps; Lithomelissa sp.; Lithomelissa spp.; Lithomelissa stigi; Lithomelissa thoracites; Lithostrobus hexagonalis; Lophophaena buetschlii; Lophophaena hispida; Lophophaena spp.; Lophospyris juvenile; Lophospyris pentagona pentagona; Lophospyris spp.; Mitrocalpis araneafera; Nassellaria; Neosemantis distephanus; Octopyle stenozona; offshore eastern New Zealand; Ommatodiscus cf. haeckeli; Peridium longispinum; Peripyramis circumtexta; Peromelissa phalacra; Phacodiscidae; Phaeodaria; Phormacantha hystrix; Phormospyris spp.; Phormospyris stabilis scaphipes; Phormospyris stabilis stabilis; Phormostichoartus corbula; Phorticium clevei; Phorticium pylonium group; Plagoniidae; Plagoniidae group; Plectacantha sp.; Plectopyramis dodecomma; Porodiscus sp.; Prunopyle spp.; Prunopyle titan; Pseudocubus obeliscus; Pseudodictyophimus gracilipes; Pterocanium praetextum group; Pterocanium sp.; Pterocanium spp.; Pterocanium trilobum; Pterocoryidae; Pterocorys clausus; Pterocorys macroceras; Pterocorys minythorax; Pterocorys sp.; Pterocorys spp.; Pterocorys zancleus; Pylolena armata; Pylonidae; Pylospira octopyle; Rhizoplegma boreale; Saccospyris antarctica; Sample code/label; Saturnalis circularis; Schizodiscus spatangus; Sethoconus tabulatus; Sethodiscus macrococcus; Sethophormis rotula; Siphocampe arachnea group; Siphocampe lineata group; Siphocampe nodosaria; Siphonosphaera martensi; Siphonosphaera socialis; Spirocyrtis scalaris group; Spirocyrtis subscalaris; Spongocore puella; Spongodiscidae; Spongodiscus resurgens; Spongopyle osculosa; Spongotrochus glacialis; Spongotrochus venustum; Spongurus pylomaticus; Spongurus sp.; Spumellaria; Stichopilium variabile var. davisianoides; Streblacantha circumtexta; Stylatractus spp. group; Stylochlamidium asteriscus; Stylochlamidium spp.; Stylodictya aculeata; Stylodictya validispina; Stylosphaera melpomene; Styptosphaera spumacea; T3034_Y8; TAN3034; Tangaroa; Tetrapyle octacantha; Thecosphaera inermis; Thecosphaera spp.; Theocorys veneris; Theocorythium trachelium dianae; Theocorythium trachelium trachelium; Theoperidae; Theopilium tricostatum; Tholonidae; Tholospyris rhombus; Triceraspyris antarctica; Triceraspyris sp. cf. T. antarctica; Trissocyclidae; Trisulcus spp.; Trisulcus triacanthus; Zygocircus productus group
    Type: Dataset
    Format: text/tab-separated-values, 16767 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 15
    Publication Date: 2023-07-10
    Keywords: Abundance; biostratigraphy; Chiasmolithus grandis; Chiasmolithus nitidus; Chiasmolithus spp.; Coccolithus eopelagicus; Coccolithus pelagicus; Cribrocentrum reticulatum; Cyclicargolithus luminis; Cyclicargolithus spp.; Dictyococcites aff. bisectus; Dictyococcites bisectus; Dictyococcites hesslandii; Dictyococcites spp.; Discoaster kuepperi; Discoaster lodonesis; Discoaster multiradiatus; Discoaster saipanensis; Discoaster spp.; Discoster barbadiensis; Eocene; Ericsonia formosa; Fasciculithus; HEIGHT above ground; Koumac, North Province, New Caledonia; Lanternithus minutus; Magnetostratigraphy; Micula murus; Nannofossil abundance; Nannotetrina; Neococcolithus dubius; New Caledonia; Octolithus spp.; Reticulofenestra; Reticulofenestra umbilicus; Sample ID; Sommet-Khian_section; Sphenolithus furcatolithoides; Sphenolithus moriformis; Sphenolithus radians; Sphenolithus spiniger; Thoracosphaera spp.; Toweius pertusus; Tribrachiatus orthostylus; Zyghrablithus bijugatus
    Type: Dataset
    Format: text/tab-separated-values, 8244 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 16
    Publication Date: 2023-06-27
    Keywords: 21-208; Acanthocircus campbelli; Actinomminae indeterminata; Amphicraspedum gracilis; Amphicraspedum prolixum; Amphipternis alamadaensis; Amphipyndax stocki; Amphisphaera cf. magnaporulosa; Amphisphaera coronata; Amphisphaera goruna; Amphisphaera kina; Amphisphaera macrosphaera; Amphymenium cf. splendiarmatum; Amphymenium concentricum; Archaeodictyomitra lamellicostata; Artostrobiidae indeterminata; Artostrobus pusillus; Aspis murus; Aspis sp.; Axoprunum cf. bispiculum; Bathropyramis magnifica; Buryella aff. foremanae; Buryella dumitricai; Buryella foremanae; Buryella granulata; Buryella helenae; Buryella insensis; Buryella kaikoura; Buryella pentadica; Buryella petrushevskayae; Buryella tetradica tetradica; Buryella tetradica tridica; Carpocaniidae indeterminata; Carpocanium spp.; Cassideus aff. mariae; Ceratocyrtis spp.; Cladoscenium aff. fulcratum; Clathrocyclas australis; Cornutella californica; Corythomelissa adunca; Cryptocarpium cf. ornatum; Cycladophora aff. pseudoadvena; Cycladophora cf. cosma; Cycladophora spp.; Cyrtocapsa campi; Cyrtocapsa livermorensis; Deep Sea Drilling Project; DEPTH, sediment/rock; Dictyomitra andersoni; Dictyomitra minima; Dictyomitra multicostata; Dictyophimus aff. campana; Dictyophimus cf. constrictum; Dictyoprora urceolus; Diploplegma aff. somphum; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Entapium regulare; Epoch; Eucyrtidiidae indeterminata; Eusyringium woodsidensis; Glomar Challenger; Heliostylus sp.; Leg21; Litheliidae indeterminata; Lithelius aff. foremanae; Lithelius minor; Lithocampe wharanui; Lithomelissa aitai; Lithomelissa cf. heros; Lithomelissa hoplites; Lithomelissa spp.; Lithomespilus coronatus; Lithostrobus cf. longus; Lithostrobus longus; Lophocyrtis auriculaleporis; Lophocyrtis sp.; Lophophaena mugaica; Lophophaena polycyrtis; Lychnocaniidae indeterminata; Lychnocanium bellum; Lychnocanium satelles; Lychnocanium spp.; Mita regina; Mita sp.; Myllocercion acineton; Nannofossil zone; Orbiculiforma renillaeformis; Palaeotetrapyle muelleri; Patulibracchium spp.; Periphaena heliasteriscus; Peritiviator dumitricai; Phacodiscidae indeterminata; Phaseliforma subcarinata; Phormocyrtis striata striata; Plagiacanthidae indeterminata; Plectodiscus circularis; Porodiscidae indeterminata; Protoxiphotractus wilsoni; Prunopyle adelstoma; Pterocodon aff. tenellus; Pterocodon lex; Pterocyrtidium praebarbadense; Pylonidae indeterminata; Radiolarian preservation; Radiolarians abundance; Radiolarian zone; Sample code/label; Saturnalinae indeterminata; Saturnalis kennetti; Sethochytris babylonis; Siphocampe altamontensis; Siphocampe nodosaria; Siphocampe quadrata; South Pacific/Tasman Sea/CONT RISE; Spirocyrtis aff. greeni; Spongodiscidae indeterminata; Spongodiscus spp.; Spongopyle sanfilippoae; Spongotripus morenoensis; Sponguridae indeterminata; Spongurus cf. bilobatus; Stichomitra bertrandi; Stichomitra carnegiense; Stichomitra cf. carnegiense; Stylodictya cf. targaeformis; Stylodictya spp.; Stylosphaera minor; Stylosphaera pusilla; Thecosphaera larnacium; Thecosphaera ptomatus; Theocampe lispa; Theocampe vanderhoofi; Theocapsomma amphora; Theocapsomma erdnussa; Theocapsomma legumen; Theocapsomma spp.; Theocorys aff. phyzella; Theocorys phyzella; Tholodiscus cf. ocellatus; Tholodiscus splendens; Tholodiscus spp.; Trissocyclidae indeterminata
    Type: Dataset
    Format: text/tab-separated-values, 2720 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 17
    Publication Date: 2023-06-27
    Keywords: 15-152; Age model; Ageprofile Datum Description; Ageprofile Datum Type; Biozone; Caribbean Sea/CONT RISE; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg15
    Type: Dataset
    Format: text/tab-separated-values, 56 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 18
    Publication Date: 2023-06-27
    Keywords: 21-208; Age model; Ageprofile Datum Description; Ageprofile Datum Type; Biozone; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg21; South Pacific/Tasman Sea/CONT RISE
    Type: Dataset
    Format: text/tab-separated-values, 120 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 19
    Publication Date: 2023-06-27
    Keywords: 43-384; Age model; Ageprofile Datum Description; Ageprofile Datum Type; Biozone; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg43; North Atlantic/RIDGE
    Type: Dataset
    Format: text/tab-separated-values, 84 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 20
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Hollis, Christopher J (2002): Biostratigraphy and paleoceanographic significance of Paleocene radiolarians from offshore eastern New Zealand. Marine Micropaleontology, 46(3-4), 265-316, https://doi.org/10.1016/S0377-8398(02)00066-X
    Publication Date: 2024-01-09
    Description: A 100-m-thick Paleocene sequence of mainly pelagic sediments at ODP Site 1121, on the eastern flanks of the Campbell Plateau, contains few to common radiolarians of relatively low diversity in the lower 40 m (Early to early Late Paleocene) and abundant, diverse radiolarian assemblages in the upper 60 m (mid-Late Paleocene). The 150 taxa recorded from the entire Paleocene interval are thought to under-represent the actual species diversity by at least one half as many morphotypes have not been differentiated below the level of genus. Assemblages in the lower 40 m are similar to those described from onland New Zealand and DSDP Site 208 (northern Lord Howe Rise); they are correlated with South Pacific radiolarian zones RP4 and RP5. Assemblages in the upper 60 m differ from other known Late Paleocene assemblages in the great abundance of plagiacanthids and cycladophorids. Similarities are noted with later Cenozoic cool-water assemblages. This upper interval is correlated with South Pacific zone RP6, as revised herein, based on comparison with faunas from Site 208 and Marlborough, New Zealand. The interval is also correlated with the upper part of North Atlantic zone RP6 (RP6b-c) based on the presence of Aspis velutochlamydosaurus, Plectodiscus circularis and Pterocodon poculum. Other species, such as Buryella tetradica and Buryella pentadica, are valuable for local correlation but exhibit considerable diachroneity between the Pacific, Indian and Atlantic Oceans. An age model for the Paleocene interval at Site 1121, based on well-constrained nannofossil and radiolarian datums, indicates that the rate of compacted sediment accumulation doubles from 15 to 30 mm/ka at the RP5/RP6 zonal boundary. In large part this is due to a sudden and pronounced increase in accumulation rates for all siliceous fossils; radiolarians and larger diatoms increase from 〈100 to 〉10 000 specimens/cm2/ka. This apparent increase in biosiliceous productivity is age-equivalent to a mid-Paleocene cooling event (57-59 Ma) identified from global stable isotope records that is associated with the heaviest delta13C values for the entire Cenozoic.
    Keywords: 122-761; 15-152; 181-1121; 181-1121B; 21-208; 43-384; Caribbean Sea/CONT RISE; COMPCORE; Composite Core; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Joides Resolution; Leg122; Leg15; Leg181; Leg21; Leg43; North Atlantic/RIDGE; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean; South Pacific/Tasman Sea/CONT RISE; South Pacific Ocean
    Type: Dataset
    Format: application/zip, 7 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...