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
  • 1
    Publication Date: 2023-02-23
    Keywords: Age, maximum/old; Age, minimum/young; Calculated; CDRILL; Core drilling; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Lithologic unit/sequence; Miaodao; Unit; Yellow Sea, China
    Type: Dataset
    Format: text/tab-separated-values, 81 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2023-02-23
    Keywords: Age, 14C AMS; Age, dated; Age, dated standard deviation; Calendar age; Calendar age, standard deviation; CDRILL; Core drilling; DEPTH, sediment/rock; Miaodao; Sample, optional label/labor no; Yellow Sea, China
    Type: Dataset
    Format: text/tab-separated-values, 15 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2023-02-23
    Keywords: Ammonia beccarii; Ammonia convexidorsa; Cassidulina carinata; CDRILL; Core drilling; Cribrononion incertum; Elphidium magellanicum; Gallitellia vivans; Globigerina bulloides; Miaodao; Pseudononionella variabilis; Pseudononion sp.; Rosalina vilardeboana; Sample ID; Yellow Sea, China
    Type: Dataset
    Format: text/tab-separated-values, 165 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Du, Shuhuan; Li, Baosheng; Chen, Muhong; Xiang, Rong; Niu, Donefeng; Si, Yuejun (2016): Paleotempestology evidence recorded by eolian deposition in the Bohai Sea coastal zone during the last interglacial period. Marine Geology, 379, 78-83, https://doi.org/10.1016/j.margeo.2016.05.013
    Publication Date: 2023-02-23
    Description: Reconstruction of the generation, development, and evolution of modern storms through paleotempestology is used to understand the regularity of storm activity and the relationship between storm activity and global climate change. Existing paleotempestology research in China is concentrated mainly on the low latitude sediments deposited since the Holocene (about 7000 a). In this study, we examine the storm deposits in the eolian sediments of the Bohai Sea coastal zone at middle latitudes, choosing the Miaodao stratigraphic section (MDS) as the target area. This area is located in the Bohai Sea strait and shows evidence of storms since the last interglacial period using an analysis of the grain size parameter, element ratios, and marine micropaleontology foraminifera fossils in the sediment during the last 130 ka that can be used in our paleotempestology research. The results include three main findings: (1) the marine micropaleontology foraminifer fossils appear in the eolian sediment of the MDS and, in combination with grain size parameter and element ratios of the sediments, serve as evidence of the paleotempestology record on the Bohai Sea coastal zone; (2) planktonic foraminifera fossils appear in the MDS, indicating that the Yellow Sea warm current affected the Bohai Sea during the last interglacial period; and (3) storm activity in the marine isotope stage (MIS) 5a has been recorded in the MDS 15 times. The findings of this study expand the paleotempestology record from 7000 a to 90 ka and serve as a reference for research for middle latitude storm activity.
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Zheng, Fan; Li, Qianyu; Li, Baohua; Chen, Muhong; Tu, Xia; Tian, Jun; Jian, Zhimin (2005): A millennial scale planktonic foraminifer record of the mid-Pleistocene climate transition from the northern South China Sea. Palaeogeography, Palaeoclimatology, Palaeoecology, 223(3-4), 349-363, https://doi.org/10.1016/j.palaeo.2005.04.018
    Publication Date: 2024-01-09
    Description: A high resolution record (~1100 yr) of planktonic foraminifers from ODP Site 1144 in the northern South China Sea reveals rapid and strongly variable climatic changes during the mid-Pleistocene transition period. The abundance of warm water species decreased from an average of 60% in marine isotope stage (MIS) 29 to 〈40% at MIS 22, followed by a steady increase in cool water species toward younger intervals. Many deep dwelling, warm water species decreased to a minimum during MIS 22 and remained extremely rare or even became absent in younger glacial intervals, indicating stepwise sea surface cooling in the region. Estimated SSTs show large fluctuations mostly at glacial-interglacial transitions. A maximum winter temperature difference of 11 °C (17-28 °C) across MIS 23/22 boundary likely corresponded to a major growth of boreal ice sheets across the MPT center at 0.9 myr, coupled with a strengthened winter monsoon over East Asia . The MPT event not only led to a better correlation between changes in species abundances and glacial-interglacial cycles but also a more constrained thermocline that shoaled considerably during subsequent glacial periods. The oxygen isotope record and the abundance of shallow water species display power spectra closely in pace with the 41,000 and 100,000 years cyclicities. A lower coherence over these cyclicities between deep-water dwelling species and the planktonic delta18O, a shoaled thermocline, and more positive glacial delta18O together suggest disturbances of surface and subsurface waters by intensified winter monsoons over the last 1.1-0.5 myr in the South China Sea.
    Keywords: 184-1144; COMPCORE; Composite Core; Joides Resolution; Leg184; Ocean Drilling Program; ODP; South China Sea
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Zhang, Lili; Chen, Muhong; Xiang, Rong; Zhang, Lanlan; Lu, Jun (2009): Productivity and continental denudation history from the South China Sea since the late Miocene. Marine Micropaleontology, 72(1-2), 76-85, https://doi.org/10.1016/j.marmicro.2009.03.006
    Publication Date: 2024-01-09
    Description: Late Miocene–Recent micropaleontological and geochemical records from Ocean Drilling Program (ODP) Site 1143 in the southern South China Sea (SCS) indicate that increase and decrease in abundance of siliceous plankton may be controlled mainly by the input of nutrients derived from land and provided by upwelling. A high export production event - a “biogenic bloom” event - occurred in the southern SCS between 12 and 6 Ma. During this period, high ratios of smectite/(illite + chlorite), smectite/quartz and Al/K indicate a high weathering intensity of the Asian continent, possibly due to the intensification of the East Asian Summer Monsoon (EASM), which may have increased the net flux of nutrients to the ocean, both directly through terrestrial input and indirectly through upwelling activity. A drop in Ba/Ti, Al/Ti and Ca/Ti values around 6 Ma may indicate a lowering of productivity, possibly due to the large consumption of sea surface nutrients by the “biogenic bloom”. Alternatively, it may indicate a shift in terrigenous input source area. At about 5.4 Ma, a decrease in weathering intensity, as indicated by a sudden decrease in the values of smectite/(illite + chlorite), smectite/quartz and Al/K, might have led to a sudden decrease of terrestrial nutrient input to the SCS. We suggest that the biogenic bloom ended when nutrients in surface waters were exhausted, because of a decrease in supply as well as a decrease in upwelling intensity due to weakening of the EASM. As a result, radiolarians were absent in the studied area between ~6 and 3.2 Ma. At ~3.2 Ma, radiolarians began to recover, possibly because the start of Northern Hemispheric glaciation and the rapid uplift of the Tibet Plateau led to intensification of the East Asian monsoon. After the Mid-Pleistocene Climate Transition at 0.9 Ma, the abundance and mass accumulation rates of radiolarians increased, probably as a result of increased upwelling activity driven by the increasing intensity of the summer monsoon.
    Keywords: 184-1143; Accumulation rate, mass; Accumulation rate, radiolarians by number; AGE; Aluminium/Potassium ratio; Aluminium/Titanium ratio; Aluminium oxide; Barium; Barium/Titanium ratio; Calcium/Titanium ratio; Calcium oxide; Calculated; COMPCORE; Composite Core; Density, dry bulk; DEPTH, sediment/rock; ICP-MS, Perkin-Elmer, Elan 6000; Joides Resolution; Leg184; Loss on ignition; Ocean Drilling Program; ODP; Potassium oxide; Radiolarians; Sedimentation rate; Silicon dioxide; South China Sea; Titanium dioxide; X-ray fluorescence (XRF)
    Type: Dataset
    Format: text/tab-separated-values, 480 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Lu, Jun; Chen, Muhong; Wang, Rujian; Pushkar, Vladimar S (2004): Data report: Diatom records of ODP Site 1143 in the southern South China Sea. In: Prell, WL; Wang, P; Blum, P; Rea, DK; Clemens, SC (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 184, 1-9, https://doi.org/10.2973/odp.proc.sr.184.212.2004
    Publication Date: 2024-01-09
    Description: Diatoms from Ocean Drilling Program Leg 184 Site 1143 in the southern South China Sea were analyzed for this paper. We found that diatoms are barren or scarce from 27.94 to 304.04 meters below seafloor. The intervals with age-diagnostic species indicate a middle Miocene age from 472.18 to 469.98 mcd, a late Miocene age or younger at 389.42 mcd, and a late Pliocene to Holocene age from 26.7 to 0.0 mcd.
    Keywords: 184-1143; Achnanthes spp.; Actinocyclus curvatulus; Actinocyclus ehrenbergii; Actinocyclus ehrenbergii var. tenella; Actinocyclus ellipticus; Actinocyclus moronensis; Actinocyclus spp.; Actinocyclus subtilis; Actinoptychus marylandicus; Actinoptychus spp.; Actinoptychus undulatus; Amphora spp.; Arachnoidiscus spp.; Asterolampra marylandica; Asteromphalus arachne; Asteromphalus elegans; Asteromphalus flabellatus; Asteromphalus heptactis; Asteromphalus spp.; Azpeitia africana; Azpeitia crenulata; Azpeitia nodulifera; Bacteriastrum hyalinum; Biddulphia spp.; Campylodiscus brightwellii; Campylodiscus spp.; Chaetoceros spp.; Cocconeis scutellum; Cocconeis spp.; COMPCORE; Composite Core; Coscinodiscus anguste-lineatus; Coscinodiscus argus; Coscinodiscus blandus; Coscinodiscus cf. endoi; Coscinodiscus curvatulus; Coscinodiscus decrescens; Coscinodiscus denarius; Coscinodiscus inclusus; Coscinodiscus kuetzingii; Coscinodiscus lacustris; Coscinodiscus lewisianus; Coscinodiscus lineatus; Coscinodiscus marginatus; Coscinodiscus minor; Coscinodiscus nitidus; Coscinodiscus oculatus; Coscinodiscus oculus-iridis; Coscinodiscus radiatus; Coscinodiscus rothii; Coscinodiscus spp.; Coscinodiscus stellaris; Coscinodiscus subconcavus var. tenuior; Coscinodiscus subtilis; Coscinodiscus tabularis; Coscinodiscus temperei; Coscinodiscus temperei var. delicata; Coscinodiscus thorii; Coscinodiscus wittanus; Coscinodiscus yabei; Counting, diatoms; Cyclotella striata; Cyclotella stylorum; Delphineis spp.; Denticulopsis dimorpha; Denticulopsis hustedtii; Denticulopsis punctata hustedtii; Denticulopsis spp.; DEPTH, sediment/rock; Diatoms; Diatoms indeterminata; Diploneis bombus; Diploneis cf. zanzibarica; Diploneis crabro; Diploneis gemmata var. pristiaphora; Diploneis nitescens; Diploneis schimidtii; Diploneis smithii; Diploneis spendida; Diploneis spp.; Diploneis suborbicularis; DSDP/ODP/IODP sample designation; Grammatophora oceanica; Grammatophora spp.; Gyrosigma spp.; Hantzschia amphioxys; Hemiaulus spp.; Hemidiscus cuneiformis; Hyalodiscus spp.; Indeterminable: broken; Indeterminable: corroded; Joides Resolution; Leg184; Licmophora spp.; Navicula directa; Navicula distans; Navicula granulata; Navicula lyra; Navicula lyroides; Navicula spp.; Nitzschia fossilis; Nitzschia interrupta; Nitzschia marina; Nitzschia porteri; Nitzschia reinholdii; Nitzschia spp.; Ocean Drilling Program; ODP; Paralia islandica; Paralia sp.; Paralia sulcata; Plagiogramma spp.; Pleurosigma spp.; Pseudoeunotia doliolus; Pyxidicula weyprechtii; Rhaphoneis amphiceros; Rhaphoneis cf. magnapunctata; Rhaphoneis clavata; Rhaphoneis gemmifera; Rhaphoneis lancettula; Rhaphoneis paralis; Rhaphoneis rhombica; Rhaphoneis sachalinensis; Rhaphoneis spp.; Rhizosolenia bergonii; Rhizosolenia hebetata forma hiemalis; Rhizosolenia spp.; Rhizosolenia styliformis; Rhopalodia spp.; Roperia tesselata; Rossiella paleacea; Rossiella spp.; Rouxia spp.; Sample code/label; South China Sea; Stephanopyxis spp.; Stictodiscus spp.; Surirella fastuosa; Surirella fluminensis; Surirella spp.; Synedra formosa; Synedra spp.; Thalassionema nitzschioides; Thalassionema nitzschioides var. parva; Thalassiosira decipiens; Thalassiosira eccentrica; Thalassiosira gravida; Thalassiosira leptopus; Thalassiosira lineata; Thalassiosira miocenica; Thalassiosira oestrupii; Thalassiosira pacifica; Thalassiosira praeconvexa; Thalassiosira sp.; Thalassiosira spp.; Thalassiothrix frauenfeldii; Thalassiothrix longissima; Trachyneis antillarum; Trachyneis aspera; Trachyneis aspera var. unilatera; Triceratium cinnamomeum; Triceratium favus; Triceratium formosum; Triceratium spp.; Tryblioptychus cocconeiformis
    Type: Dataset
    Format: text/tab-separated-values, 64370 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2024-01-09
    Keywords: 184-1144; Beella digitata; Candeina nitida; COMPCORE; Composite Core; Counting 〉150 µm fraction; DEPTH, sediment/rock; Foraminifera, planktic; Foraminifera, planktic, other; Foraminifera, planktic indeterminata; Globigerina bulloides; Globigerina calida; Globigerina falconensis; Globigerina quinqueloba; Globigerina rubescens; Globigerinella aequilateralis; Globigerinita glutinata; Globigerinoides conglobatus; Globigerinoides ruber pink; Globigerinoides ruber white; Globigerinoides sacculifer sac; Globigerinoides sacculifer wo sac; Globigerinoides tenellus; Globoquadrina conglomerata; Globoquadrina dutertrei; Globorotalia bermudezi; Globorotalia crassaformis; Globorotalia hirsuta; Globorotalia inflata; Globorotalia menardii dextral; Globorotalia menardii sinistral; Globorotalia scitula; Globorotalia truncatulinoides dextral; Globorotalia truncatulinoides sinistral; Globorotalia tumida; Joides Resolution; Leg184; Neogloboquadrina blowi; Neogloboquadrina pachyderma dextral; Neogloboquadrina pachyderma sinistral; Ocean Drilling Program; ODP; Orbulina universa; Pulleniatina obliquiloculata; South China Sea; Sphaeroidinella dehiscens
    Type: Dataset
    Format: text/tab-separated-values, 16812 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2024-01-09
    Keywords: 184-1144; Age model; Ageprofile Datum Description; COMPCORE; Composite Core; DEPTH, sediment/rock; Joides Resolution; Leg184; Marine isotopic stage; Ocean Drilling Program; ODP; South China Sea
    Type: Dataset
    Format: text/tab-separated-values, 38 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Chen, Muhong; Wang, Rujian; Yang, Lihong; Han, Jianxiu; Lu, Jun (2003): Development of east Asian summer monsoon environments in the late Miocene: radiolarian evidence from Site 1143 of ODP Leg 184. Marine Geology, 201(1-3), 169-177, https://doi.org/10.1016/S0025-3227(03)00215-9
    Publication Date: 2024-01-09
    Description: Abundant radiolarians are preserved in the relatively complete upper Miocene section of ODP Site 1143. Three radiolarian zones, RN6, RN7 and RN8, are recognized on the basis of Diartus petterssoni (total range in RN6, 〈11.9-8.77 Ma), Diartus hughesi (last appearance at RN7/RN8, 7.7 Ma) and Stichocorys delmontensis (RN6 to RN8, 〉6.7 Ma). Variations in the abundance of radiolarians,especially Pyloniid forms,radiolarian flux and species diversity are good proxies of upwelling which,similar to today's,was likely driven by summer monsoons. These radiolarian paleomonsoon proxies indicate that the east Asian summer monsoon first initiated close to the middle/late Miocene boundary at ~12-11 Ma and reached a maximum strength at ~8.24 Ma. Therefore,the initiation of the east Asian summer monsoon was likely earlier than the first Indian monsoon,which appeared ~8 myr ago.
    Keywords: 184-1143; Age model; Age model, biostratigraphy; Ageprofile Datum Description; Code; COMPCORE; Composite Core; DEPTH, sediment/rock; Joides Resolution; Leg184; Ocean Drilling Program; ODP; South China Sea
    Type: Dataset
    Format: text/tab-separated-values, 33 data points
    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...