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  • 1
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] In the present-day climate, surface water salinities are low in the western tropical Pacific Ocean and increase towards the eastern part of the basin. The salinity of surface waters in the tropical Pacific Ocean is thought to be controlled by a combination of atmospheric convection, ...
    Type of Medium: Electronic Resource
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  • 2
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    AGU (American Geophysical Union)
    In:  In: Methane Hydrates in Quaternary Climate Change: The Clathrate Gun Hypothesis. AGU (American Geophysical Union), Washington, DC, pp. 1-9. ISBN 0-87590-296-0
    Publication Date: 2015-09-09
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 3
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    AGU (American Geophysical Union)
    In:  In: Methane Hydrates in Quaternary Climate Change: The Clathrate Gun Hypothesis. AGU (American Geophysical Union), Washington, DC, pp. 105-107. ISBN 0-87590-296-0
    Publication Date: 2015-09-09
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 4
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    PANGAEA
    In:  Supplement to: van Geen, Alexander; Zheng, Y; Bernhard, Joan M; Cannariato, Kevin G; Carriquiry, José D; Dean, Walter E; Eakins, B W; Ortiz, Joseph D; Pike, Jennifer (2003): On the preservation of laminated sediments along the western margin of North America. Paleoceanography, 18(4), 1098, https://doi.org/10.1029/2003PA000911
    Publication Date: 2023-05-12
    Description: Piston, gravity, and multicores as well as hydrographic data were collected along the Pacific margin of Baja California to reconstruct past variations in the intensity of the oxygen-minimum zone (OMZ). Gravity cores collected from within the OMZ north of 24°N did not contain laminated surface sediments even though bottom water oxygen (BWO) concentrations were close to 5 µmol/kg. However, many of the cores collected south of 24°N did contain millimeter- to centimeter-scale, brown to black laminations in Holocene and older sediments but not in sediments deposited during the Last Glacial Maximum. In addition to the dark laminations, Holocene sediments in Soledad Basin, silled at 290 m, also contain white coccolith laminae that probably represent individual blooms. Two open margin cores from 430 and 700 m depth that were selected for detailed radiocarbon dating show distinct transitions from bioturbated glacial sediment to laminated Holocene sediment occurring at 12.9 and 11.5 ka, respectively. The transition is delayed and more gradual (11.3-10.0 ka) in another dated core from Soledad Basin. The observations indicate that bottom-water oxygen concentrations dropped below a threshold for the preservation of laminations at different times or that a synchronous hydrographic change left an asynchronous sedimentary imprint due to local factors. With the caveat that laminated sections should therefore not be correlated without independent age control, the pattern of older sequences of laminations along the North American western margin reported by this and previous studies suggests that multiple patterns of regional productivity and ventilation prevailed over the past 60 kyr.
    Keywords: Age, 14C AMS; Age, 14C calibrated; Age, comment; Age, dated; Age, dated standard error; Calendar age; Calendar age, standard error; Depth, relative; DEPTH, sediment/rock; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; Melville; MUC; MultiCorer; North Pacific/Gulf of California; OXMZ01MV; OXMZ01MV-GC31; OXMZ01MV-GC32; OXMZ01MV-GC38; OXMZ01MV-GC41; OXMZ01MV-MC17; OXMZ01MV-MC19; OXMZ01MV-PC08; OXMZ01MV-PC09; OXMZ01MV-PC10; OXMZ01MV-PC14; PC; Piston corer; Reservoir age; Reservoir age, standard error; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 438 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Cannariato, Kevin G; Kennett, James P; Behl, Richard J (1999): Biotic response to late Quaternary rapid climate switches in Santa Barbara Basin: Ecological and evolutionary implications. Geology, 27(1), 63-66, https://doi.org/10.1130/0091-7613(1999)027%3C0063:BRTLQR%3E2.3.CO;2
    Publication Date: 2024-01-09
    Description: Benthic foraminiferal assemblages from Santa Barbara Basin exhibit major faunal and ecological switches associated with late Quaternary millennial- to decadal-scale global climate oscillations. Repeated turnovers of entire faunas occurred rapidly (〈40-400 yr) without extinction or speciation in conjunction with Dansgaard-Oeschger shifts in thermohaline circulation, ventilation, and climate, confirming evolutionary model predictions of Roy et al. Consistent faunal successions of dysoxic taxa during successive interstadials reflect the extreme sensitivity and adaptation of the benthic ecosystem to the rapid environmental changes that marked the late Quaternary and possibly other transitional intervals in the history of the Earth's ocean-atmosphere-cryosphere system. These data support the hypothesis that broad segments of the biosphere are well adapted to rapid climate change.
    Keywords: 146-893A; AGE; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Foraminifera, benthic; Joides Resolution; Leg146; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 3136 data points
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  • 6
    Publication Date: 2024-01-09
    Keywords: 167-1017E; Age, comment; Age model; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg167; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 66 data points
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  • 7
    Publication Date: 2024-01-09
    Keywords: 167-1017E; Age, 14C AMS; Age, 14C milieu/reservoir corrected; Age, comment; Age, dated; Age, dated standard deviation; Calendar age; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg167; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 78 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Cannariato, Kevin G; Ravelo, Ana Christina (1997): Pliocene-Pleistocene evolution of eastern tropical Pacific surface water circulation and thermocline depth. Paleoceanography, 12(6), 805-820, https://doi.org/10.1029/97PA02514
    Publication Date: 2024-01-09
    Description: We evaluated the response of eastern equatorial Pacific upper water column hydrography to the Panama seaway closure and the initiation of large-scale northern hemisphere glaciation, The d18O gradient between Globorotalia tumida and Globigerinoides sacculifer indicates a general shoaling of the thermocline between 4.2 and 3.0 Ma which may be related to a recorded decrease in southeast trade wind strength. The d13C gradients suggest that surface water nutrient concentrations have increased during the last 5 Myr and that upwelling intermediate waters began to change sources at ~3.2 Ma. Changes in the trans-Pacific east-west temperature and nutrient gradients at 4.0 and 1.5 Ma are coincident with the seaway closure and a major phase of northern hemisphere glaciation. Changes in the sensitivity of surface circulation to Milankovitch forcing, d18O records linearly related to orbital variations only after 3.2 Ma, are associated with the seaway closure. Pleistocene initiation of 100 and 41 kyr cycles in the thermocline depth proxy may suggest that the hydrographic response to Milankovitch forcing is enhanced by air-sea interactions which maintain the relatively steep Pleistocene trans-Pacific gradients. The d13C records are dominated by the 41 kyr period and are usually coherent with high-latitude climate, suggesting that associated changes in the global carbon reservoir dominate the tropical d13C signals.
    Keywords: 138-851; AGE; COMPCORE; Composite Core; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Globigerinoides sacculifer, δ13C; Globigerinoides sacculifer, δ18O; Globorotalia tumida, δ13C; Globorotalia tumida, δ18O; Joides Resolution; Leg138; Mass spectrometer Fisons Optima; Neogloboquadrina dutertrei, δ13C; Neogloboquadrina dutertrei, δ18O; Neogloboquadrina humerosa, δ13C; Neogloboquadrina humerosa, δ18O; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 6521 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Cannariato, Kevin G; Kennett, James P (1999): Climatically related millennial-scale fluctuations in strength of California margin oxygen-minimum zone during the past 60 k.y. Geology, 27(11), 975-978, https://doi.org/10.1130/0091-7613(1999)027%3C0975:CRMSFI%3E2.3.CO;2
    Publication Date: 2024-01-09
    Description: A strong oxygen-minimum zone (OMZ) currently exists along the California margin because of a combination of high surface-water productivity and poor intermediate-water ventilation. However, the strength of this OMZ may have been sensitive to late Quaternary ocean-circulation and productivity changes along the margin. Although sediment-lamination strength has been used to trace ocean-oxygenation changes in the past, oxygen levels on the open margin are not sufficiently low for laminations to form. In these regions, benthic foraminifera are highly sensitive monitors of OMZ strength, and their fossil assemblages can be used to reconstruct past fluctuations. Benthic foraminiferal assemblages from Ocean Drilling Program Site 1017, off Point Conception, exhibit major and rapid faunal oscillations in response to late Quaternary millennial-scale climate change (Dansgaard-Oeschger cycles) on the open central California margin. These faunal oscillations can be correlated to and are apparently synchronous with those reported from Santa Barbara Basin. Together they represent major fluctuations in the strength of the OMZ which were intimately associated with global climate change-weakening, perhaps disappearing, during cool periods and strengthening during warm periods. These rapid, major OMZ strength fluctuations were apparently widespread on the Northeast Pacific margin and must have influenced the evolution of margin biota and altered biogeochemical cycles with potential feedbacks to global climate change.
    Keywords: 167-1017E; AGE; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Foraminifera, benthic; Joides Resolution; Leg167; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 2127 data points
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  • 10
    Publication Date: 2024-01-09
    Keywords: 167-1017E; AGE; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Globigerina bulloides, δ18O; Joides Resolution; Leg167; Mass spectrometer Finnigan MAT 251; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; Uvigerina peregrina curticosta, δ18O
    Type: Dataset
    Format: text/tab-separated-values, 1404 data points
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