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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Bolton, Clara T; Bailey, Ian; Friedrich, Oliver; Tachikawa, Kazuyo; de Garidel-Thoron, Thibault; Vidal, Laurence; Sonzogni, Corinne; Marino, Gianluca; Rohling, Eelco J; Robinson, Marci M; Ermini, Magali; Koch, Mirjam C; Cooper, Matthew J; Wilson, Paul A (2018): North Atlantic Midlatitude Surface‐Circulation Changes Through the Plio‐Pleistocene Intensification of Northern Hemisphere Glaciation. Paleoceanography and Paleoclimatology, 33(11), 1186-1205, https://doi.org/10.1029/2018PA003412
    Publication Date: 2023-07-05
    Description: The North Atlantic Current (NAC) transports warm salty water to high northern latitudes, with important repercussions for ocean circulation and global climate. A southward displacement of the NAC and Subarctic Front, which separate subpolar and subtropical water masses, is widely suggested for the last glacial maximum (LGM) and may have acted as a positive feedback in glacial expansion at this time. However, the role of the NAC during the intensification of northern hemisphere glaciation (iNHG) ~3.5 to 2.5 Ma, is less clear. Here, we present new records from IODP Site U1313 (41°N) spanning ~2.8-2.4 Ma to trace the influence of Subarctic Front waters above this mid-latitude site. We reconstruct surface and permanent pycnocline temperatures and seawater δ18O using paired Mg/Ca-δ18O measurements on the planktic foraminifers Globigerinoides ruber and Globorotalia crassaformis, and determine abundances of the subpolar foraminifer Neogloboquadrina atlantica. We find that the first significant glacial incursions of Subarctic Front surface waters above Site U1313 did not occur until ~2.6 Ma. At no time during our study interval was (sub)surface reorganisation in the mid-latitude North Atlantic analogous to the LGM. Our findings suggest that LGM-like processes sensu stricto cannot be invoked to explain interglacial-glacial cycle amplification during iNHG. They also imply that increased glacial productivity at Site U1313 during iNHG was not only driven by southward deflections of the Subarctic Front. We suggest nutrient injection from cold-core eddies and enhanced glacial dust delivery may have played additional roles in increasing export productivity in the mid-latitude North Atlantic from 2.7 Ma.
    Keywords: Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 2
    Publication Date: 2023-12-02
    Keywords: 306-U1313; after Bolton etal., 2010; AGE; COMPCORE; Composite Core; Counting 〉150 µm fraction; Depth, composite; Exp306; Foraminifera, planktic, other; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Neogloboquadrina atlantica; North Atlantic Climate 2; Sample comment
    Type: Dataset
    Format: text/tab-separated-values, 789 data points
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  • 3
    Publication Date: 2023-12-02
    Keywords: 306-U1313; after Bolton etal., 2010; AGE; COMPCORE; Composite Core; Depth, composite; Exp306; Globigerinoides ruber, Magnesium/Calcium ratio; Globigerinoides ruber, δ18O; Globorotalia crassaformis, Magnesium/Calcium ratio; Globorotalia crassaformis, δ18O; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; North Atlantic Climate 2; Sea surface temperature; Thermocline water temperature
    Type: Dataset
    Format: text/tab-separated-values, 6707 data points
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  • 4
    Publication Date: 2024-01-09
    Keywords: 198-1210B; AGE; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg198; Mass spectrometer, Finnigan, MAT 253; North Pacific Ocean; Nuttallides truempyi, δ13C; Nuttallides truempyi, δ18O; Ocean Drilling Program; ODP; Rugoglobigerina rugosa, δ13C; Rugoglobigerina rugosa, δ18O; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 2170 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Koch, Mirjam C; Friedrich, Oliver (2012): Campanian-Maastrichtian intermediate- to deep-water changes in the high latitudes: Benthic foraminiferal evidence. Paleoceanography, 27(2), PA2209, https://doi.org/10.1029/2011PA002259
    Publication Date: 2024-01-09
    Description: During the latest Cretaceous cooling phase, a positive shift in benthic foraminiferal d18O values lasting about 1.5 Myr (71.5-70 Ma) can be observed at a global scale (Campanian-Maastrichtian Boundary Event, CMBE). This d18O excursion is interpreted as being influenced by a change in intermediate- to deep-water circulation or by temporal build-up of Antarctic ice sheets. Here we test whether benthic foraminiferal assemblages from a southern high-latitudinal site near Antarctica (ODP Site 690) are influenced by the CMBE. If the d18O transition reflects a change in intermediate- to deep-water circulation from low-latitude to high-latitude water masses, then this change would result in cooler temperatures, higher oxygen concentration, and possibly lower organic-matter flux at the seafloor, resulting in a major benthic foraminiferal assemblage change. If, however, the d18O transition was mainly triggered by ice formation, no considerable compositional difference in benthic foraminiferal assemblages would be expected. Our data show a separation of the studied succession into two parts with distinctly different benthic foraminiferal assemblages. Species dominating the older part (73.0-70.5 Ma) tolerate less bottom water oxygenation and are typical components of low-latitude assemblages. In contrast, the younger part (70.0-68.0 Ma) is characterized by species that indicate well-oxygenated bottom waters and species common in high-latitude assemblages. We interpret the observed change in benthic foraminiferal assemblages toward a well-oxygenated environment to reflect the onset of a shift from low-latitude toward high-latitude dominated intermediate- to deep-water sources. This implies that a change in oceanic circulation was at least a major component of the CMBE.
    Keywords: 113-690C; AGE; Alabamina sp.; Allomorphina cf. navarroana; Allomorphina minuta; Allomorphina sp.; Allomorphina trochoides; Angulogavelinella sp.; Aragonia velascoensis; Arenobulimina preslii; Arenobulimina sp.; Astacolus cretaceus; Astacolus sp.; Ataxophragmium rimosum; Biedafranciszkina polonica; Bolivina incrassata; Bolivina sp.; Bolivina witwickae; Bolivinoides paleocenicus; Bulimina sp.; Buliminella cf. excavata; Chrysalogonium tenuistriatum; Cibicides cf. excavata; Cibicidoides bembix; Cibicidoides sp.; Cibicidoides velascoensis; Cibicidoides voltzianus; Counting 〉125 µm fraction; Cuneus minutus; Cuneus trigona; Dentalina sp.; Dentalina sulcata; DEPTH, sediment/rock; Dorothia oxycona; Dorothia pupa; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Ellipsodimorphina hrubieszowcensis; Ellipsodimorphina sp.; Ellipsodimorphina variabilis; Ellipsoidella gracillima; Ellipsoidella kugleri; Ellipsoidella pleurostomelloides; Ellipsoidella polonica; Ellipsoidella sp.; Ellipsoidella variabilis; Epistominella alata; Eponides beisseli; Eponides concinna; Eponides sp.; Fissurina laticarinata; Fissurina orbignyana; Fissurina sp.; Foraminifera, benthic; Frondicularia frankei; Frondicularia lineata; Frondicularia sp.; Gaudryina pyramidata; Gaudryina sp.; Gavelinella beccariiformis; Gavelinella brotzeni; Gavelinella lorneiana; Gavelinella monterelensis; Gavelinella multipunctata; Gavelinella sp.; Globobulimina sp.; Globorotalites conicus; Globorotalites sp.; Globorotalites subconicus; Globulina lacrima; Globulina prisca; Globulina pseudopupa; Globulina subsphaerica; Guttulina cretacea; Guttulina pseudoscripta; Guttulina sp.; Guttulina trigonula; Gyroidina parva; Gyroidina sp.; Gyroidinoides lenticulus; Gyroidinoides nitidus; Gyroidinoides quadratus; Gyroidinoides tellburnaensis; Gyroidinoides umbilicatus; Joides Resolution; Laevidentalina catenula; Laevidentalina cf. siliqua; Laevidentalina communis; Laevidentalina concinna; Laevidentalina distincta; Laevidentalina monile; Laevidentalina oligostegia; Laevidentalina pseudonana; Laevidentalina soluta; Laevidentalina sp.; Lagena cf. grahami; Lagena paucicosta; Lagena semiinterrupta; Lagena semilineata; Lagena sp.; Lagena sulcatiformis; Lagena tricostulata; Leg113; Lenticulina cf. adenalensis; Lenticulina mariae; Lenticulina rotulata; Lingulina sp.; Marginulina loisana; Marginulina sp.; Milliammina spp.; Neoflabellina permutata; Neoflabellina reticulata; Neoflabellina rugosa; Neoflabellina sp.; Nodogenerina pseudoscripta; Nodosaria aspera; Nodosaria velascoensis; Nonion sp.; Nuttallides sp.; Nuttallides truempyi; Nuttallinella florealis; Ocean Drilling Program; ODP; Oolina globosa; Oolina sp.; Oolina sphaerica; Orbignyna ovata; Oridorsalis spp.; Osangularia cordieriana; Osangularia navarroana; Paralabamina hillebrandti; Paralabamina lunata; Paralabamina sp.; Paratrochamminoides sp.; Patellina trochiformis; Pleurostomella nitida; Pleurostomella subnodosa; Praebulimina pusilla; Praebulimina sp.; Praebulimina ventricosa; Procerolagena cylindrica; Pseudonodosaria manifesta; Pseudonodosaria sp.; Pullenia jarvisi; Pullenia marssoni; Pullenia reussi; Pyramidulina majuscula; Pyrolinoides acuminatus; Quadrimorphina allomorphinoides; Quadrimorphina camerata; Ramulina aculeata; Ramulina sp.; Reussella szajnochae; Reussoolina apiculata; Reussoolina simplex; Rosalina spp.; Rotaliidae; Sample code/label; Saracenaria cf. erlita; Saracenaria cf. navicula; Saracenaria sp.; Saracenaria triangularis; Sitella sp.; South Atlantic Ocean; Spiroplectammina sp.; Svenia laevigata; Trochammina sp.; Vaginulina trilobata
    Type: Dataset
    Format: text/tab-separated-values, 20881 data points
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  • 6
    Publication Date: 2024-01-09
    Keywords: 198-1210B; AGE; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg198; Neodymium-143/Neodymium-144 ratio; Neodymium-143/Neodymium-144 ratio, error; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, error; ε-Neodymium (0); ε-Neodymium (T)
    Type: Dataset
    Format: text/tab-separated-values, 272 data points
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  • 7
    Publication Date: 2024-01-09
    Keywords: 198-1210B; AGE; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg198; Neodymium-143/Neodymium-144 ratio; Neodymium-143/Neodymium-144 ratio, error; North Pacific Ocean; Ocean Drilling Program; ODP; Sample code/label; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, error; ε-Neodymium (0)
    Type: Dataset
    Format: text/tab-separated-values, 101 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Jung, Claudia; Voigt, Silke; Friedrich, Oliver; Koch, Mirjam C; Frank, Martin (2013): Campanian-Maastrichtian ocean circulation in the tropical Pacific. Paleoceanography, 28(3), 562-573, https://doi.org/10.1002/palo.20051
    Publication Date: 2024-01-09
    Description: The Pacific Ocean is the largest water body on Earth, and circulation in the Pacific contributed significantly to climate evolution in the latest Cretaceous, the culmination of a period of long-term cooling. Here, we present new high-resolution late Campanian to Maastrichtian benthic and planktic foraminiferal stable isotope data and a neodymium (Nd) isotope record obtained from sedimentary ferromanganese oxide coatings of Ocean Drilling Program Hole 1210B from the tropical Pacific Ocean (Shatsky Rise). These new records resolve 13 million years in the latest Cretaceous, providing insights into changes in surface and bottom water temperatures and source regions of deep to intermediate waters covering the carbon isotope excursions of the Campanian-Maastrichtian Boundary Event (CMBE) and the Mid-Maastrichtian event (MME). Our new benthic foraminiferal d18O and Nd isotope records together with published Nd isotope data show markedly parallel trends across the studied interval over a broad range of bathyal to abyssal water depths interpreted to reflect changes in the intensity of deep-ocean circulation in the tropical Pacific. In particular, we observe a three-million-year-long period of cooler conditions in the early Maastrichtian (72.5 to 69.5 Ma) when a concomitant change toward less radiogenic seawater Nd isotope signatures probably marks a period of enhanced admixture and northward flow of deep waters with Southern Ocean provenance. We suggest this change to have been triggered by intensified formation and convection of deep waters in the high southern latitudes, a process that weakened during the MME (69.5 to 68.5 Ma). The early Maastrichtian cold interval is closely related to the negative and positive carbon isotope trends of the CMBE and MME. The millions-of-years long duration of these carbon cycle perturbations suggests a tectonic forcing of climatic cooling, possibly related to changes in ocean basin geometry and bathymetry.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 9
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    PANGAEA
    In:  Supplement to: Weinkauf, Manuel F G; Moller, Tobias F; Koch, Mirjam C; Kucera, Michal (2014): Disruptive selection and bet-hedging in planktonic Foraminifera: shell morphology as predictor of extinctions. Frontiers in Ecology and Evolution, 2, https://doi.org/10.3389/fevo.2014.00064
    Publication Date: 2024-02-15
    Description: Extinction is a remarkably difficult phenomenon to study under natural conditions. This is because the outcome of stress exposure and associated fitness reduction is not known until the extinction occurs and it remains unclear whether there is any phenotypic reaction of the exposed population that can be used to predict its fate. Here we take advantage of the fossil record, where the ecological outcome of stress exposure is known. Specifically, we analyze shell morphology of planktonic Foraminifera in sediment samples from the Mediterranean, during an interval preceding local extinctions. In two species representing different plankton habitats, we observe shifts in trait state and decrease in variance in association with non-terminal stress, indicating stabilizing selection. At terminal stress levels, immediately before extinction, we observe increased growth asymmetry and trait variance, indicating disruptive selection and bet-hedging. The pre-extinction populations of both species show a combination of trait states and trait variance distinct from all populations exposed to non-terminal levels of stress. This finding indicates that the phenotypic history of a population may allow the detection of threshold levels of stress, likely to lead to extinction. It is thus an alternative to population dynamics in studying and monitoring natural population ecology.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 10
    Publication Date: 2024-02-15
    Keywords: 567; AGE; Center for Marine Environmental Sciences; Coefficient of determination; DEPTH, sediment/rock; Gravity corer (Kiel type); M51/3; M51/3_567_SL104; MARUM; Meteor (1986); Regression dip; Regression intercept; Sample code/label; SL
    Type: Dataset
    Format: text/tab-separated-values, 2568 data points
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