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  1. Article ; Online: Subsurface ocean warming preceded Heinrich Events.

    Max, Lars / Nürnberg, Dirk / Chiessi, Cristiano M / Lenz, Marlene M / Mulitza, Stefan

    Nature communications

    2022  Volume 13, Issue 1, Page(s) 4217

    Abstract: Although the global environmental impact of Laurentide Ice-Sheet destabilizations on glacial climate during Heinrich Events is well-documented, the mechanism driving these ice-sheet instabilities remains elusive. Here we report foraminifera-based ... ...

    Abstract Although the global environmental impact of Laurentide Ice-Sheet destabilizations on glacial climate during Heinrich Events is well-documented, the mechanism driving these ice-sheet instabilities remains elusive. Here we report foraminifera-based subsurface (~150 m water depth) ocean temperature and salinity reconstructions from a sediment core collected in the western subpolar North Atlantic, showing a consistent pattern of rapid subsurface ocean warming preceding the transition into each Heinrich Event identified in the same core of the last 27,000 years. These results provide the first solid evidence for the massive accumulation of ocean heat near the critical depth to trigger melting of marine-terminating portions of the Laurentide Ice Sheet around Labrador Sea followed by Heinrich Events. The repeated build-up of a subsurface heat reservoir in the subpolar Atlantic closely corresponds to times of weakened Atlantic Meridional Overturning Circulation, indicating a precursor role of ocean circulation changes for initiating abrupt ice-sheet instabilities during Heinrich Events. We infer that a weaker ocean circulation in future may result in accelerated interior-ocean warming of the subpolar Atlantic, which could be critical for the stability of modern, marine-terminating Arctic glaciers and the freshwater budget of the North Atlantic.
    MeSH term(s) Climate ; Foraminifera ; Ice Cover ; Oceans and Seas ; Water Movements
    Language English
    Publishing date 2022-07-21
    Publishing country England
    Document type Journal Article ; Research Support, Non-U.S. Gov't
    ZDB-ID 2553671-0
    ISSN 2041-1723 ; 2041-1723
    ISSN (online) 2041-1723
    ISSN 2041-1723
    DOI 10.1038/s41467-022-31754-x
    Database MEDical Literature Analysis and Retrieval System OnLINE

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  2. Book ; Online: A global climatology of the ocean surface during the Last Glacial Maximum mapped on a regular grid (GLOMAP)

    Paul, André / Mulitza, Stefan / Stein, Rüdiger / Werner, Martin

    eISSN: 1814-9332

    2021  

    Abstract: We present a climatology of the near-sea-surface temperature (NSST) anomaly and the sea-ice extent during the Last Glacial Maximum (LGM, 23 000–19 000 years before present) mapped on a global regular

    Abstract We present a climatology of the near-sea-surface temperature (NSST) anomaly and the sea-ice extent during the Last Glacial Maximum (LGM, 23 000–19 000 years before present) mapped on a global regular <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1</mn><msup><mi/><mo>∘</mo></msup><mo>×</mo><mn mathvariant="normal">1</mn><msup><mi/><mo>∘</mo></msup></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="34pt" height="11pt" class="svg-formula" dspmath="mathimg" md5hash="18e249d247dd6d35235fb683ecd82671"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="cp-17-805-2021-ie00001.svg" width="34pt" height="11pt" src="cp-17-805-2021-ie00001.png"/></svg:svg> grid. It is an extension of the Glacial Atlantic Ocean Mapping (GLAMAP) reconstruction of the Atlantic NSST based on the faunal and floral assemblage data of the Multiproxy Approach for the Reconstruction of the Glacial Ocean Surface (MARGO) project and several recent estimates of the LGM sea-ice extent. Such a gridded climatology is highly useful for the visualization of the LGM climate, calculation of global and regional NSST averages, and estimation of the equilibrium climate sensitivity, as well as a boundary condition for atmospheric general circulation models. The gridding of the sparse NSST reconstruction was done in an optimal way using the Data-Interpolating Variational Analysis (DIVA) software, which takes into account the uncertainty in the reconstruction and includes the calculation of an error field. The resulting Glacial Ocean Map (GLOMAP) confirms the previous findings by the MARGO project regarding longitudinal and meridional NSST differences that were greater than today in all oceans. Taken at face value, the estimated global and tropical cooling would imply an equilibrium climate sensitivity at the lower end of the currently accepted range. However, because of anticipated changes in the seasonality and thermal structure of the upper ocean during the LGM as well as uneven spatial sampling, the estimated cooling and implied climate sensitivity are likely to be biased towards lower values.
    Subject code 551
    Language English
    Publishing date 2021-04-08
    Publishing country de
    Document type Book ; Online
    Database BASE - Bielefeld Academic Search Engine (life sciences selection)

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  3. Article ; Online: Technical note

    Langner, Michael / Mulitza, Stefan

    PaleoDataView – a software toolbox for the collection, homogenization and visualization of marine proxy data

    2019  

    Abstract: We present a software toolbox that allows the efficient collection, management and maintenance of larger paleoceanographic data sets. The program combines a graphical user interface (GUI) with a simple document-based database and functionality for ... ...

    Abstract We present a software toolbox that allows the efficient collection, management and maintenance of larger paleoceanographic data sets. The program combines a graphical user interface (GUI) with a simple document-based database and functionality for visualization, stratigraphy (visual alignment and radiocarbon calibration), age modelling and efficient ensemble time-series generation to create larger homogenous data compilations. Data can be imported from Excel or text files, are stored locally in netCDF format and can be easily exchanged between collaborating scientists. Within a data collection, data can be imported either to proxy-specific sub-collections or to a multi-proxy (“miscellaneous”) sub-collection that allows the import and management of any downcore data. A single age model is shared among all proxies of a core within a collection. The stand-alone software can be used with Windows and macOS and does not require web access. Installers of the current version for both Windows 10 and macOS including the C++ code can be downloaded from https://www.marum.de/Stefan-Mulitza/PaleoDataView.html (last access: 5 December 2019) along with a detailed user guide.
    Subject code 005
    Language English
    Publishing date 2019-12-19
    Publisher Copernicus Publications (EGU)
    Publishing country de
    Document type Article ; Online
    Database BASE - Bielefeld Academic Search Engine (life sciences selection)

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  4. Article ; Online: A global climatology of the ocean surface during the Last Glacial Maximum mapped on a regular grid (GLOMAP)

    Paul, André / Mulitza, Stefan / Stein, Rüdiger / Werner, Martin

    2021  

    Abstract: We present a climatology of the near-sea-surface temperature (NSST) anomaly and the sea-ice extent during the Last Glacial Maximum (LGM, 23 000–19 000 years before present) mapped on a global regular 1∘×1∘ grid. It is an extension of the Glacial Atlantic ...

    Abstract We present a climatology of the near-sea-surface temperature (NSST) anomaly and the sea-ice extent during the Last Glacial Maximum (LGM, 23 000–19 000 years before present) mapped on a global regular 1∘×1∘ grid. It is an extension of the Glacial Atlantic Ocean Mapping (GLAMAP) reconstruction of the Atlantic NSST based on the faunal and floral assemblage data of the Multiproxy Approach for the Reconstruction of the Glacial Ocean Surface (MARGO) project and several recent estimates of the LGM sea-ice extent. Such a gridded climatology is highly useful for the visualization of the LGM climate, calculation of global and regional NSST averages, and estimation of the equilibrium climate sensitivity, as well as a boundary condition for atmospheric general circulation models. The gridding of the sparse NSST reconstruction was done in an optimal way using the Data-Interpolating Variational Analysis (DIVA) software, which takes into account the uncertainty in the reconstruction and includes the calculation of an error field. The resulting Glacial Ocean Map (GLOMAP) confirms the previous findings by the MARGO project regarding longitudinal and meridional NSST differences that were greater than today in all oceans. Taken at face value, the estimated global and tropical cooling would imply an equilibrium climate sensitivity at the lower end of the currently accepted range. However, because of anticipated changes in the seasonality and thermal structure of the upper ocean during the LGM as well as uneven spatial sampling, the estimated cooling and implied climate sensitivity are likely to be biased towards lower values.
    Subject code 551
    Language English
    Publishing date 2021-04-08
    Publisher Copernicus Publications (EGU)
    Publishing country de
    Document type Article ; Online
    Database BASE - Bielefeld Academic Search Engine (life sciences selection)

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  5. Book: Climate history and sedimentation processes off NW Africa

    Mulitza, Stefan

    cruise no. 65 ; June 11 - August 10, 2005, Dakar (Senegal) - Las Palmas (Spain)

    (Meteor-Berichte ; [20]08,2)

    2008  

    Institution Leitstelle Meteor, Maria S. Merian
    Author's details Leitstelle METEOR, Institut für Meereskunde der Universität Hamburg. Stefan Mulitza
    Series title Meteor-Berichte ; [20]08,2
    Language English
    Size Getr. Zählung, Ill., graph. Darst., Kt.
    Publishing place Hamburg
    Document type Book
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  6. Article ; Online: Molecular distribution and isotopic composition (δD and δ

    Rozo, Laura / Lazzari, Leticia / Schefuß, Enno / Mulitza, Stefan / Carreira, Renato

    Data in brief

    2020  Volume 33, Page(s) 106508

    Abstract: The distribution and isotopic composition ( ... ...

    Abstract The distribution and isotopic composition (δ
    Language English
    Publishing date 2020-11-06
    Publishing country Netherlands
    Document type Journal Article
    ZDB-ID 2786545-9
    ISSN 2352-3409 ; 2352-3409
    ISSN (online) 2352-3409
    ISSN 2352-3409
    DOI 10.1016/j.dib.2020.106508
    Database MEDical Literature Analysis and Retrieval System OnLINE

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  7. Article: Molecular distribution and isotopic composition (δD and δ13C) of lipids dataset for a sediment core (GeoB16202-2) from the north-eastern Brazilian margin

    Rozo, Laura / Lazzari, Leticia / Schefuß, Enno / Mulitza, Stefan / Carreira, Renato

    Data in Brief. 2020 Dec., v. 33

    2020  

    Abstract: The distribution and isotopic composition (δ¹³C and δD) of lipids are proxies used to determinate paleoenvironmental conditions including precipitation regimes, vegetation changes and sources of organic matter, among others. This data article describes ... ...

    Abstract The distribution and isotopic composition (δ¹³C and δD) of lipids are proxies used to determinate paleoenvironmental conditions including precipitation regimes, vegetation changes and sources of organic matter, among others. This data article describes five datasets of distribution (n-alkanes, fatty acids, n-alkanols and sterols) and isotopic composition (n-alkanes and fatty acids) of lipids determined in 50 samples from a gravity core (GeoB16202–2) retrieved on the continental slope off northeastern Brazil. The core site is influenced by the Parnaiba freshwater discharge, the North Brazil Current and by the Intertropical Convergence Zone (ITCZ). Previous work focused on inorganic proxies in this core revealed important clues of climatic conditions during the Heinrich Stadial 1 (HS1). The baseline dataset of molecular and isotopic proxies of the organic matter provided here are additional and/or complimentary evidences to help elucidate past climate change during the Quaternary in the Equatorial Atlantic, where less information is available in comparison to other regions in this ocean.
    Keywords alkanes ; climate change ; data collection ; freshwater ; gravity ; organic matter ; paleoecology ; sediments ; sterols ; vegetation ; Brazil
    Language English
    Dates of publication 2020-12
    Publishing place Elsevier Inc.
    Document type Article
    ZDB-ID 2786545-9
    ISSN 2352-3409
    ISSN 2352-3409
    DOI 10.1016/j.dib.2020.106508
    Database NAL-Catalogue (AGRICOLA)

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  8. Book ; Online: A global climatology of the ocean surface during the Last Glacial Maximum mapped on a regular grid (GLOMAP)

    Paul, André / Mulitza, Stefan / Stein, Rüdiger / Werner, Martin

    eISSN: 1814-9332

    2020  

    Abstract: We present a climatology of the sea-surface temperature (SST) anomaly and the sea-ice extent during the Last Glacial Maximum (LGM, 23 000–19 000 years before present) mapped on a global regular 1° × 1° grid. It is an extension of the Glacial Atlantic ... ...

    Abstract We present a climatology of the sea-surface temperature (SST) anomaly and the sea-ice extent during the Last Glacial Maximum (LGM, 23 000–19 000 years before present) mapped on a global regular 1° × 1° grid. It is an extension of the Glacial Atlantic Ocean Mapping (GLAMAP) reconstruction of the Atlantic SST based on the results of the Multiproxy Approach for the Reconstruction of the Glacial Ocean Surface (MARGO) project and several recent estimates of the LGM sea-ice extent. Such a gridded climatology is highly useful for the visualization of the LGM climate, calculation of global and regional SST averages and estimation of the equilibrium climate sensitivity, as well as a boundary condition for atmospheric general circulation models. The gridding of the sparse SST reconstruction was done in an optimal way using the Data-Interpolating Variational Analysis (DIVA) software, which takes into account the uncertainty on the reconstruction and includes the calculation of an error field. The resulting Glacial Ocean Map (GLOMAP) confirmed the previous findings by the MARGO project regarding longitudinal and meridional SST differences that were greater than today in all oceans and an equilibrium climate sensitivity at the lower end of the currently accepted range.
    Subject code 551
    Language English
    Publishing date 2020-02-19
    Publishing country de
    Document type Book ; Online
    Database BASE - Bielefeld Academic Search Engine (life sciences selection)

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  9. Book: Report and preliminary results of Meteor-Cruise M65/1, Dakar - Dakar, 11.06. - 1.07.2005

    Mulitza, Stefan

    (Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen ; 252)

    2006  

    Author's details Mulitza, S
    Series title Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen ; 252
    Keywords Meereskunde ; Meteor ; Expedition ; Meeresgeologie ; Kontinentalabhang ; Atlantischer Ozean ; Westafrika
    Language English
    Size 151 S., graph. Darst., Kt.
    Publisher Fachbereich Geowiss., Univ
    Publishing place Bremen
    Document type Book
    Note Literaturverz. S. [153] - [165]
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  10. Article ; Online: Subsurface ocean warming preceded Heinrich Events

    Max, Lars / Nürnberg, Dirk / Chiessi, Cristiano M. / Lenz, Marlene M. / Mulitza, Stefan

    2022  

    Abstract: Although the global environmental impact of Laurentide Ice-Sheet destabilizations on glacial climate during Heinrich Events is well-documented, the mechanism driving these ice-sheet instabilities remains elusive. Here we report foraminifera-based ... ...

    Abstract Although the global environmental impact of Laurentide Ice-Sheet destabilizations on glacial climate during Heinrich Events is well-documented, the mechanism driving these ice-sheet instabilities remains elusive. Here we report foraminifera-based subsurface (~150 m water depth) ocean temperature and salinity reconstructions from a sediment core collected in the western subpolar North Atlantic, showing a consistent pattern of rapid subsurface ocean warming preceding the transition into each Heinrich Event identified in the same core of the last 27,000 years. These results provide the first solid evidence for the massive accumulation of ocean heat near the critical depth to trigger melting of marine-terminating portions of the Laurentide Ice Sheet around Labrador Sea followed by Heinrich Events. The repeated build-up of a subsurface heat reservoir in the subpolar Atlantic closely corresponds to times of weakened Atlantic Meridional Overturning Circulation, indicating a precursor role of ocean circulation changes for initiating abrupt ice-sheet instabilities during Heinrich Events. We infer that a weaker ocean circulation in future may result in accelerated interior-ocean warming of the subpolar Atlantic, which could be critical for the stability of modern, marine-terminating Arctic glaciers and the freshwater budget of the North Atlantic.
    Language English
    Publishing date 2022-07-21
    Publisher Nature Research
    Publishing country de
    Document type Article ; Online
    Database BASE - Bielefeld Academic Search Engine (life sciences selection)

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