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  • ANT-XXVIII/2; ANT-XXVIII/4; ANT-XXVIII/5; BacGeoPac; BAT_SPE; Bering Sea; Canarias Sea; Central Pacific Ocean; CTD/Rosette; CTD-RO; Dissolved Organic Matter; Drake Passage; Equatorial Pacific; Fourier-transform ion cyclotron mass spectrometry; Fourier transform ion cyclotron resonance mass spectrometer (FT-ICR MS, 15 T Bruker Solarix); Global Ocean; HOT_SPE; Lazarev Sea; Mass of molecular formulas; molecular composition; Molecular formula; MUC; MultiCorer; North Atlantic Ocean; North Pacific Ocean; Peak intensity; Polarstern; Pori Bac NewZ; PS79; PS79/035-3; PS79/036-1; PS79/037-1; PS79/038-2; PS79/039-3; PS79/040-2; PS79/041-3; PS79/042-2; PS79/043-2; PS79/044-1; PS79/045-1; PS79/046-3; PS79/048-1; PS79/049-2; PS79/052-2; PS79/053-3; PS79/054-3; PS79/178-1; PS79/179-1; PS79/193-2; PS79/205-1; PS79/217-1; PS79/232-1; PS79/235-3; PS79/241-3; PS79/244-2; PS79/247-1; PS79/251-1; PS79/262-3; PS79/267-1; PS79/277-2; PS79/281-1; PS79/287-2; PS79/296-3; PS79/297-3; PS79/298-3; PS79/300-4; PS79/301-3; PS79/302-4; PS79/304-2; PS79/306-2; PS79/307-4; PS79/308-2; PS79/310-4; PS79/311-2; PS79/312-4; PS79/313-4; PS79/314-4; PS79/315-4; PS79/317-4; PS79/318-4; PS79/319-4; PS79/320-3; PS79/321-4; PS79/322-4; PS79/323-2; PS79/324-4; PS79/328-3; PS79/329-4; Scotia Sea; SO245; SO245_10-1; SO245_1-1; SO245_11-1; SO245_12-2; SO245_13-1; SO245_14-2; SO245_15-2; SO245_2-2; SO245_3-1; SO245_4-1; SO245_5-1; SO245_6-1; SO245_7-4; SO245_8-1; SO245_9-1; SO248; SO248_10-2a; SO248_10-2b; SO248_1-1; SO248_11-1; SO248_12-1; SO248_12-3; SO248_13-3; SO248_14-3; SO248_14-7; SO248_15-1; SO248_16-10; SO248_16-13; SO248_16-15; SO248_16-2; SO248_16-3; SO248_16-5; SO248_17-4; SO248_18-3; SO248_18-5; SO248_19-1; SO248_19-2; SO248_2-1; SO248_2-4; SO248_3-1; SO248_4-1; SO248_4-3; SO248_5-1; SO248_6-1; SO248_6-10; SO248_6-11; SO248_6-13; SO248_6-2; SO248_6-4; SO248_6-5; SO248_7-1; SO248_7-4; SO248_8-2; SO248_8-4; SO248_9-3; SO254; SO254_23-1; SO254_32-1; SO254_38-1; SO254_45-1; SO254_47-1; SO254_59-1; SO254_65-1; Sonne_2; South Atlantic Ocean; South Pacific Ocean; UltraPac, GEOTRACES; Weddell Sea  (1)
  • FT-ICR MS  (1)
Document type
Keywords
Years
  • 1
    Publication Date: 2022-05-27
    Description: Author Posting. © American Geophysical Union, 2021. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Global Biogeochemical Cycles 35(6), (2021): e2021GB006938, https://doi.org/10.1029/2021GB006938.
    Description: As climate-driven El Niño Southern Oscillation (ENSO) events are projected to increase in frequency and severity, much attention has focused on impacts regarding ecosystem productivity and carbon balance in Amazonian rainforests, with comparatively little attention given to carbon dynamics in fluvial ecosystems. In this study, we compared the wet 2012 La Niña period to the following normal hydrologic period in the Amazon River. Elevated water flux during the La Niña period was accompanied by dilution of inorganic ion concentrations. Furthermore, the La Niña period exported 2.77 Tg C yr−1 more dissolved organic carbon (DOC) than the normal period, an increase greater than the annual amount of DOC exported by the Mississippi River. Using ultra-high-resolution mass spectrometry, we detected both intra- and interannual differences in dissolved organic matter (DOM) composition, revealing that DOM exported during the dry season and the normal period was more aliphatic, whereas compounds in the wet season and following the La Niña event were more aromatic, with ramifications for its environmental role. Furthermore, as this study has the highest temporal resolution DOM compositional data for the Amazon River to-date we showed that compounds were highly correlated to a 6-month lag in Pacific temperature and pressure anomalies, suggesting that ENSO events could impact DOM composition exported to the Atlantic Ocean. Therefore, as ENSO events increase in frequency and severity into the future it seems likely that there will be downstream consequences for the fate of Amazon Basin-derived DOM concurrent with lag periods as described here.
    Description: This work was partially supported by National Science Foundation grant OCE-1464396 to Robert G. M. Spencer and funding from the Harbourton Foundation to Robert G. M. Spencer, R. Max Holmes, and Bernhard Peucker-Ehrenbrink.
    Description: 2021-12-11
    Keywords: Amazon river ; carbon cycling ; dissolved organic carbon ; dissolved organic matter ; ENSO ; FT-ICR MS
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-06-12
    Description: This data includes the dissolved organic matter (DOM) molecular composition data obtained via Fourier-transform ion cyclotron resonance mass spectrometry for multiple oceanographic cruises collected in the Atlantic, Pacific and Southern oceans (HOTS, BATS, SO254, SO245, SO248, ANT 28-II, ANT 28-IV, and 28-V) between 2009 and 2017. This analysis was conducted to assess the molecular composition of DOM in the context of ocean mixing. DOM was extracted and desalted using the solid phase extraction method as described in Dittmar et al. 2008. The extracts were stored frozen in methanol until analysis in 2019, when aliquots of the extracts were mixed with 50% ultrapure water (50:50 v/v) and diluted to a final carbon concentration of 2.5 ppm. DOM composition was determined on a SolariX XR FT-ICR-MS (Bruker Daltonik GmbH, Bremen, Germany) equipped with a 15 Tesla superconducting magnet and an electrospray ionization source (ESI; Bruker Apollo II ion source) in negative ion mode, as described in (Bercovici, Dittmar, and Niggemann 2022). Subsequent data processing and molecular formula assignment was conducted in ICBM-OCEAN, as described in (Merder et al. 2020).
    Keywords: ANT-XXVIII/2; ANT-XXVIII/4; ANT-XXVIII/5; BacGeoPac; BAT_SPE; Bering Sea; Canarias Sea; Central Pacific Ocean; CTD/Rosette; CTD-RO; Dissolved Organic Matter; Drake Passage; Equatorial Pacific; Fourier-transform ion cyclotron mass spectrometry; Fourier transform ion cyclotron resonance mass spectrometer (FT-ICR MS, 15 T Bruker Solarix); Global Ocean; HOT_SPE; Lazarev Sea; Mass of molecular formulas; molecular composition; Molecular formula; MUC; MultiCorer; North Atlantic Ocean; North Pacific Ocean; Peak intensity; Polarstern; Pori Bac NewZ; PS79; PS79/035-3; PS79/036-1; PS79/037-1; PS79/038-2; PS79/039-3; PS79/040-2; PS79/041-3; PS79/042-2; PS79/043-2; PS79/044-1; PS79/045-1; PS79/046-3; PS79/048-1; PS79/049-2; PS79/052-2; PS79/053-3; PS79/054-3; PS79/178-1; PS79/179-1; PS79/193-2; PS79/205-1; PS79/217-1; PS79/232-1; PS79/235-3; PS79/241-3; PS79/244-2; PS79/247-1; PS79/251-1; PS79/262-3; PS79/267-1; PS79/277-2; PS79/281-1; PS79/287-2; PS79/296-3; PS79/297-3; PS79/298-3; PS79/300-4; PS79/301-3; PS79/302-4; PS79/304-2; PS79/306-2; PS79/307-4; PS79/308-2; PS79/310-4; PS79/311-2; PS79/312-4; PS79/313-4; PS79/314-4; PS79/315-4; PS79/317-4; PS79/318-4; PS79/319-4; PS79/320-3; PS79/321-4; PS79/322-4; PS79/323-2; PS79/324-4; PS79/328-3; PS79/329-4; Scotia Sea; SO245; SO245_10-1; SO245_1-1; SO245_11-1; SO245_12-2; SO245_13-1; SO245_14-2; SO245_15-2; SO245_2-2; SO245_3-1; SO245_4-1; SO245_5-1; SO245_6-1; SO245_7-4; SO245_8-1; SO245_9-1; SO248; SO248_10-2a; SO248_10-2b; SO248_1-1; SO248_11-1; SO248_12-1; SO248_12-3; SO248_13-3; SO248_14-3; SO248_14-7; SO248_15-1; SO248_16-10; SO248_16-13; SO248_16-15; SO248_16-2; SO248_16-3; SO248_16-5; SO248_17-4; SO248_18-3; SO248_18-5; SO248_19-1; SO248_19-2; SO248_2-1; SO248_2-4; SO248_3-1; SO248_4-1; SO248_4-3; SO248_5-1; SO248_6-1; SO248_6-10; SO248_6-11; SO248_6-13; SO248_6-2; SO248_6-4; SO248_6-5; SO248_7-1; SO248_7-4; SO248_8-2; SO248_8-4; SO248_9-3; SO254; SO254_23-1; SO254_32-1; SO254_38-1; SO254_45-1; SO254_47-1; SO254_59-1; SO254_65-1; Sonne_2; South Atlantic Ocean; South Pacific Ocean; UltraPac, GEOTRACES; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 6762084 data points
    Location Call Number Limitation Availability
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