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  • Nature Publishing Group  (561)
  • Blackwell Publishing Ltd  (482)
  • American Chemical Society (ACS)
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  • 11
    Publication Date: 2011-10-05
    Description: Analytical Chemistry DOI: 10.1021/ac201237r
    Print ISSN: 0003-2700
    Electronic ISSN: 1520-6882
    Topics: Chemistry and Pharmacology
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  • 12
    Publication Date: 2013-03-07
    Description: Analytical Chemistry DOI: 10.1021/ac303522h
    Print ISSN: 0003-2700
    Electronic ISSN: 1520-6882
    Topics: Chemistry and Pharmacology
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  • 13
    Publication Date: 2014-12-25
    Description: Journal of the American Chemical Society DOI: 10.1021/ja510998s
    Print ISSN: 0002-7863
    Electronic ISSN: 1520-5126
    Topics: Chemistry and Pharmacology
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  • 14
    Publication Date: 2023-03-14
    Keywords: Alkalinity, total; Autotitrator Metrohm 785 and electrode; Barium/Calcium ratio; Barium/Calcium ratio, standard deviation; Comment; Experiment; ICP-MS, Agilent 7500-ce; Number of observations; pH; Strontium-86/Strontium-88, standard deviation; Strontium-86/Strontium-88 ratio; Strontium-87/Strontium-88, standard deviation; Strontium-87/Strontium-88 ratio; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 98 data points
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  • 15
    Publication Date: 2023-03-14
    Keywords: Barium/Calcium ratio; Experiment; ICP-MS, Agilent 7500-ce; LA-ICP-MS, Laser-ablation inductively coupled plasma mass spectrometer; Neogloboquadrina dutertrei, Barium/Calcium ratio; pH; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 325 data points
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  • 16
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    PANGAEA
    In:  Supplement to: Baxter, Allix J; Hopmans, Ellen C; Russell, James M; Sinninghe Damsté, Jaap S (2019): Bacterial GMGTs in East African lake sediments: Their potential as palaeotemperature indicators. Geochimica et Cosmochimica Acta, 259, 155-169, https://doi.org/10.1016/j.gca.2019.05.039
    Publication Date: 2023-03-14
    Description: Glycerol monoalkyl glycerol tetraethers (GMGTs) are a group of membrane spanning lipids produced by some species of archaea and bacteria. They differ from the more commonly studied glycerol dialkyl glycerol tetraethers (GDGTs) in having an additional covalent carbon-carbon bond connecting the two alkyl chain. The relative abundance and distribution of bacterial branched GMGTs (brGMGTs) in surface sediments from a set of East African lakes were studied. The abundance of brGMGTs relative to the brGDGTs is positively correlated to measured mean annual air temperature (MAAT), although with a significant amount of scatter. BrGMGT abundance was not correlated to lake water pH. Seven major brGMGTs that vary in degree of methylation were identified, with m/z 1020, 1034 and 1048. Further, the mass chromatograms of the m/z 1020 and 1034 brGMGTs show an interesting distribution of peaks, which likely relates to the occurrence of distinct brGMGT isomers. This structural complexity is higher than previously observed in peats and marine sediments. Principal component analysis of the fractional abundance of bacterial tetraether lipids revealed the brGMGTs behave similarly to one another but differently from both the 5- or 6-methyl brGDGTs. This suggests the brGMGTs are produced by a common source organism and are methylated at a different position. The distribution of the seven brGMGTs showed considerable correlation with MAAT. This variability was captured in a new proxy index (the brGMGTI), which showed a strong positive linear relationship with MAAT. Lacustrine brGMGTs show potential to be applied to ancient settings to provide information about paleoclimate.
    Keywords: Albert_Lake; Bandara_Lake; Batoda_Lake; Bigata_Lake; Branched glycerol dialkyl glycerol tetraether, Ia; Branched glycerol dialkyl glycerol tetraether, Ia (peak area); Branched glycerol dialkyl glycerol tetraether, Ib; Branched glycerol dialkyl glycerol tetraether, Ib (peak area); Branched glycerol dialkyl glycerol tetraether, Ic; Branched glycerol dialkyl glycerol tetraether, Ic (peak area); Branched glycerol dialkyl glycerol tetraether, IIa; Branched glycerol dialkyl glycerol tetraether, IIa'; Branched glycerol dialkyl glycerol tetraether, IIa' (peak area); Branched glycerol dialkyl glycerol tetraether, IIa (peak area); Branched glycerol dialkyl glycerol tetraether, IIb; Branched glycerol dialkyl glycerol tetraether, IIb'; Branched glycerol dialkyl glycerol tetraether, IIb' (peak area); Branched glycerol dialkyl glycerol tetraether, IIb (peak area); Branched glycerol dialkyl glycerol tetraether, IIIa; Branched glycerol dialkyl glycerol tetraether, IIIa'; Branched glycerol dialkyl glycerol tetraether, IIIa' (peak area); Branched glycerol dialkyl glycerol tetraether, IIIa (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1020a; Branched glycerol monoalkyl glycerol tetraethers, H1020a (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1020b; Branched glycerol monoalkyl glycerol tetraethers, H1020b (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1020c; Branched glycerol monoalkyl glycerol tetraethers, H1020c (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1034a; Branched glycerol monoalkyl glycerol tetraethers, H1034a (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1034b; Branched glycerol monoalkyl glycerol tetraethers, H1034b (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1034c; Branched glycerol monoalkyl glycerol tetraethers, H1034c (peak area); Branched glycerol monoalkyl glycerol tetraethers, H1048; Branched glycerol monoalkyl glycerol tetraethers, H1048 (peak area); Bugwagi_Lake; Bukurungu_East_Lake; Central_Lake; Chibwera_Lake; Country; Crane_Lake; DEPTH, water; Dimtu_Lake; Edward_Lake; Elevation of event; Enchanted_Lake__Lake; Event label; Gallery_Tarn_Lake; Garba_Gurach_Lake; GDGTs; GMGT; Hanging_Tarn_Lake; Hara_Laki_Lake; Hara_Lucas_Lake; Haro_Lakota_Lake; Harris_Tarn_Lake; Hausburg_Tarn_Lake; H-GDGT; Hut_Tarn_Lake; Ibamba_Lake; Kacuba_Lake; Kako_Lake; Kamweru_Lake; Kanyabutetere_Lake; Kanyanchu_Lake; Kasirya_Lake; Katanda_Lake; Katunda_Lake; Kifuruka_Lake; Kisibendi_Lake; Kitere_Lake; Kopello_Lake; Koromi_Lake; Kuware_Lake; Kyasunduka_Lake; Kyerbwato_Lake; Kyogo_Lake; Lake; Lake_Ellis; lakes; Lake surface area; Large_Hall_Tarn_Lake; Latitude of event; Longitude of event; Lower_Kachope_Lake; Lower_Simba_Lake; Mahoma_Lake; Mahuhura_Lake; Mbayo_Lake; membrane lipids; Middle_Kachope_Lake; Mirambi_Lake; MULT; Multiple investigations; Murabio_Lake; Murusi_Lake; Mwengenyi_Lake; Nanyuki_Tarn_Lake; NIOZ_UU; NIOZ Royal Netherlands Institute for Sea Research, and Utrecht University; Njarayabana_Lake; Nkuruba_Lake; Nyamugosani_Lake; Nyamusingere_Lake; Nyantonde_Lake; Oblong_Tarn_Lake; palaeotemperature; pH; Ruhandika_Lake; Rutundu_Lake; sediments; Small_Hall_Tarn_Lake; Square_Tarn_Lake; Sum; Tanganyika_Lake; Teleki_Tarn_Lake; Temperature, air, annual mean; Temperature, water; tetraethers; Thompson_Lake_Lake; Togona_Lake; Veggi_Tarn_Lake; Wandakara_Lake; Wankenzi_Lake
    Type: Dataset
    Format: text/tab-separated-values, 2991 data points
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  • 17
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    PANGAEA
    In:  Supplement to: McDuff, Russell E (1984): The chemistry of interstitial waters from the upper ocean crust, Site 395, Deep Sea Drilling Project Leg 78B. In: Hyndman, RD; Salisbury, MH; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 78B, 795-799, https://doi.org/10.2973/dsdp.proc.78b.114.1984
    Publication Date: 2023-05-12
    Description: Chemical analysis of fluids sampled in situ during Leg 78B has been carried out. The fluids found in Hole 395A upon reoccupation of the site after a five-year hiatus were identical in composition to local bottom seawater to depths of at least 400 meters, suggesting drawdown. No local bottom-water component is present at 543 meters however. The chemistry of this deep sample shows a large depletion in magnesium, with charge balance maintained by sodium, rather than calcium, enrichment. Calcium is lost through calcite precipitation. A sediment interstitial-water sample from the offset Hole 395B has a chemical signature indicative of glacial influence, thereby constraining drawdown through the sediments to a velocity less than 0.5 cm/y.
    Keywords: Deep Sea Drilling Project; DSDP
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 18
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    PANGAEA
    In:  Supplement to: Tierney, Jessica E; Oppo, Delia W; Rosenthal, Yair; Russell III, James M; Linsley, Braddock K (2010): Coordinated hydrological regimes in the Indo-Pacific region during the past two millennia. Paleoceanography, 25(1), PA1102, https://doi.org/10.1029/2009PA001871
    Publication Date: 2023-05-12
    Description: Instrumental data suggest that major shifts in tropical Pacific atmospheric dynamics and hydrology have occurred within the past century, potentially in response to anthropogenic warming. To better understand these trends, we use the hydrogen isotopic ratios of terrestrial higher plant leaf waxes (DDwax) in marine sediments from southwest Sulawesi, Indonesia, to compile a detailed reconstruction of central Indo-Pacific Warm Pool (IPWP) hydrologic variability spanning most of the last two millennia. Our paleodata are highly correlated with a monsoon reconstruction from Southeast Asia, indicating that intervals of strong East Asian summer monsoon (EASM) activity are associated with a weaker Indonesian monsoon (IM). Furthermore, the centennial-scale oscillations in our data follow known changes in Northern Hemisphere climate (e.g., the Little Ice Age and Medieval Warm Period) implying a dynamic link between Northern Hemisphere temperatures and IPWP hydrology. The inverse relationship between the EASM and IM suggests that migrations of the Intertropical Convergence Zone and associated changes in monsoon strength caused synoptic hydrologic shifts in the IPWP throughout most of the past two millennia.
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 19
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    PANGAEA
    In:  Supplement to: Russell, Ann D; Spero, Howard J (2000): Field examination of the oceanic carbonate ion effect on stable isotopes in planktonic foraminifera. Paleoceanography, 15(1), 43-52, https://doi.org/10.1029/1998PA000312
    Publication Date: 2023-05-12
    Description: We determined the d18O and d13C of individual Globigerinoides ruber and Pulleniatina obliquiloculata from sediment traps located from 5°N to 12°S along 140°W in the Pacific Ocean to evaluate the effects of varying [CO3=] on shell d18O and d13C. Variations in the offset between shell d13C and d13CDIC (Dd13Cs-DIC) are attributed to differences in [CO3]2-, temperature, and shell size between sample sites. When Dd13Cs-DIC of G. ruber was corrected for variations in [CO3]2- using the experimental slope of Bijma et al. (1998), the residual Dd13Cs-DIC was correlated with mixed layer temperature (+0.10±0.04 per mil °C**-1). The slope of this temperature effect is consistent with experimental results. In P. obliquiloculata, Dd13Cs-DIC and temperature were strongly anticorrelated (−0.14±0.03 per mil C**-1). We are unable to separate the influences of [CO3]2- and temperature in this species without independent experimental data. Correcting for [CO3]2- variability on d18Os of G. ruber improves the accuracy of estimated sea surface temperatures.
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 20
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    PANGAEA
    In:  Supplement to: Hastings, D; Russell, Ann D; Emerson, Steven R (1998): Foraminiferal magnesium in Globeriginoides sacculifer as a paleotemperature proxy. Paleoceanography, 13(2), 161-169, https://doi.org/10.1029/97PA03147
    Publication Date: 2023-05-12
    Description: Foraminiferal magnesium shows increasing promise as a paleothermometer, but the accuracy and precision are limited by biases introduced by partial dissolution, salinity variations, Mg-rich gametogenic calcite, and contaminant phases. We improved cleaning methods and reduced errors introduced by partial dissolution by sampling from well-preserved cores in the equatorial Atlantic and the Caribbean Sea with different dissolution histories. All cores reveal a synchronous 25% increase in Mg/Ca from the stage 2/3 boundary to the Holocene core top, indicating that dissolution is not a controlling factor. Modern temperatures estimated from core top Mg/Ca are 24.5°-25.0°C, equal to mean annual water temperatures at 50-100 m. We estimate that sea surface temperature increased by 2.6°C (±1.3) from the last glacial maximum to the Holocene. Holocene values were comparable to those during isotope stage 5e. Our data indicate that biases from contaminant phases and partial dissolution can be reduced. This paleothermometer holds promise if uncertainties introduced by salinity variations and gametogenic calcite can be constrained.
    Type: Dataset
    Format: application/zip, 3 datasets
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