@article {2950,
	title = {Queen triggerfish Balistes vetula: Validation of otolith-based age, growth, and longevity estimates via application of bomb radiocarbon},
	journal = {PLOS ONE},
	volume = {17},
	year = {2022},
	month = {Jul-01-2022},
	pages = {e0262281},
	abstract = {Ensuring the accuracy of age estimation in fisheries science through validation is an essential step in managing species for long-term sustainable harvest. The current study used Δ14 C in direct validation of age estimation for queen triggerfish Balistes vetula and conclusively documented that triggerfish sagittal otoliths provide more accurate and precise age estimates relative to dorsal spines. Caribbean fish samples (n = 2045) ranged in size from 67-473 mm fork length (FL); 23 fish from waters of the southeastern U.S. (SEUS) Atlantic coast ranged in size from 355-525 mm FL. Otolith-based age estimates from Caribbean fish range from 0-23 y, dorsal spine-based age estimates ranged from 1-14 y. Otolith-based age estimates for fish from the SEUS ranged from 8-40 y. Growth function estimates from otoliths in the current study (L$\infty$ = 444, K = 0.13, t0 = -1.12) differed from spined-derived estimates in the literature. Our work indicates that previously reported maximum ages for Balistes species based on spine-derived age estimates may underestimate longevity of these species since queen triggerfish otolith-based ageing extended maximum known age for the species by nearly three-fold (14 y from spines versus 40 y from otoliths). Future research seeking to document age and growth population parameters of Balistes species should strongly consider incorporating otolith-based ageing in the research design.},
	doi = {10.1371/journal.pone.0262281},
	url = {https://dx.plos.org/10.1371/journal.pone.0262281},
	author = {Shervette, Virginia R. and Rivera Hern{\'a}ndez, Jes{\'u}s M.},
	editor = {Claydon, John A. B.}
}
@book {2833,
	title = {Quaternary Glaciation of the Great Lakes Region: Process, Landforms, Sediments, and ChronologyMinimum age of the Mapleton, Tully, and Labrador Hollow moraines indicates correlation with the Port Huron Phase in central New York State},
	year = {2018},
	publisher = {Geological Society of America},
	organization = {Geological Society of America},
	abstract = {The glaciated terrain along the northern edge of the Appalachian Plateau in the eastern Finger Lakes of central New York has long been recognized as an important location for meltwater routing and for proglacial lake development in the Great Lakes region. Despite recognition of multiple ice margins formed by the Ontario Lobe of the Laurentide ice sheet during the late Wisconsinan, numerical age control of several margins has been elusive, particularly in regard to regional readvances of the Port Bruce (ca. 16,980{\textendash}18,000 cal [calibrated] yr B.P.) and Port Huron (ca. 14,300{\textendash} 16,000 cal yr B.P.) Phases. Utilizing light detection and ranging (LiDAR) terrain models in the eastern Finger Lakes area, we identified and described the Mapleton, Tully, and Labrador Hollow moraines. Associated ice-marginal landforms include push moraines, fans, and hummocky topography. In places, these features intrude into the northern heads of through valleys. Coring of three basins directly associated with these landforms yielded more than 20 samples of boreal tree needles and twigs, and Dryas leaves. Accelerated mass spectrometry (AMS) radiocarbon assay results indicate that poststadial lacustrine sedimentation began at ca. 15,000 cal yr B.P., consistent with ages of the Port Huron Phase.},
	doi = {10.1130/SPE53010.1130/2018.2530(10)},
	url = {https://pubs.geoscienceworld.org/books/book/2055/chapter/113619040/Minimum-age-of-the-Mapleton-Tully-and-Labrador},
	author = {Kehew, Alan E. and Curry, B. Brandon and Kozlowski, Andrew L. and Bird, Brian C. and Lowell, Thomas V. and Smith, Colby A. and Feranec, Robert S. and Graham, Brandon Lars}
}
@article {2509,
	title = {Quantifying bamboo coral growth rate nonlinearity with the radiocarbon bomb spike: A new model for paleoceanographic chronology development},
	journal = {Deep Sea Research Part I: Oceanographic Research Papers},
	year = {2017},
	month = {Jan-04-2017},
	abstract = {Bamboo corals, long-lived cold water gorgonin octocorals, offer unique paleoceanographic archives of the intermediate ocean. These Isididae corals are characterized by alternating gorgonin nodes and high Mg-calcite internodes, which synchronously extend radially. Bamboo coral calcite internodes have been utilized to obtain geochemical proxy data, however, growth rate uncertainty has made it difficult to construct precise chronologies for these corals. Previous studies have relied upon a single tie point from records of the anthropogenic Δ14C bomb spike preserved in the gorgonin nodes of live-collected corals to calculate a mean radial extension rate for the outer ~50 years of skeletal growth. Bamboo coral chronologies are typically constructed by applying this mean extension rate to the entire coral record, assuming constant radial extension with coral age. In this study, we aim to test this underlying assumption by analyzing the organic nodes of six California margin bamboo corals at high enough resolution (<0.5 mm) to identify the Δ14C bomb spike, including two tie points at 1957 and 1970, plus the coral collection date (2007.5) for four samples. Radial extension rates between tie points ranged from 10 to 204 {\textmu}m/year, with a decrease in growth rate evident between the 1957{\textendash}1970 and 1970{\textendash}2007.5 periods for all four corals. A negative correlation between growth rate and coral radius (r =-0.7; p=0.04) was determined for multiple bamboo coral taxa and individuals from the California margin, demonstrating a decline in radial extension rate with specimen age and size. To provide a mechanistic basis for these observations, a simple mathematical model was developed based on the assumption of a constant increase in circular cross sectional area with time to quantify this decline in radial extension rate with coral size between chronological tie points. Applying the area-based model to our Δ14C bomb spike time series from individual corals improves chronology accuracy for all live-collected corals with complete Δ14C bomb spikes. Hence, this study provides paleoceanographers utilizing bamboo corals with a method for reducing age model uncertainty within the anthropogenic bomb spike era (~1957-present). Chronological uncertainty is larger for the earliest portion of coral growth, particularly for skeleton precipitated prior to bomb spike tie points, meaning age estimations for samples living before 1957 remain uncertain. Combining this technique with additional chronological markers could improve age models for an entire bamboo coral. Finally, the relative consistency in growth rate in similarly-aged corals of the same depth and location supports the hypothesis that skeletal growth may be limited by local environmental conditions.},
	keywords = {14C nuclear bomb spike, Bamboo coral, Chronologies, Gorgonin, Growth rate, paleoceanography, radiocarbon},
	issn = {09670637},
	doi = {10.1016/j.dsr.2017.04.006},
	url = {https://doi.org/10.1016/j.dsr.2017.04.006},
	author = {Frenkel, M.M. and LaVigne, M. and Miller, H.R. and Hill, T.M. and McNichol, A. and Gaylord, M. Lardie}
}
@article {14,
	title = {Quantification of refractory organic material in Amazon mudbanks of the French Guiana Coast},
	journal = {Marine Geology},
	volume = {363},
	year = {2015},
	pages = {93-101},
	abstract = {Sub-oxic overturning mudbanks originating in the Amazon outlet and traveling northwestward along the coast of South America store 3.5 Tg organic carbon on the Amazon shelf, annually. The predominance of old soil carbon burial associated with the sediment has been supported by relatively old bulk radiocarbon ages (~ 2200{\textendash}3200 14C y) reported, but this amount has yet to be quantified for this dynamic setting. Here, we employ ramped pyrolysis radiocarbon dating to mudbank sediments from three cores to further constrain the amount of refractory sedimentary organic carbon present. Using radiocarbon age as a proxy for reactivity, we find that at least 36\% of this organic carbon is pre-aged refractory terrestrial organic carbon, likely sourced from terrestrial soils and averaging ages of 16,100 {\textpm} 300 14C y. This implies significant preservation of pre-aged terrestrial soil material in this marine environment despite the mobility and oxygen availability in the muds. Concurrently, an average of 77\% of this organic material is aged over 1000 14C y, consistent with previous estimates that the majority of organic carbon buried along the shelf is refractory. Analyses of extracted lignin phenols and terrestrial humic acids also support this preservation of refractory terrestrial material. These data indicate that sediment discharged from the Amazon River may preserve refractory terrestrial carbon in marine sediments at a minimum of 3.1 Tg C/y, which is more efficient than originally thought.},
	issn = {0025-3227},
	doi = {10.1016/j.margeo.2015.02.009},
	url = {http://www.sciencedirect.com/science/article/pii/S0025322715000456},
	author = {Williams, Elizabeth K. and Rosenheim, Brad E. and Allison, Mead and McNichol, Ann P. and Xu, Li}
}
@article {2503,
	title = {Quantifying overwash flux in barrier systems: An example from Martha{\textquoteright}s Vineyard, Massachusetts, USA},
	journal = {Marine Geology},
	volume = {343},
	year = {2013},
	month = {Jan-09-2013},
	pages = {15 - 28},
	abstract = {Coastal barriers are particularly susceptible to the effects of accelerated sea-level rise and intense storms. Over centennial scales, barriers are maintained via overtopping during storms, which causes deposition of washover fans on their landward sides. Understanding barrier evolution under modern conditions can help evaluate the likelihood of future barrier stability. This study examines three washover fans on the undeveloped south shore of Martha{\textquoteright}s Vineyard using a suite of vibracores, ground penetrating radar, high resolution dGPS, and LiDAR data. From these data, the volumes of the deposits were determined and range from 2.1 to 2.4 {\texttimes} 104 m3. Two of these overwash events occurred during Hurricane Bob in 1991. The water levels produced by this storm have a calculated return interval of ~ 28 years, implying an onshore sediment flux of 2.4{\textendash}3.4 m3/m/yr. The third washover was deposited by a nor{\textquoteright}easter in January 1997, which has a water level return interval of ~ 6 years, suggesting a flux of 8.5 m3/m/yr. These onshore fluxes are smaller than the erosional flux of sediment resulting from shoreline retreat, suggesting that the barrier is not in long-term equilibrium, a result supported by the thinning of the barrier in recent years.},
	keywords = {barrier system, Coastal evolution, overwash flux, sea-level rise, storm impacts},
	issn = {00253227},
	doi = {10.1016/j.margeo.2013.05.013},
	url = {http://linkinghub.elsevier.com/retrieve/pii/S002532271300114Xhttp://api.elsevier.com/content/article/PII:S002532271300114X?httpAccept=text/xmlhttp://api.elsevier.com/content/article/PII:S002532271300114X?httpAccept=text/plain},
	author = {Carruthers, Emily A. and Lane, D. Philip and Evans, Rob L. and Donnelly, Jeffrey P. and Ashton, Andrew D.}
}
@article {262,
	title = {Quaternary paleoceanography of the central arctic based on Integrated Ocean Drilling Program Arctic Coring Expedition 302 foraminiferal assemblages},
	journal = {Paleoceanography},
	volume = {23},
	year = {2008},
	note = {id: 813; 281VR Times Cited:10 Cited References Count:84Y},
	abstract = {The Integrated Ocean Drilling Program (IODP) Arctic Coring Expedition (ACEX) Hole 4C from the Lomonosov Ridge in the central Arctic Ocean recovered a continuous 18 m record of Quaternary foraminifera yielding evidence for seasonally ice-free interglacials during the Matuyama, progressive development of large glacials during the mid-Pleistocene transition (MPT) similar to 1.2-0.9 Ma, and the onset of high-amplitude 100-ka orbital cycles similar to 500 ka. Foraminiferal preservation in sediments from the Arctic is influenced by primary (sea ice, organic input, and other environmental conditions) and secondary factors (syndepositional, long-term pore water dissolution). Taking these into account, the ACEX 4C record shows distinct maxima in agglutinated foraminiferal abundance corresponding to several interglacials and deglacials between marine isotope stages (MIS) 13-37, and although less precise dating is available for older sediments, these trends appear to continue through the Matuyama. The MPT is characterized by nearly barren intervals during major glacials (MIS 12, 16, and 22-24) and faunal turnover (MIS 12-24). Abundant calcareous planktonic (mainly Neogloboquadrina pachyderma sin.) and benthic foraminifers occur mainly in interglacial intervals during the Brunhes and very rarely in the Matuyama. A distinct faunal transition from calcareous to agglutinated foraminifers 200-300 ka in ACEX 4C is comparable to that found in Arctic sediments from the Lomonosov, Alpha, and Northwind ridges and the Morris Jesup Rise. Down-core disappearance of calcareous taxa is probably related to either reduced sea ice cover prior to the last few 100-ka cycles, pore water dissolution, or both.},
	issn = {0883-8305},
	doi = {10.1029/2007pa001484},
	author = {Cronin, T. M. and Smith, S. A. and Eynaud, F. and O{\textquoteright}Regan, M. and King, J.}
}
@article {515,
	title = {Quantification and radiocarbon source apportionment of black carbon in atmospheric aerosols using the CTO-375 method},
	journal = {Atmospheric Environment},
	volume = {41},
	year = {2007},
	note = {id: 818; 243XB Times Cited:8 Cited References Count:58Y},
	pages = {7895-7906},
	abstract = {To make progress towards linking the atmosphere and biogeosphere parts of the black carbon (BC) cycle, a chemothermal oxidation method (CTO-375), commonly applied for isolating BC from complex geomatrices such as soils, sediments and aquatic particles, was applied to investigate the BC also in atmospheric particles. Concentrations and C-14-based source apportionment of CTO-375 based BC was established for a reference aerosol (NIST RM-8785) and for wintertime aerosols collected in Stockholm and in a Swedish background area. The results were compared with thermal-optical (OC/EC) measurements. For NIST RM-8785, a good agreement was found between the BCCTO-375 concentration and the reported elemental carbon (EC) concentration measured by the "Speciation Trends Network - National Institute of Occupational Safety and Health" method (ECNIOSH) with BCCTO-375 of 0.054+/-0.002gg(-1) and ECNIOSH of 0.067+/-0.008gg(-1). In contrast, there was an average factor of ca. 20 difference between BC(CTO-37)5 and ECNIOSH for the ambient Scandinavian wintertime aerosols, presumably reflecting a combination of BCCTO-375 isolating only the recalcitrant soot-BC portion of the BC continuum and the ECNIOSH metric inadvertently including some intrinsically non-pyrogenic organic matter. Isolation of BCCTO-375 with subsequent off-line radiocarbon analysis yielded fraction modern values (fM) for total organic carbon (TOC) of 0.93 (aerosols from a Swedish background area), and 0.58 (aerosols collected in Stockholm); whereas the fM for BCCTO-375 isolates were 1.08 (aerosols from a Swedish background area), and 0.87 (aerosols collected in Stockholm). This radiocarbon-based source apportionment suggests that contribution from biomass combustion to cold-season atmospheric BCCTO-375 in Stockholm was 70\% and in the background area 88\%. (C) 2007 Elsevier Ltd. All rights reserved.},
	issn = {1352-2310},
	doi = {10.1016/j.atmosenv.2007.06.006},
	author = {Zencak, Z. and Elmquist, M. and Gustafsson, O.}
}
@article {977,
	title = {Quantity, C-14 age and lability of desorbed soil organic carbon in fresh water and seawater},
	journal = {Organic Geochemistry},
	volume = {38},
	year = {2007},
	note = {id: 1161},
	pages = {1547-1557},
	abstract = {Soil organic carbon (OC) resulting from terrestrial photosynthesis is one of the largest reactive pools of sequestered atmospheric CO2. As an intermediate storage mechanism for organic material through time, the vertical distribution of carbon in a soil profile generally shows an age continuum with depth. Aged soil carbon is often the result of sorptive preservation, a physical mechanism that protects organic matter (OM) from microbial decay. Sorptive preservation is, however, a reversible process. Upon desorption, previously protected OM could be available for decomposition. Here we present simple fresh and salt water desorption experiments designed to determine the amount, 14C age and lability of {\textquotedblleft}reversible{\textquotedblright} OM. Results suggest that 1.1{\textendash}3.9\% and 1.5{\textendash}6.7\% of OC, and 0.7{\textendash}3\% and 0.6{\textendash}5\% of total soil nitrogen can be desorbed using fresh and salt water, respectively. Radiocarbon data suggest this desorbed carbon is Δ14C-enriched compared to the bulk soil, with Δ14C values close to modern atmospheric Δ14CO2 at the soil surface, and aging with depth. Of this extractable aged carbon, upwards of 23{\textendash}56\% is labile across all treatments and with depth. Additional carbon is extracted with salt water compared to fresh water and this surplus is non-labile and younger than the labile component. Radiocarbon dating shows that the 14C age of soil carbon increases with depth and that there is a pool of Δ14C-depleted OC that is readily remineralized upon entering an aquatic/marine environment. These results indicate that eroded soil particles can release OC and organic N when entering rivers and oceans and that up to 50\% of this carbon is available for aquatic metabolism.},
	doi = {10.1016/j.orggeochem.2007.05.011},
	author = {Butman, D. and Raymond, P. A. and Oh, N. H. and Mull, K.}
}
@article {651,
	title = {Quaternary depositional patterns and sea-level fluctuations, northeastern North Carolina},
	journal = {Quaternary Research},
	volume = {67},
	year = {2007},
	note = {131tvTimes Cited:18Cited References Count:56},
	month = {Jan},
	pages = {83-99},
	abstract = {A detailed record of late Quaternary sea-level oscillations is preserved within the upper 45 in of deposits along an eight kin transect across Croatan Sound, a drowned tributary of the Roanoke/Albemarle drainage system, northeastern North Carolina. Drill-hole and seismic data reveal nine relatively complete sequences filling an antecedent valley comprised of discontinuous middle and early Pleistocene deposits. On interfluves, lithologically similar marine deposits of different sequences occur stacked in vertical succession and separated by ravinement surfaces. Within the paleo-drainage, marine deposits are separated by fluvial and/or estuarine sediments deposited during periods of lowered sea level. Foraminiferal and molluscan fossil assemblages indicate that marine facies were deposited in a shallow-marine embayment with open connection to shelf waters. Each sequence modifies or truncates portions of the preceding sequence or sequences. Sequence boundaries are the product of a combination of fluvial, estuarine, and marine erosional processes. Stratigraphic and age analyses constrain the ages of sequences to late Marine Isotope Stage (MIS) 6 and younger (similar to 140 ka to present), indicating multiple sea-level oscillations during this interval. Elevations of highstand deposits associated with late MIS 5 and MIS 3 imply that sea level was either similar to present during those times, or that the region may have been influenced by glacio-isostatic uplift and Subsidence. (c) 2006 University of Washington. All rights reserved.},
	issn = {0033-5894},
	doi = {10.1016/j.yqres.2006.07.003},
	author = {Parham, P. R. and Riggs, S. R. and Culver, S. J. and Mallinson, D. J. and Wehmiller, J. F.}
}
@article {1532,
	title = {Quaternary geology of the San Luis Basin, southern Colorado and Northern New Mexico--Rocky Mountain Section Friends of the Pleistocene Guidebook},
	year = {2007},
	note = {id: 625},
	month = {2007},
	author = {Machette, M. N. and Coates, M. M. and Johnson, M. J.}
}
@article {421,
	title = {Quaternary glaciation and hydrologic variation in the South American tropics as reconstructed from the Lake Titicaca drilling project},
	journal = {Quaternary Research},
	volume = {68},
	year = {2007},
	note = {id: 841; 227AJ Times Cited:9 Cited References Count:63Y},
	pages = {410-420},
	abstract = {A 136-m-long drill core of sediments was recovered from tropical high-attitude Lake Titicaca, Bolivia-Peru, enabling a reconstruction of past climate that spans four cycles of regional glacial advance and retreat and that is estimated to extend continuously over the last 370,000 yr. Within the errors of the age model, the periods of regional glacial advance and retreat are concordant respectively with global glacial and interglacial stages. Periods of ice advance in the southern tropical Andes generally were periods of positive water balance, as evidenced by deeper and fresher conditions in Lake Titicaca. Conversely, reduced glaciation occurred during periods of negative water balance and shallow closed-basin conditions in the lake. The apparent coincidence of positive water balance of Lake Titicaca and glacial growth in the adjacent Andes with Northern Hemisphere ice sheet expansion implies that regional water balance and glacial mass balance are strongly influenced by global-scale temperature changes, as well as by precessional forcing of the South American summer monsoon. (c) 2007 University of Washington. All rights reserved.},
	issn = {0033-5894},
	doi = {10.1016/J.Yqres.2007.07.008},
	author = {Fritz, S. C. and Baker, P. A. and Seltzer, G. O. and Ballantyne, A. and Tapia, P. and Cheng, H. and Edwards, R. L.}
}
@article {1942,
	title = {Quantifying archaeal community autotrophy in the mesopelogic ocean using natural radiocarbon},
	journal = {Proc. Natl. Acad. Sci. USA},
	volume = {103},
	year = {2006},
	note = {id: 502},
	month = {2006},
	pages = {6442-6447},
	author = {Ingalls, A. E. and Shah, S. R. and Hansman, R. L. and Aluwihare, L. I. and Santos, G. M. and Druffel, E. R. M. and Pearson, A.}
}
@article {2035,
	title = {Quartz content and the quartz-to-plagioclase ratio determined by X-ray diffraction: a proxy for ice rafting in the northern North Atlantic?},
	journal = {Earth and Planetary Science Letters},
	volume = {218},
	year = {2004},
	note = {id: 713},
	month = {2004},
	pages = {389-401},
	author = {Moros, M. and McManus, J. F. and Rasmussen, T. and Kuijpers, A. and Dokken, T. and Snowball, I. and Jansen, E. and Neilsen, T.}
}
@inbook {1444,
	title = {Quaternary sea level history of the United States},
	booktitle = {The Quaternary period in the United States, Developments in Quaternary science},
	year = {2004},
	note = {id: 706},
	month = {2004},
	pages = {147-183},
	publisher = {Elsevier},
	organization = {Elsevier},
	address = {Amsterdam},
	author = {Muhs, D. R. and Wehmiller, J. F. and Simmons, K. R. and York, L. L.},
	editor = {Gillespie, A. R.}
}
@article {360,
	title = {Quantitative estimates of time-averaging in terebratulidbrachiopod shell accumulations from a modern tropical shelf},
	journal = {Paleobiology},
	volume = {29},
	year = {2003},
	note = {id: 2231; Source type: scholarlyjournals; Object type: Article; Object type: Feature; CSAUnique: BONE5712965; AccNum: 5712965; DOI: 10.1043/0094-8373(2003)029(0381:QEOTIT)2.0.CO;2; ISSN: 0094-8373; Peer Reviewed: true},
	pages = {381-402},
	abstract = {Quantitative estimates of time-averaging in marine shellaccumulations available to date are limited primarily toaragonitic mollusk shells. We assessed time-averaging in Holoceneassemblages of calcitic brachiopod shells by direct dating ofindividual specimens of the terebratulid brachiopod Bouchardiarosea. The data were collected from exceptional (brachiopod-rich)shell assemblages, occurring surficially on a tropical mixedcarbonate-siliciclastic shelf (the Southeast Brazilian Bight, SWAtlantic), a setting that provides a good climatic andenvironmental analog for many Paleozoic brachiopod shell beds ofNorth America and Europe. A total of 82 individual brachiopodshells, collected from four shallow (5-25 m) nearshore (},
	issn = {0094-8373, 0094-8373},
	doi = {10.1043/0094-8373(2003)029(0381:QEOTIT)2.0.CO;2},
	author = {Carroll, M. and Kowalewski, M. and Simoes, M. G. and Goodfriend, G. A.}
}
@article {2206,
	title = {Quantitative estimates of time-averaging in articulate brachiopod accumulations from a Holocene tropical shelf (Southern Brazil)},
	journal = {Geological Society of America Abstracts with Programs},
	volume = {32},
	year = {2000},
	note = {id: 124},
	month = {2000},
	pages = {A13-A14},
	author = {Carroll, M. and Kowalewski, M. and Simoes, M. G. and Goodfriend, G. A.}
}
@mastersthesis {1204,
	title = {Quaternary Geology of Central Sheboygan County, Wisconsin, Thesis},
	volume = {MS},
	year = {2000},
	month = {2000},
	school = {University of Wisconsin},
	address = {Madison, Wisconsin},
	author = {Chapel, Dawn}
}
@article {749,
	title = {Quaternary palaeohydrological evolution of a playa lake: Salada Mediana, central Ebro Basin, Spain},
	journal = {Sedimentology},
	volume = {47},
	year = {2000},
	note = {383xwTimes Cited:31Cited References Count:76},
	month = {Dec},
	pages = {1135-1156},
	abstract = {Sedimentary features, mineralogy, bulk geochemical composition, stable isotope analyses and pollen data from sediment cores were used to reconstruct the Late Quaternary depositional evolution of the Salada Mediana playa lake (central Ebro Basin, northeastern Spain). The 150-cm-long sediment core sequence is composed of gypsum- and dolomite-rich muds (Lower and Middle sections) and black, laminated, calcite-bearing sediments (Upper section). The Salada Mediana formed as a karstic depression in the Miocene gypsum substratum during the Late Pleistocene. The Lower section was deposited in a sulphate-carbonate saline lake that ended with a period of desiccation and basin floor deflation. Subsequent deposition (Middle section) took place in a playa-lake system. Two cycles of lower water table and expanded saline mud flats occurred. The Holocene sequence is missing, probably as a result of aeolian erosion. Sedimentation resumed only a few centuries ago, and saline pan environments dominated until modern times. The Salada Mediana facies succession was mainly governed by fluctuations in the hydrological balance, brine composition, and salinity; however, aeolian processes (detrital input and deflation) and recycling of previously precipitated salts also played a significant role.},
	issn = {0037-0746},
	doi = {10.1046/j.1365-3091.2000.00346.x},
	author = {Valero-Garces, B. L. and Delgado-Huertas, A. and Navas, A. and Machin, J. and Gonzalez-Samperiz, P. and Kelts, K.}
}
@article {981,
	title = {Quantitative Production of H2 by Pyrolysis of Gas Chromatographic Effluents},
	journal = {Analytical Chemistry},
	volume = {70},
	year = {1998},
	note = {id: 1731},
	pages = {5136-5141},
	doi = {10.1021/ac980248v},
	author = {Burgoyne, Thomas W. and Hayes, John M.}
}
@inbook {1391,
	title = {Quantification and characterization of porewater organic colloids},
	booktitle = {Organic Substances and Sediments in Water. Processes and Analytical},
	volume = {2},
	year = {1991},
	note = {id: 1744},
	month = {1991},
	pages = {107-126},
	publisher = {CRC Press},
	organization = {CRC Press},
	address = {Boca Raton, FL},
	author = {Chin, Y. P. and McNichol, A. P. and Gschwend, P. M.},
	editor = {Baker, R. A.}
}
