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Data were drawn from the Whitehall II study with baseline examination in 1991; follow-up screenings in 1997, 2003, and 2008; and additional disease ascertainment from hospital data and registry linkage on 5318 participants (mean age 54.8 years, 31% women) without depressive symptoms at baseline. Vascular risk was asses... | {
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The Whitehall II study is a prospective cohort study of British civil servants established in 1985 to study associations between risk factors, pathophysiological changes, and clinical disease (22). The target population was all London-based office staff, aged 35 to 55, working in 20 civil service departments on recruit... | {
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We used standard operating protocols to measure risk factors for the Framingham general CVD risk score (sex, age, diabetes, smoking, treated and untreated systolic blood pressure, total cholesterol, high-density lipoprotein [HDL] cholesterol), CHD risk score (sex, age, diabetes, smoking, systolic and diastolic blood pr... | {
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new venous blood samples were taken at 2 hours postadministration of a 75 g glucose solution. Blood glucose was measured using the glucose oxidase method on a YSI MODEL 2300 STAT PLUS Analyzer (YSI Corporation, Yellow Springs, Ohio; mean coefficient of variation: 1.4%–3.1%). Diabetes was defined by fasting glucose ≥7.0... | {
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medication was requested at phases 3, 5, and 7. | {
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The validity of the Framingham risk scores as measures of vascular risk was supported in our study, as they strongly predicted incidence of subsequent (manifest) vascular disease. Age- and sex-adjusted odds ratio for 10% increment in risk was 2.84 (95% confidence interval [CI] 1.66–4.88) for the stroke risk score-incid... | {
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We used three indicators (or proxy measures) to identify persons with depressive symptoms. First, participants responded to the self-administered 30-item General Health Questionnaire (GHQ) at phases 3, 5, 7, and 9, a screening instrument designed for and widely used in population-based surveys and trials (26). Each que... | {
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against diagnosed depressive episodes based on a structured psychiatric interview were 80% and 81%, respectively. | {
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Second, at phases 7 and 9, depressive symptoms were also assessed using the Center for Epidemiologic Studies Depression Scale (CES-D) (note that CES-D was not included in earlier screening phases of our study) (29). The 20 items of the CES-D measure symptoms associated with depression; participants are asked to score t... | {
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Third, at phases 3, 5, 7, and 9, participants were asked whether they had taken any medication in the past 14 days and, if so, to provide the name of the medication. Medications were coded using British National Formulary codes to define antidepressant medication use (codes: 040301–040304) (31). | {
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We constructed Framingham CVD, CHD, and stroke risk scores for each participant and used logistic regression to examine the association of each risk score at baseline with depressive symptoms at follow-up. Crude, age- and sex-adjusted, and multivariably adjusted odds ratios and 95% confidence intervals per 10% absolute... | {
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Differences between the analytic sample and the excluded participants were generally small (Table S1 in Supplement 1). Compared with those included, participants excluded from the analyses were more likely to be women, nonwhite, and current smokers, although other characteristics were similar in the two groups. Across ... | {
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After adjustment for multiple covariates (age, sex, marital status, education, socioeconomic status, retirement, cognitive impairment, body mass index, alcohol consumption, menopausal status [women], and nonvascular chronic condition), the association between vascular disease and subsequent CES-D depressive symptoms re... | {
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This longitudinal study of British adults shows that manifest cardiovascular disease (CHD and stroke) is associated with increased risk of depressive symptoms. There was also some evidence to suggest an association between higher Framingham stroke risk score and increased onset of depressive symptoms before the age of ... | {
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A few previous studies have examined the longitudinal association between overall vascular risk and later-life depression using other indicators of vascular risk status. In the Health, Aging and Body Composition study of adults aged 70 or higher, a score combining selected vascular risk factors (body mass index, metabo... | {
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There are caveats to the results reported here. We measured depressive symptoms using validated instruments, such as the General Health Questionnaire and CES-D, and information on prescribed antidepressant medication use (26,29,49). These instruments are not designed to make a psychiatric diagnosis of first or recurren... | {
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Despite a high response to the survey (range 66% to 88%) at the successive data collection phases, loss to follow-up accumulated over the extended follow-up, as is inevitable in long-term prospective studies. However, differences between the included and excluded participants were generally small. Our study is based on... | {
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These results suggest that public health measures to improve vascular status will influence the incidence of later-life depression, primarily via reduced rates of manifest vascular disease. Our findings on diagnosed vascular disease support current clinical guidelines to screen patients with coronary heart disease or s... | {
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Association Between Framingham Risk Scores (per 10% Increase) and Subsequent Onset of Depressive Symptoms Before and After Age 65 | {
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Environmental changes associated with the Paleocene–Eocene thermal maximum (PETM, ∼56 Ma) have not yet been documented in detail from the North Sea Basin. Located within proximity to the North Atlantic igneous province (NAIP), the Kilda Basin, and the northern rain belt (paleolatitude 54 °N) during the PETM, this is a ... | {
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at the onset and within the earliest CIE which, coupled with evidence for sea level rise, may be interpreted as resulting from an increase in precipitation over NW Europe consistent with an enhanced hydrologic cycle in response to global warming during the PETM. Palynological evidence indicates a flora dominated by pol... | {
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The PETM was a period of geologically-rapid global warming that punctuated a warming Eocene climate 55.8 Ma ago (Charles et al., 2011), and saw sea surface temperatures rise by 5–8 °C from background levels (Zachos et al., 2005; Sluijs et al., 2007). It was associated with a substantial injection of δ13C-depleted carbo... | {
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During the late Paleocene–early Eocene the North Sea was a restricted marine basin, characterised by siliciclastic sedimentation and high terrigenous input, principally from the Scotland–Faeroe–Shetland landmass (Knox 1998, Fig. S1). Core 22/10a-4 is located in the central part of the basin (Figs. 1 and S1) and is ther... | {
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As 22/10a-4 is in the deep (>0.5 km) central part of the basin, it acted as a depocentre and exhibits a Paleocene-Eocene transition sequence that is not only expanded but is also close to being stratigraphically complete. The only evidence for breaks in the succession is minor erosion at the base of thin turbidite sand... | {
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et al., 2011), due to the thermal expansion of sea water and possible melting of ice caps, although the North Sea basin remained restricted as evidenced by the persistence of low oxygen facies in 22/10a-4. The North Sea had a widespread freshwater catchment area, and a halocline was in place from the late Paleocene to ... | {
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Borehole 22/10a-4 (57°44’8.47”N; 1°50’26.59”E) provides a continuous core through the Forties Sandstone Member and into the Lista Formation (Fig. 2). The core consists of variably fissile claystone with interbedded fine to coarse grained sandstone layers interpreted as turbidites, with occasional mm-thick ash layers (F... | {
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A total of 71 palynology samples were prepared at the British Geological Survey using standard preparation procedures (Moore et al., 1991). Samples were demineralised with hydrochloric (HCl) and hydrofluoric (HF) acids, and residual mineral grains removed using heavy liquid (zinc bromide) separation. Elvacite was used ... | {
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amorphous organic matter (AOM), were also analysed for δ13C. Foraminifera samples between 20 and 60 g of dried sediment were processed by washing through a 63 μm sieve with water. All specimens were counted and converted to foraminifera/g (Table S2). All species exhibited agglutinated (non calcareous) test walls. | {
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All analyses were carried out at the NERC Isotope Geosciences Laboratory. C and N analyses (from which we present weight % C/N) were performed on 225 samples by combustion in a Costech ECS4010 Elemental Analyser (EA) calibrated against an acetanilide standard (Table S3). C/N atomic ratios were calculated by multiplying... | {
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was also carried out on palynology residues of the >250 μm size fractions dominated by AOM. 13C/12C analyses were performed on 35 samples by combustion in a Costech Elemental Analyser (EA) online to a VG TripleTrap and Optima dual-inlet mass spectrometer, with δ13C values calculated to the VPDB scale using a within-run... | {
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A negative carbon isotope excursion of 5‰ has been identified from δ13CTOC and δ13CAOM in an expanded Paleocene–Eocene boundary section from the central North Sea Basin. Palynological (dinoflagellate cyst, pollen, and spore assemblages) and sedimentologic (C/N ratios and kaolinite distribution) evidence indicate major ... | {
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this location (paleolatitude 54 oN) increased precipitation would support the hypothesis that a poleward migration of storm tracks from an enhanced hydrologic cycle resulted from global warming during the PETM (Pagani et al., 2006b). | {
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"text": "paleolatitude",
"start": 15,
"end": 28
}
],
"measured entity": [
{
"text": "location",
"start... | {
"entities": [
{
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"description_source":... |
Carbon isotopic results of total organic matter (δ13CTOC) and amorphous organic matter (δ13CAOM) against core 22/10a-4 lithology and Apectodinium spp. (%). Blue=bulk rock δ13CTOC; black=δ13CAOM; solid red symbols=bulk rock δ13CTOC from samples with <30% wood/plant tissue (determined from palynological residue of the sa... | {
"entities": {
"quantity": [
{
"text": "<30%",
"start": 249,
"end": 253
},
{
"text": ">30%",
"start": 380,
"end": 384
},
{
"text": "2614.7 and 2619.6 m",
"start": 658,
"end": 677
}
],
"measured pro... | {
"entities": [
{
"label": "quantity",
"description": "A count, consisting of a value, or a measurement, consisting of a value and usually a unit, including contiguous modifiers such as tolerances, 'approximately' or '<'; e.g. '355 ml', 'five' samples, 'room temperature'.",
"description_source":... |
The abrupt onset of Antarctic glaciation during the Eocene–Oligocene Transition (∼33.7 Ma, Oi1) is linked to declining atmospheric pCO2 levels, yet the mechanisms that forced pCO2 decline remain elusive. Biogenic silicon cycling is inextricably linked to both long and short term carbon cycling through the diatoms, sili... | {
"entities": {
"quantity": [
{
"text": "∼33.7 Ma",
"start": 81,
"end": 89
},
{
"text": "up to 40%",
"start": 368,
"end": 377
},
{
"text": "0.6‰",
"start": 895,
"end": 899
},
{
"text": "1.5‰",... | {
"entities": [
{
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"description": "A count, consisting of a value, or a measurement, consisting of a value and usually a unit, including contiguous modifiers such as tolerances, 'approximately' or '<'; e.g. '355 ml', 'five' samples, 'room temperature'.",
"description_source":... |
acid concentration in the high southern latitudes. Intermediate depth silicic acid concentration peaked at ∼31.5 Ma, coincident with the final establishment of a deepwater pathway through the Tasman Gateway and Drake Passage. These results suggest that upwelling intensification related to the spin-up of a circum-Antarc... | {
"entities": {
"quantity": [
{
"text": "∼31.5 Ma",
"start": 107,
"end": 115
}
],
"measured entity": [
{
"text": "Intermediate depth silicic acid concentration",
"start": 51,
"end": 96
}
],
"measured property": [
{
... | {
"entities": [
{
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"description": "A count, consisting of a value, or a measurement, consisting of a value and usually a unit, including contiguous modifiers such as tolerances, 'approximately' or '<'; e.g. '355 ml', 'five' samples, 'room temperature'.",
"description_source":... |
In the Furlo section the CTBI lies within the Scaglia Bianca Formation, which includes abundant biosiliceous limestone. The Livello Bonarelli is a 1 m thick condensed interval of millimetre-laminated black shale and brown radiolarian sand that represents the sedimentary expression of part of OAE 2 (Arthur and Premoli S... | {
"entities": {
"quantity": [
{
"text": "1 m",
"start": 147,
"end": 150
},
{
"text": "Up to 20 m",
"start": 333,
"end": 343
},
{
"text": "∼−25.9 to −26.5‰.",
"start": 537,
"end": 554
},
{
"tex... | {
"entities": [
{
"label": "quantity",
"description": "A count, consisting of a value, or a measurement, consisting of a value and usually a unit, including contiguous modifiers such as tolerances, 'approximately' or '<'; e.g. '355 ml', 'five' samples, 'room temperature'.",
"description_source":... |
Sensitivity analysis carried out on MTDATA software, for 9 and 21 trace elements. | {
"entities": {
"quantity": [
{
"text": "9 and 21",
"start": 57,
"end": 65
}
],
"measured entity": [
{
"text": "trace elements",
"start": 66,
"end": 80
}
]
},
"relations": {
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{
"head": {
... | {
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"description_source":... |
The fate of trace elements was investigated in a 90 kW oxy-combustion pilot plant fed with coal and limestone [7]. It was shown that 82% of elemental Hg was emitted in the exhaust gas, as was 81% of Cl. It was further suggested that the relatively low temperatures, and high Ca content in the system from limestone use p... | {
"entities": {
"quantity": [
{
"text": "90 kW",
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"end": 54
},
{
"text": "82%",
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"end": 136
},
{
"text": "81%",
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],
"measured entity": [
{
... | {
"entities": [
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"description_source":... |
Those elements at the higher concentrations in the flue gas include Na, Si, K, Zn, and Br. For Na in particular which was present in reduced amounts in the solid, this suggests that some of it may be partitioning to the flue gas for bed inventories 6 and 13 kg. | {
"entities": {
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{
"text": "6 and 13 kg",
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"measured entity": [
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"text": "bed inventories",
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]
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"description_source":... |
For Na, Al, K and Fe, the lowest bed inventory of 4.5 kg resulted in a concentration in the flue gas which was less than that of the blank sample, values which then increased for the higher bed inventories. This suggests that a certain amount of these elements is being absorbed, perhaps by the sorbent in the case of Fe... | {
"entities": {
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"text": "4.5 kg",
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{
"text": "4.5 kg and 13 kg",
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},
{
"text": "6 kg",
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"end": 488
},
{
"text": "<... | {
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"description_source":... |
Effect of bed inventory on increase of solid major elemental concentrations for bed inventories of 4.5 kg, 6 kg and 13 kg CaCO3. | {
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"quantity": [
{
"text": "4.5 kg, 6 kg and 13 kg",
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],
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],
"qualifier": [
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"text": "CaCO3",
... | {
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"description_source":... |
SEM–EDS analysis of sorbent for reactions undertaken with different SO2 concentrations, showing error bars of +1%. | {
"entities": {
"quantity": [
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"text": "+1%",
"start": 110,
"end": 113
}
],
"measured entity": [
{
"text": "error bars",
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]
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"description_source":... |
Enceladus, one out of currently 62 satellites of Saturn, orbits the planet at a distance of 3.95 Saturn radii RS (1RS = 60,268 km) and is embedded in the radiation belts of Saturn’s inner magnetosphere. Even with a small radius REnc of only 252 km and an apparent similarity to other icy moons, this moon is by far the m... | {
"entities": {
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"text": "62 satellites",
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"end": 45
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{
"text": "3.95 Saturn radii RS",
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},
{
"text": "60,268 km",
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{
... | {
"entities": [
{
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"description_source":... |
2006) from those geysers is the main source of the E-ring and the neutral torus and is the major plasma source of water group ions in the magnetosphere. A summary of Enceladus findings from Cassini measurements is very well presented by Spencer et al. (2009). | {
"entities": {},
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} | {
"entities": [
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"description_source":... |
Illustrated electron drift paths for different energies near Enceladus in a perturbed electric field configuration. Only the equatorial plane is shown where x points in the flow direction and y points toward the planet. The energy is mentioned on the top of each figure, The parameter a = 0.1 is the assumed surface velo... | {
"entities": {
"quantity": [
{
"text": "0.1",
"start": 289,
"end": 292
},
{
"text": "10%",
"start": 328,
"end": 331
}
],
"measured entity": [
{
"text": "parameter a",
"start": 275,
"end": 286
},
... | {
"entities": [
{
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"description": "A count, consisting of a value, or a measurement, consisting of a value and usually a unit, including contiguous modifiers such as tolerances, 'approximately' or '<'; e.g. '355 ml', 'five' samples, 'room temperature'.",
"description_source":... |
H-band slit-viewing VLT images taken on 6 November 2011 UT, just two days before the close approach of BS1 and BS2. (The relatively poor quality of the images arises from optimization of image quality for the science detector, which records spectra, instead of the slit viewing detector. When these images were taken, bo... | {
"entities": {
"quantity": [
{
"text": "6 November 2011 UT",
"start": 40,
"end": 58
},
{
"text": "two days",
"start": 65,
"end": 73
},
{
"text": "30 min",
"start": 596,
"end": 602
}
],
"measured pr... | {
"entities": [
{
"label": "quantity",
"description": "A count, consisting of a value, or a measurement, consisting of a value and usually a unit, including contiguous modifiers such as tolerances, 'approximately' or '<'; e.g. '355 ml', 'five' samples, 'room temperature'.",
"description_source":... |
The observed peak in the fractional integrated differential brightness of BS1 in the H filter was observed to be 0.64% in the discovery image on 26 October 2011, and declined to 0.02% by December 16. | {
"entities": {
"quantity": [
{
"text": "0.64%",
"start": 113,
"end": 118
},
{
"text": "26 October 2011",
"start": 145,
"end": 160
},
{
"text": "0.02%",
"start": 178,
"end": 183
},
{
"text": "... | {
"entities": [
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"description_source":... |
Notice also that background ∣B∣ is similar to what is measured at all flybys except R1. During the latter, ∣B∣ was on average 3–4 nT stronger compared to all other flybys. | {
"entities": {
"quantity": [
{
"text": "average 3–4 nT",
"start": 118,
"end": 132
}
],
"measured property": [
{
"text": "stronger",
"start": 133,
"end": 141
}
],
"measured entity": [
{
"text": "∣B∣",
"st... | {
"entities": [
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"description_source":... |
Observed deviations from the typical, plasma-absorbing interaction region profile may explain some differences. These deviations do not necessarily mean the main interaction mode at Rhea is not plasma absorption. For instance, Simon et al. (2012) demonstrates that the combination of low magnetosonic Mach number and the... | {
"entities": {
"quantity": [
{
"text": "One",
"start": 495,
"end": 498
}
],
"measured entity": [
{
"text": "features",
"start": 508,
"end": 516
}
]
},
"relations": {
"has quantity": [
{
"head": {
"... | {
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{
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"description_source":... |
plasma ions, appear to also have an impact on the wake dynamics (Halekas et al., 2011). For instance, the self-pick up process has been shown to lead to enhanced ULF wave activity in the lunar, at least 10% of the time (Nakagawa et al., 2012). Whether a similar process is important the inferred instability at Rhea is q... | {
"entities": {
"quantity": [
{
"text": "at least 10%",
"start": 194,
"end": 206
}
],
"measured entity": [
{
"text": "enhanced ULF wave activity in the lunar",
"start": 153,
"end": 192
}
],
"measured property": [
{
... | {
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"description": "A count, consisting of a value, or a measurement, consisting of a value and usually a unit, including contiguous modifiers such as tolerances, 'approximately' or '<'; e.g. '355 ml', 'five' samples, 'room temperature'.",
"description_source":... |
A new addition to the thermospheric energy equation is the inclusion of H3+ cooling, a process known to be important on Jupiter (Miller et al., 2006, 2010). At thermospheric temperatures typically found on Saturn (320–500 K, Nagy et al., 2009), we do not expect H3+ cooling to play an important role, but we included the... | {
"entities": {
"quantity": [
{
"text": "320–500 K",
"start": 214,
"end": 223
},
{
"text": "above ∼500 K",
"start": 430,
"end": 442
}
],
"measured property": [
{
"text": "thermospheric temperatures",
"start": 160... | {
"entities": [
{
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"description_source":... |
Density profiles O and H based on the C2 model (Paper I) and the density profile of H based on the empirical model of K10 with a mean temperature of 7200 K. | {
"entities": {
"quantity": [
{
"text": "7200 K",
"start": 149,
"end": 155
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],
"measured property": [
{
"text": "mean temperature",
"start": 129,
"end": 145
}
],
"measured entity": [
{
"text": "empirical model o... | {
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"description_source":... |
Moutou et al. (2001) looked for absorption by species such as Na,H,He,CH+,CO+,N2+, and H2O+ in the upper atmosphere of HD209458b. These observations were followed by Moutou et al. (2003) who attempted to measure the transit depth in the He 1083 nm line that was predicted to be significant by Seager and Sasselov (2000).... | {
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"quantity": [
{
"text": "1083 nm",
"start": 240,
"end": 247
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],
"measured property": [
{
"text": "line",
"start": 248,
"end": 252
}
],
"measured entity": [
{
"text": "He",
"start": 237,
... | {
"entities": [
{
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"description": "A count, consisting of a value, or a measurement, consisting of a value and usually a unit, including contiguous modifiers such as tolerances, 'approximately' or '<'; e.g. '355 ml', 'five' samples, 'room temperature'.",
"description_source":... |
MeasEval
MeasEval (named entity recognition and relation extraction), rebuilt for MNEB from the original release with character-level offsets.
Source: https://github.com/harperco/MeasEval (commit 1fa738b6, official TSV annotations)
| config | split | records |
|---|---|---|
| default | train | 297 |
| default | validation | 92 |
| default | test | 170 |
Labels
entities: quantity, measured entity, measured property, qualifier
relations: has quantity, has property, qualifies
Format
Each record has input (the text), output (gold annotations grouped by label) and schema (the label set with descriptions). Offsets are character offsets into input, half-open [start, end).
"output": {
"entities": {"<label>": [{"text", "start", "end"}]},
"relations": {"<label>": [{"head": {"text", "start", "end"},
"tail": {"text", "start", "end"}}]},
"events": {"<label>": [{"trigger": {"text", "start", "end"},
"arguments": [{"role", "text", "start", "end"}]}]}
}
Each schema item has a description and a description_source: official when adapted from the dataset's paper or guideline, mneb when written for MNEB. Relation datasets also give setting (end_to_end or gold_entity) and negative_label; relation items give symmetric. Event items list the roles valid for that event type.
Within a record, identical annotations are kept once and outer whitespace is trimmed from spans; source annotations are otherwise kept as annotated.
Notes
- Licence: not stated for the annotations; the texts are CC BY ScienceDirect articles.
- test =
eval, train =train, validation =trial. - Documents longer than 1,200 characters are cut at whitespace outside every annotated span (CalOn, arXiv:2610.17113); annotations whose parts fall in different pieces are dropped and counted.
- Units, normalised values and modifiers are not kept.
Build
Built by scripts/datasets/meas_eval.py in the MNEB repository.
Citation
Harper et al. (2021), SemEval-2021 Task 8: MeasEval - Extracting Counts and Measurements and their Related Contexts. SemEval.
License: not stated by the source; see the original release.
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