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Institution

University of Maine

EducationOrono, Maine, United States
About: University of Maine is a education organization based out in Orono, Maine, United States. It is known for research contribution in the topics: Population & Ice sheet. The organization has 8637 authors who have published 16932 publications receiving 590124 citations. The organization is also known as: University of Maine at Orono.


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Journal ArticleDOI
22 Jan 1999-Science
TL;DR: The authors investigated possible causal connections between these simultaneous developments and are finding a complex pattern of cultural responses to climatic change between about 8000 and 3000 years ago, and found that human cultures experienced a period of substantial progress toward more complex societies, as exemplified by the first temple mounds in South America, the Egyptian pyramids and the rise and fall of civilizations in East Asia.
Abstract: Between about 8000 and 3000 years ago, climate worldwide underwent substantial changes. At the same time, human cultures experienced a period of substantial progress toward more complex societies, as exemplified by the first temple mounds in South America, the Egyptian pyramids, and the rise and fall of civilizations in East Asia. Archeologists and paleoclimotologists alike are now investigating possible causal connections between these simultaneous developments and are finding a complex pattern of cultural responses to climatic change.

154 citations

Journal ArticleDOI
TL;DR: The molybdenum blue method of Dick and Tabatabai in 1977 reduced errors pertaining to nonenzymatic hydrolysis of organic phosphorus (Po) as discussed by the authors.
Abstract: In characterizing organic phosphorus (Po) by phosphatase hydrolysis, the quantity of hydrolyzable Po is represented by the difference in orthophosphate [i.e., inorganic P (Pi)] determined after and prior to enzymatic incubation. Therefore, precise determination of Pi is of major importance for accurate application of the enzymatic hydrolysis approach. The strong acid conditions required for conventional molybdenum blue methods interferes with Pi determination due to rapid hydrolysis of labile Po and precipitation of enzymes (proteins). The molybdenum blue method of Dick and Tabatabai in 1977 reduced errors pertaining to nonenzymatic hydrolysis of Po. This study revisited the method, finding that the absorption coefficient at 850 nm was 45–49% higher than at 700 nm, and linear up to at least 80 nmol Pi in 1‐mL assay solution. Therefore, adaptation of the readings at 850 nm improved the sensitivities of Pi determination by about 45%. Enzyme precipitation during Pi determination was prevented by add...

154 citations

Journal ArticleDOI
TL;DR: Sir: Observer effects are rooted in the universal human tendency to interpret data in a manner consistent with one’s expectations, and can result in false inclusions under not uncommon conditions of ambiguity encountered in actual casework.
Abstract: Sir: Observer effects are rooted in the universal human tendency to interpret data in a manner consistent with one’s expectations (1). This tendency is particularly likely to distort the results of a scientific test when the underlying data are ambiguous and the scientist is exposed to domain-irrelevant information that engages emotions or desires (2). Despite impressions to the contrary, forensic DNA analysts often must resolve ambiguities, particularly when interpreting difficult evidence samples such as those that contain mixtures of DNA from two or more individuals, degraded or inhibited DNA, or limited quantities of DNA template. The full potential of forensic DNA testing can only be realized if observer effects are minimized. We met on December 1 and 2, 2007 in Washington, D.C. to discuss the implications of observer effects in forensic DNA testing and ways to minimize them. The interpretation of an evidentiary DNA profile should not be influenced by information about a suspect’s DNA profile (3–6). Each item of evidence must be interpreted independently of other items of evidence or reference samples. Yet forensic analysts are commonly aware of submitted reference profiles when interpreting DNA test results, creating the opportunity for a confirmatory bias, despite the best intentions of the analyst. Furthermore, analysts are sometimes exposed to information about the suspects, such as their history or motives, eyewitness identifications, presence or absence of a confession, and the like. Such information should have no bearing on how the results of a DNA test are interpreted, yet may compound an unintentional confirmatory bias. This bias can result in false inclusions under not uncommon conditions of ambiguity encountered in actual casework. It can also render currently used frequency statistics or likelihood ratios misleading. These problems can be minimized by preventing analysts from knowing the profile of submitted references (i.e., known samples) when interpreting testing results from evidentiary (i.e., unknown or questioned) samples. The necessary filtering or masking of submitted reference profiles can be accomplished in several ways, perhaps most easily by sequencing the laboratory workflow such that evidentiary samples are interpreted, and the interpretation is fully documented, before reference samples are compared. A simple protocol would dictate a separation of tasks between a qualified individual familiar with case information (a case manager) and an analyst from whom domain-irrelevant information is masked. Such a protocol would have the following steps. First, the analyst interprets the results of testing on the evidentiary samples. In this initial interpretation, the analyst would perform the following:

154 citations

Journal ArticleDOI
TL;DR: Drought-induced reductions in tree growth were greatest when the droughts occurred during early- season peaks in radial growth, especially for trees growing in the warmest, driest regions, and it is found that future increases in early-season PET may exacerbate these effects, and potentially offset gains in C uptake and storage in ENA owing to other global change factors.
Abstract: Projected changes in temperature and drought regime are likely to reduce carbon (C) storage in forests, thereby amplifying rates of climate change. While such reductions are often presumed to be greatest in semi-arid forests that experience widespread tree mortality, the consequences of drought may also be important in temperate mesic forests of Eastern North America (ENA) if tree growth is significantly curtailed by drought. Investigations of the environmental conditions that determine drought sensitivity are critically needed to accurately predict ecosystem feedbacks to climate change. We matched site factors with the growth responses to drought of 10,753 trees across mesic forests of ENA, representing 24 species and 346 stands, to determine the broad-scale drivers of drought sensitivity for the dominant trees in ENA. Here we show that two factors-the timing of drought, and the atmospheric demand for water (i.e., local potential evapotranspiration; PET)-are stronger drivers of drought sensitivity than soil and stand characteristics. Drought-induced reductions in tree growth were greatest when the droughts occurred during early-season peaks in radial growth, especially for trees growing in the warmest, driest regions (i.e., highest PET). Further, mean species trait values (rooting depth and ψ50 ) were poor predictors of drought sensitivity, as intraspecific variation in sensitivity was equal to or greater than interspecific variation in 17 of 24 species. From a general circulation model ensemble, we find that future increases in early-season PET may exacerbate these effects, and potentially offset gains in C uptake and storage in ENA owing to other global change factors.

154 citations

Journal ArticleDOI
TL;DR: Results indicate that formamide has a destabilizing effect on the helical state, and that sequence-dependent variations in hydration patterns are primarily responsible for small variations in sensitivity to the denaturant.
Abstract: Formamide lowers melting temperatures (Tm) of DNAs linearly by 2.4-2.9 degrees C/mole of formamide (C(F)) depending on the (G+C) composition, helix conformation and state of hydration. The inherent cooperativity of melting is unaffected by the denaturant. dTm/dC(F)for 11 plasmid domains of 0.23 coil transitions. Results indicate that formamide has a destabilizing effect on the helical state, and that sequence-dependent variations in hydration patterns are primarily responsible for small variations in sensitivity to the denaturant. The average unit transition enthalpy delta H(m)[see text for complete expression], exhibits a biphasic dependence on formamide concentration. The initial drop of -0.8 kcal/mol bp at low formamide concentrations is attributable to a delta delta H(m)[see text for complete expression], for exchange of solvent in the vicinity of the helix: displacement by formamide of weakly bound hydrate or counterion. The phenomenological effects are equivalent to lowering the bulk counterion concentration. Poly(dA.dT) exhibits a much lower sensitivity to formamide, due to the specific pattern of tightly bound, immobilized water bridges that buttress the helix from within the narrow minor groove. Tracts of three (A.T)-pairs behave normally, but tracts of six exhibit the same level of reduced sensitivity as the polymer, suggesting a conformational shift as tracts are elongated beyond some critical length [McCarthy J.G. and Rich,A. (1991) Nucleic Acids Res. 19, 3421-3429].

153 citations


Authors

Showing all 8729 results

NameH-indexPapersCitations
Clifford J. Rosen11165547881
Juan S. Bonifacino10830346554
John D. Aber10720448500
Surendra P. Shah9971032832
Charles T. Driscoll9755437355
Samuel Madden9538846424
Lihua Xiao9349532721
Patrick G. Hatcher9140127519
Pedro J. J. Alvarez8937834837
George R. Pettit8984831759
James R. Wilson89127137470
Steven Girvin8636638963
Peter Marler8117422070
Garry R. Buettner8030429273
Paul Andrew Mayewski8042029356
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Performance
Metrics
No. of papers from the Institution in previous years
YearPapers
202332
2022134
2021834
2020756
2019738
2018725