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G M MacDonald

Publications and source records attributed to G M MacDonald.

9 recordsLinked to original sources

Disappearing Arctic lakes.

Historical archived satellite images were compared with contemporary satellite data to track ongoing changes in more than 10,000 large lakes in rapidly warming Siberia. A widespread decline in lake abundance and area has occurred since 1973, despite slight precipitation increases to the region. The spatial pattern of lake disappearance suggests (i) that thaw and "breaching" of permafrost is driving the observed losses, by enabling rapid lake draining into the subsurface; and (ii) a conceptual model in which high-latitude warming of permafrost triggers an initial but transitory phase of lake and wetland expansion, followed by their widespread disappearance.

Journal Article↗

Siberian peatlands a net carbon sink and global methane source since the early Holocene.

Interpolar methane gradient (IPG) data from ice cores suggest the "switching on" of a major Northern Hemisphere methane source in the early Holocene. Extensive data from Russia's West Siberian Lowland show (i) explosive, widespread peatland establishment between 11.5 and 9 thousand years ago, predating comparable development in North America and synchronous with increased atmospheric methane concentrations and IPGs, (ii) larger carbon stocks than previously thought (70.2 Petagrams, up to approximately 26% of all terrestrial carbon accumulated since the Last Glacial Maximum), and (iii) little evidence for catastrophic oxidation, suggesting the region represents a long-term carbon dioxide sink and global methane source since the early Holocene.

Journal Article↗

A difference Fourier transform infrared spectroscopic study of chlorophyll oxidation in hydroxylamine-treated photosystem II.

In oxygenic photosynthesis, photosystem II is the chlorophyll-containing reaction center that carries out the light-induced transfer of electrons from water to plastoquinone. Fourier transform infrared spectroscopy can be used to obtain information about the structural changes that accompany electron transfer in photosystem II. The vibrational difference spectrum associated with the reduction of photosystem II acceptor quinones is of interest. Previously, a high concentration of the photosystem II donor, hydroxylamine, has been used to obtain a spectrum attributed to QA- -QA (Berthomieu, C., Nabedryk, E., Mantele, W. and Breton, J. FEBS Lett. (1990) 269, 363). Here, we use electron paramagnetic resonance, Fourier transform infrared spectroscopy, and 15N isotopic labeling to show that the difference infrared spectrum, obtained under these conditions, also exhibits a contribution from the oxidation of chlorophyll.

Chlorophyll↗

A difference infrared study of hydrogen bonding to the Z. tyrosyl radical of photosystem II.

Photosystem II, the photosynthetic water oxidizing complex, contains two well characterized redox active tyrosines, D and Z. D forms a stable radical of unknown function. Z is an electron carrier between the primary chlorophyll donor and the manganese catalytic site. The vibrational difference spectra associated with the oxidation of tyrosines Z and D have been obtained through the use of infrared spectroscopy (MacDonald, G. M., Bixby, K.A., and Barry, B.A. (1993) Proc. Natl. Acad. Sci. U.S.A. 90, 11024-11028). Here, we examine the effect of deuterium exchange on these vibrational difference spectra. While the putative C-O vibration of stable tyrosine radical D. downshifts in 2H2O, the putative C-O vibration of tyrosine radical Z. does not. This result is consistent with the existence of a hydrogen bond to the phenol oxygen of the D. radical; we conclude that a hydrogen bond is not formed to the Z. radical. In an effort to identify the amino acid residue that is the proton acceptor for Z, we have performed global 15N labeling. While significant 15N shifts are observed in the vibrational difference spectrum, substitution of a glutamine for a histidine that is predicted to lie in the environment of tyrosine Z has little or no effect on the difference infrared spectrum. There is also no significant change in the yield or lineshape of the Z. EPR signal under continuous illumination in this mutant. Our results are inconsistent with the possibility that this residue, histidine 190 of the D1 polypeptide, acts as the sole proton acceptor for tyrosine Z.

Cyanobacteria↗

Dedicated short-stay spinal unit.

Prolonged waiting periods for patients with benign spinal surgical lesions led to the creation of a Dedicated Short Stay Spinal Surgical Unit. This unit was implemented in November, 1992, on a 29 bed Neuroscience Unit in a 1200 bed Acute Care Teaching Hospital. Considerations for implementation were many, including psychological impact of chronic pain for patients on prolonged waiting lists, the increased probability of permanent waiting lists, the increased probability of permanent neurological deficits, and the economic impact to patient, societal and hospital budgets. This paper will focus on explanation of the design of the unit, define the benefits and provide study results of the first 85 patients admitted to the unit.

Adult↗

Comparison of cytochrome b-559 content in photosystem II complexes from spinach and Synechocystis species PCC 6803.

Cytochrome b-559 is an integral component of photosystem II complexes from both plants and cyanobacteria. However, the number of cytochrome b-559 associated with the photosystem II reaction center has been the subject of controversy. Some studies have concluded that there is one heme equivalent of cytochrome b-559 per reaction center, some studies have found two, and some studies have reported intermediate values. Most of the previous experiments have used only one method to quantitate the antenna size of the preparation. In this study, we compare the cytochrome b-559 content in a cyanobacterial and a plant photosystem II preparation. The plant preparation is derived from spinach, and previous work has shown that it has an antenna size of approximately 100 chlorophylls [MacDonald, G. M., & Barry, B. A. (1992) Biochemistry 31, 9848-9856]. The cyanobacterial preparation is from Synechocystis sp. PCC 6803, and previous work has shown that it has an antenna size of approximately 60 chlorophylls [Noren, G. H., Boerner, R. J., & Barry, B. A. (1991) Biochemistry 30, 3943-3950]. Both preparations are isolated through the use of ion-exchange chromatography, and both preparations are monodisperse in the same nonionic detergent. In our comparative study, we quantitate antenna size by three different methods. Our work shows that, depending on the method used to estimate antenna size, the oxygen-evolving spinach photosystem II preparation contains 0.82-1.0 cytochrome b-559 per reaction center, while the oxygen-evolving cyanobacterial preparation contains 1.5-2.1 cytochrome b-559 per reaction center.

Cyanobacteria↗

A difference Fourier-transform infrared study of two redox-active tyrosine residues in photosystem II.

Photosystem II, the photosynthetic water-oxidizing complex, contains two redox-active tyrosine residues. Although current models suggest that these tyrosines are located in symmetric positions in the reaction center, there are functional differences between them. To elucidate those structural factors that give rise to this functional asymmetry, we have used difference Fourier-transform infrared spectroscopy to obtain the vibrational difference spectrum associated with the oxidation of each of these redox-active residues. Isotopic labeling was employed to definitively assign vibrational lines to the redox-active tyrosines. This work has shown that the vibrational spectra of the two redox-active species are significantly different from each other. This result suggests that the structure of the redox-active residue helps to determine its role in electron transfer in the reaction center.

Cyanobacteria↗

Difference FT-IR study of a novel biochemical preparation of photosystem II.

There are two redox-active tyrosines in photosystem II, the water-splitting complex, that form neutral tyrosine radicals. One of these tyrosine radicals, D., is stable and has an unknown function. The other redox-active tyrosine, Z, acts to transfer oxidizing equivalents from the primary chlorophyll donor of photosystem II to the manganese cluster, where water oxidation occurs. In an attempt to obtain more information about Z and its interaction with its environment, we have begun a study using Fourier-transform infrared (FT-IR) vibrational spectroscopy. To facilitate these studies, we have developed a procedure to isolate spinach photosystem II complexes with an antenna size of approximately 100-110 chlorophylls per reaction center. These complexes show an approximately 2-fold increase in the specific activity of oxygen evolution over the activity of the starting material, photosystem II membranes. Although fully solubilized in detergent, these complexes retain the 24- and 18-kDa extrinsic proteins and exhibit no calcium chloride requirement for optimal oxygen evolution. In manganese-depleted photosystem II samples, Z. can be accumulated in the light. In the dark, the tyrosine radical is reduced and reprotonated to form the neutral tyrosine. Since this process is reversible and light-dependent, we have used light-minus-dark difference FT-IR spectroscopy to observe the vibrational difference spectrum that is associated with the oxidation of this residue. As a control, EPR spectra were measured under identical conditions to assess the amount of Z. that accumulated in the light. We also hope to use difference FT-IR to identify the amino acid with which Z may form a hydrogen bond.(ABSTRACT TRUNCATED AT 250 WORDS)

Electron Spin Resonance Spectroscopy↗