Abstract. Nutrient resorption in plants influences nutrient availability and cycling and is a key process in biogeochemical models. Improved estimates of resorption parameters are needed for predicting long-term primary productivity and for improving such models. Currently, most models assume a value of 50% resorption for nitrogen (N) and phosphorus (P) and lack resorption data for other nutrients and for specific vegetation types. We provide global estimates of resorption efficiencies and nutrient concentrations for carbon (C), N, and P and the first global-scale estimates for essential nutrients such as potassium (K), calcium (Ca), and magnesium (Mg). We also examine leaf mass loss during senescence (LML) globally and for different plant types, thus defining a mass loss correction factor (MLCF) needed to quantify unbiased resorption values. We used a global meta-analysis of 86 studies and ;1000 data points across climates for green and senesced leaves in six plant types: ferns, forbs, graminoids, conifers, and evergreen and deciduous woody angiosperms. In general, N and P resorption differed significantly from the commonly used global value of 50% (62.1%, 64.9%, respectively; P , 0.05). Ca, C, and Mg showed lower average resorptions of 10.9%, 23.2%, and 28.6%, respectively, while K had the highest resorption, at 70.1%. We also found that resorption of all nutrients except Ca depended on leaf nutrient-status; globally, C, N, P, K, and Mg showed a decrease in resorption with increased nutrient status. On average, global leaf mass loss was 24.2%. Overall, our resorption data differ substantially from commonly assumed values and should help improve ecological theory and biogeochemical and landsurface models.

Highly weathered kaolinitic soils in Brazil often have adequate levels of K and Mg to support plant growth. The source of K and Mg in these soils and their relationship with the dominant mineral, kaolinite, is addressed in this article. Crystallographic, chemical, and morphological properties of kaolinite, from selected highly weathered Brazilian soils, were investigated by x‐ray diffraction (XRD), analytical electron microscopy (AEM), chemical, and thermal methods. Kaolinite properties showed significant variations such as d(001) spacing ranging between 0.713 to 0.728 nm, width at half height (WHH) between 0.30 to 0.97 °2θ, and dehydroxylation temperature between 489 to 518°C. Kaolinite in the clay fraction has relatively poor crystal order with a mean crystallinity index value(CI) of 12.7. The dominant forms of the clay‐fraction kaolinite were elongated and rounded, with relatively lower proportions of hexagonal particles. The silt‐fraction kaolinite showed a tendency to form subspherical large aggregates with high stability. The average Fe2O3 level in the kaolinite of the clay fraction (19.1 g kg−1) was higher than that obtained for the silt fraction (6.6 g kg−1). The smaller kaolinite particles of the clay fraction showed a lower degree of crystal order, higher K and Mg levels, and lower dehydroxylation temperatures. From the strong relationship between the asymmetry index (AI) of the (001) diffraction line and the level of K in kaolinite from the younger soils, we believe that both K and Mg in kaolinite are part of residual micaceous layers interleaved in kaolinite crystals.

RESUMOPara avaliar as características dos óxidos de ferro e de alumínio, foram coletadas amostras de solos desenvolvidos de diferentes materiais de origem e estádios de desenvolvimento nos estados de MG, ES, RS e RR. A fração argila das amostras foi estudada por difratometria de raios-X (DRX), análise termodiferencial (ATD), análise termogravimétrica diferencial (ATGD) e microscopia eletrônica. Nos extratos resultantes da extração com oxalato de amônio (OA) e ditionito-citrato-bicarbonato (DCB), determinaram-se os teores de Al, Si e microelementos, inclusive Fe. Em geral, a goethita (Gt) foi o principal óxido de ferro da fração argila. Apenas para os solos desenvolvidos de basalto e de arenito, verificou-se o predomínio de hematita (Hm). Os solos do Grupo Barreiras (ES) apresentaram os menores teores de óxidos de ferro em decorrência do intenso processo de desferrificação sofrido pelos sedimentos. Por ser a Gt um óxido hidratado, quanto maior a relação Gt/(Gt + Hm), maior o teor de água extraída pelo DCB (r = 0,70 *** ). Os solos menos desenvolvidos, principalmente no horizonte C, apresentaram os maiores teores de material menos cristalino extraído pelo OA (chegando a 28% para a amostra 17) e os maiores valores para a relação FeOA/FeDCB. Este material menos cristalino é constituído principalmente por Al, com menor participação de Fe. Parte das amostras apresentou valores próximos para o diâmetro médio do cristal (DMC) da Gt nas direções (110) e (111), indicando formato isodimensional do mineral. Os maiores valores de DMC para a Hm resultaram na menor superfície específica em relação à Gt. A substituição isomórfica de Fe por Al (SI) na Gt foi consideravelmente superior à da Hm (média de 218 e 85 mmol mol -1 , respectivamente). Com a entrada de Al na estrutura da Gt, verificou-se redução no tamanho, principalmente na

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Aluminum (Al) tolerance mechanisms in crop plants have been extensively researched, but our understanding of the physiological mechanisms underlying Al tolerance in trees is still limited. To investigate Al tolerance in eucalypts, seedlings of six species (Eucalyptus globulus Labill., Eucalyptus urophylla S.T. Blake, Eucalyptus dunnii Maiden, Eucalyptus saligna Sm., Eucalyptus cloeziana F. J. Muell. and Eucalyptus grandis w. Hill ex Maiden) and seedlings of six clones of Eucalyptus species were grown for 10 days in nutrient solutions containing Al concentrations varying from 0 to 2.5 microM (0 to 648 microM Al3+ activities). Root elongation of most species was inhibited only by high Al3+ activities. Low to intermediate Al3+ activities were beneficial to root elongation of all species and clones. Among the species tested, E. globulus and E. urophylla were more tolerant to Al toxicity, whereas E. grandis and E. cloeziana were more susceptible to Al-induced damage. Although E. globulus seedlings were tolerant to Al toxicity, they were highly sensitive to lanthanum (La), indicating that the tolerance mechanism is specific for Al. Fine roots accumulated more Al and their elongation was inhibited more than that of thick roots. In E. globulus, accumulation of Al in root tips increased linearly with increasing Al concentration in the nutrient solution. The majority of Al taken up was retained in the root system, and the small amounts of Al translocated to the shoot system were found mainly in older leaves. No more than 60% of the Al in the thick root tip was in an exchangeable form in the apoplast that could be removed by sequential citrate rinses. Gas chromatography/mass spectrometry and ion chromatography analyses indicated that root exposure to Al led to a greater than 200% increase in malic acid concentration in the root tips of all eucalypt species. The increase in malate concentration in response to Al treatment correlated with the degree of Al tolerance of the species. A small increase in citric acid concentration was also observed in all species, but there were no consistent changes in the concentrations of other organic acids in response to Al treatment. In all eucalypt species, Al treatment induced the secretion of citric and malic acid in root exudates, but no trend with respect to Al tolerance was observed. Thus, although malate and citrate exudation by roots may partially account for the overall high Al tolerance of these eucalypt species, it appears that tolerance is mainly derived from the internal detoxification of Al by complexation with malic acid.