Climatic and local effects on stalagmite δC values at Lianhua Cave, China

Carbon isotopes in speleothems may serve as indicators of vegetative change, climatic conditions, and karst processes. In many recent studies of Chinese stalagmites, however, carbon isotopes have often been neglected or underutilized in interpreting paleoenvironments. Here, we present a continuous decadal-scale δ¹³C record (819 measurements) of the mid- to late-Holocene from a precisely-dated (10 ²³⁰Th dates) aragonite stalagmite from Lianhua Cave, Hunan Province, China. Compared to coeval stalagmites from other Chinese caves, the average δ¹³C value (− 3.6‰) of stalagmite A1 is higher by ~ 2–7‰. Variations in the δ¹³C values (0.1‰ to − 6.0‰) reflect changes in both vegetative productivity and inorganic processes, which respond to climatic processes. The δ¹³C record of stalagmite A1 can be subdivided into three intervals: 1) warm–humid stage (6.6 to 3.8 ka); 2) transitional stage (3.8 to 1.6 ka); and 3) cool–arid stage (1.6 ka to present). Comparisons with other stalagmite and paleoclimatic records demonstrate that these intervals are generally consistent with changes in regional vegetation and climatic conditions.     

Variation in δC values for the seagrass Thalassia testudinum and its relations to mangrove carbon

Carbon isotope ratios (¹³C/¹²C) were measured for the leaves of the seagrass Thalassia testudinum Banks ex König and carbonates of shells collected at the seagrass beds from seven sites along the coast of southern Florida, U.S.A. The δ¹³C values of seagrass leaves ranged from −7.3 to −16.3‰ among different study sites, with a significantly lower mean value for seagrass leaves from those sites near mangrove forests (−12.8 ± 1.1‰) than those far from mangrove forests (−8.3 ± 0.9‰; P < 0.05). Furthermore, seagrass leaves from a shallow water area had significantly lower δ¹³C values than those found in a deep water area (P < 0.01). There was no significant variation in δ¹³C values between young and mature leaves (P = 0.59) or between the tip and base of a leaf blade (P = 0.46). Carbonates of shells also showed a significantly lower mean δ¹³C value in the mangrove areas (−2.3 ± 0.6‰) than in the non-mangrove areas (0.6 ± 0.3‰; P <0.025). In addition, the δ¹³C values of seagrass leaves were significantly correlated with those of shell carbonates (δ¹³C seagrass leaf = −9.1 + 1.3δ¹³C shell carbonate (R² = 0.83, P < 0.01)). These results indicated that the input of carbon dioxide from the mineralization of mangrove detritus caused the variation in carbon isotope ratios of seagrass leaves among different sites in this study.     

Antinoceptive effect of triterpenoid α,β-amyrin in rats on orofacial pain induced by formalin and capsaicin

The effects of α,β-amyrin, a pentacyclic triterpene isolated from Protium heptaphylum was investigated on rat model of orofacial pain induced by formalin or capsaicin. Rats were pretreated with α,β-amyrin (10, 30, and 100 mg/kg, i.p.), morphine (5 mg/kg, s.c.) or vehicle (3% Tween 80), before formalin (20 μl, 1.5%) or capsaicin (20 μl, 1.5 μg) injection into the right vibrissa. In vehicle-treated controls, formalin induced a biphasic nociceptive face-rubbing behavioral response with an early first phase (0–5 min) and a late second phase (10–20 min) appearance, whereas capsaicin produced an immediate face-rubbing (grooming) behavior that was maximal at 10–20 min. Treatment with α,β-amyrin or morphine significantly inhibited the face-rubbing response in both test models. While morphine produced significant antinociception in both phases of formalin test, α,β-amyrin inhibited only the second phase response, more prominently at 30 mg/kg, in a naloxone-sensitive manner. In contrast, α,β-amyrin produced much greater antinociceptive effect at 100 mg/kg in the capsaicin test, which was also naloxone-sensitive. These results provide first time evidence to show that α,β-amyrin attenuates orofacial pain atleast, in part, through a peripheral opioid mechanism but warrants further detailed study for its utility in painful orofacial pathologies.     

Changes in leaf δC and δN for three Mediterranean tree species in relation to soil water availability

A rain exclusion experiment simulating drought conditions expected in Mediterranean areas for the following decades (15% decrease in soil moisture) was conducted in a Mediterranean holm oak forest to study the response of leaf δ¹³C, δ¹⁵N, and N concentrations to the predicted climatic changes for the coming decades. Plant material was sampled in 2000, 2003, 2004, and 2005 in eight plots: four of them were control plots and the other four plots received the rain exclusion treatment. Although there was a negative relationship between δ¹³C and soil moisture, for each species and year, the rain exclusion treatment did not have any significant effect on δ¹³C, and therefore on the intrinsic water use efficiency (iWUE) of the three dominant species: Phillyrea latifolia, Arbutus unedo, and Quercus ilex. On the other hand, rain exclusion clearly increased the δ¹⁵N values in the three species studied, probably indicating higher N losses at the soil level leading to a ¹⁵N enrichment of the available N. It suggested that rain exclusion exerted a greater effect on the nitrogen biogeochemical cycle than on the carbon assimilation process. δ¹⁵N values were inversely correlated with summer soil moisture in Q. ilex and A. unedo, but no relationship was observed in P. latifolia. This latter species showed the lowest iWUE values, but it was the only species with no decrease in annual basal increment in response to the rain exclusion treatment, and it also had the highest resistance to the hot and dry conditions projected for the Mediterranean basin in the coming decades. The different strategies to resist rain exclusion conditions of these species could induce changes in their competitive ability and future distribution. The losses of N from the ecosystem may further limit plant growth and ecosystem functioning.     

Phosphorylations of αA- and αB-crystallin

In addition to being refractive proteins in the vertebrate lens, the two α-crystallin polypeptides (αA and αB) are also molecular chaperones that can protect proteins from thermal aggregation. The αB-crystallin polypeptide, a functional member of the small heat shock family, is expressed in many tissues in a developmentally regulated fashion, is stress-inducible, and is overexpressed in many degenerative diseases and some tumors indicating that it plays multiple roles. One possible clue to α-crystallin functions is the fact that both polypeptides are phosphorylated on serine residues by cAMP-dependent and cAMP-independent mechanisms. The cAMP-independent pathway is an autophosphorylation that has been demonstrated in vitro, depends on magnesium and requires cleavage of ATP. Disaggregation of αA-, but not αB-crystallin into tetramers results in an appreciable increase in autophosphorylation activity, reminiscent of other heat shock proteins, and suggests the possibility that changes in the aggregation state of αA-crystallin are involved in yet undiscovered signal transduction pathways. The α-crystallin polypeptides differ with respect to their abilities to undergo cAMP-dependent phosphorylation, with preference given to the αB-crystallin chain. These differences and complexities in α-crystallin phosphorylations, coupled with the differences in expression patterns of the two α-crystallin polypeptides, are consistent with the idea that each polypeptide has distinctive structural and metabolic roles.     

Differential steric effects in the axial ligation of pyridine and imidazole to α- and β-alkylcobinamides

One subclass of B₁₂-requiring enzymes is now known to bind their B₁₂ coenzymes “base-off,” with a histidine residue from the protein supplying an imidazole ligand to the cobalt center. Recent results from Sirovatka and Finke (J.M. Sirovatka and R.G. Finke, J.Am. Chem. Soc. 119, (1997) 3057) show that imidazole has an extraordinary trans effect on the mode of carbon–cobalt bond cleavage in coenzyme B₁₂ analogs, compared to pyridine or the natural 5,6-dimethylbenzimidazole ligand, and it was suggested that a differential steric effect could, in part, account for the uniqueness of the imidazole ligand. Such a differential steric effect for imidazole and pyridine is now demonstrated by studies of the thermodynamics of ligation of these ligands to the α and β diastereomers of two alkylcobinamides (RCbi⁺s, derivatives of cobalamins which lack the normal axial nucleotide) based on the known differences in steric crowding of the α (“lower”) and β (“upper”) axial ligand positions of cobalt corrinoids. Imidazole binds more tightly than pyridine to both diastereomers of NCCH₂Cbi⁺ and CF₃Cbi⁺, in all cases due to a more favorable entropy change, which is the result of lowered steric interference with corrin side chain thermal motions.     

Cardiovascular actions of prostaglandins F2α; 15-me-F2α; F1α; F2β and F1β in the cat

Prostaglandin F_2α (5μg/kg, i.v.) causes an increase in pulmonary arterial pressure, decrease in systemic arterial pressure, and reflex bradycardia in the anesthetized cat. The same dose of the 15-methyl analogue of PGF_2α produces the same triad of effects but of greater magnitude and duration. Although prostaglandins F_1α, F_2β and F_1β also cause the same cardiovascular effects as F_2α, there is a decrease in potency for all parameters measured, with PGF_2α>PGF_1α>PGF_2β>PGF_1β. When compared to the actions of PGF_2α in producing an increase in pulmonary arterial pressure, PGs F_1α, F_2β and F_1β were less potent by approximately 10, 100, and 1000 fold respectively.     

η-N-succinimidato complexes of iron, molybdenum and tungsten as reversible inhibitors of papain

Recently we have found that the metallocarbonyl complexes (η⁵-C₅H₅)M(CO)_x(η¹-N-maleimidato) (M = Fe, Mo, W; x = 2 or 3) bearing a maleimide function were irreversible inhibitors of the enzyme papain. To get further insight into the binding mechanism of these compounds we synthesized the related complexes (η⁵-C₅H₅)M(CO)_x(η¹-N-succinimidato) (M = Fe, Mo, W; x = 2 or 3) that lacked the ethylenic bond responsible for alkylation of the cysteine 25 thiol group in the papain‘s catalytic pocket. We performed kinetic studies of the interaction of the synthesized complexes towards papain. We found that they act as reversible inhibitors of the enzyme with IC₅₀ values in the range 480–1700 μM. Docking experiments confirmed binding of these complexes to the enzyme’s catalytic pocket.     

Separation and concentration of Δ-6-keto-PGF1α using monoclonal antibody to ω3-olefin structure of trienoic prostanoids

A monoclonal antibody against cis-3-hexen-1-ol was prepared and used to separate and/or concentrate Δ¹⁷-6-keto-prostaglandin F_1α (PGF_1α) in the human sera. cis-3-Hexen-1-ol was conjugated with the human serum albumin (HSA) according to the N-succinimidylester method and hyperimmunized to BALB/c mouse. The monoclonal afntibodies were obtained from hybridoma clones established by a fusion between SP2/0-Ag14-k13 mouse myeloma cells and splenocytes of a mouse. A monoclonal antibody, named 4G9-12B, recognized the epitope characteristic for ω3-olefin structure. The 4G9-12B antibody became more specific for Δ¹⁷-6-keto-PGF_1α than 6-keto-PGF_1α by applying inhibition ELISA using amino-residue coating plates. Using the prepared immunoaffinity columns of this antibody, Δ¹⁷-6-keto-PGF_1α was clearly detected in 6 pg/ml of the human blood sera by GC/MS analysis. These results suggest that the monoclonal antibody to the partial structure of trienoic prostanoid, ω3-olefin unit, and that its immunoaffinity columns are useful in separating and concentrating Δ¹⁷-6-keto-PGF_1α in the human blood or urine.     

Organic matter rain rates, oxygen availability, and vital effects from benthic foraminiferal δC in the historic Skagerrak, North Sea

The sediment cores 225514 and 225510 were recovered from 420 and 285 m water depth, respectively. They were investigated for their benthic foraminiferal δ¹³C during the last 500 years. Both cores were recovered from the southern flank of the Skagerrak. The δ¹³C values of Uvigerina mediterranea and other shallow infaunal species in both cores indicate that organic matter rain rates to the seafloor varied around a mean value until approximately AD 1950 after which they increased. This increase might result from changes in the North Atlantic Current System and a co-occurring persistently high North Atlantic Oscillation index state in the 1980s to 1990s, rather than from anthropogenic eutrophication. Using δ¹³C mean values of multiple species, we reconstruct δ¹³C gradients of dissolved inorganic carbon (DIC) within pore waters for the time periods AD 1500 to 1950 and AD 1950 to 2000. The calculated δ¹³C_DIC ranges, interpreted as indicating total organic matter remineralization due to respiration, are generally bigger in Core 225514 than in Core 225510. Since mean δ¹³C values of U. mediterranea suggest that organic matter rain rates were similar at both locations, differences in total organic matter remineralization are attributed to differing oxygen availability. However, oxygen concentrations in the overlying bottom water masses are not likely to have differed significantly. Thus, we suggest that organic matter remineralization was controlled by oxygen availability within the sediments, reflecting strong differences in sedimentation rates at the two investigated core sites. Based on the assumptions that tests of benthic foraminiferal species inhabiting the same microhabitat depth should show equal δ¹³C values unless they are affected by vital effects and that Globobulimina turgida records pore water δ¹³C_DIC, we estimate microhabitat-corrected vital effects for several species with respect to G. turgida: > 0.7‰ for Cassidulina laevigata, > 1.3‰ for Hyalinea balthica, and > 0.7‰ for Melonis barleeanus. Melonis zaandami seems to closely record pore water δ¹³C_DIC.     

Homologous long-chain δ-lactones in leaf cuticular waxes of Cerinthe minor

A homologous series of eleven δ-lactones (1,5-alkanolides) was identified in cuticular waxes from leaves of Cerinthe minor L., six of them representing novel compounds. They accounted for 79% of the total coverage of 41 μg wax per cm² leaf area. Various chemical transformations with product identification by GC-mass spectrometry and GC-FTIR were employed to assign the structures. The chain-lengths of the δ-lactones ranged from C₂₂ to C₃₂ and even-numbered homologues were prevalent. Additionally, aldehydes (C₂₆–C₃₀), alkanes (C₂₃–C₂₉), primary alcohols (C₂₆–C₃₂), alkanoic acids (C₂₀–C₃₂), wax esters (C₄₀–C₅₆) and lupeol were detected.     

α2-macroglobulin ‘fast’ forms inhibit superoxide production by activated macrophages

Mouse peritoneal macrophages activated by bacillus Calmette-Guerin (BCG) were incubated with human α₂-macroglobulin converted to its ‘fast’ form with either trypsin or methylamine before being stimulated with phorbol myrystate acetate. Both α₂-macroglobulin-trypsin and α₂-macroglobulin-methylamine inhibited macrophage production of superoxide anion (O₂⁻) while native α₂-macroglobulin had little effect except at high concentration. The α₂-macroglobulin ‘fast’ forms, which bind with a K_d of about 8 nM, inhibited 50% generation of O₂⁻(ID₅₀) at a concentration of 7 nM while α₂-macroglobulin inhibited O₂⁻ production with an ID₅₀ of 141 nM. The ‘fast’ forms of α₂-macroglobulin may play a role in the feedback regulation of inflammatory reactions.     

Bioactive and osteoblast cell attachment studies of novel α- and β-chitin membranes for tissue-engineering applications

Chitin is a novel biopolymer and has excellent biological properties such as biodegradation in the human body and biocompatible, bioabsorable, antibacterial and wound healing activities. In this work, α- and β-chitin membranes were prepared using α- and β-chitin hydrogel. The bioactivity studies were carried out using these chitin membranes with the simulated body fluid solution (SBF) for 7, 14 and 21 days. After 7, 14 and 21 days the membranes were characterized using SEM, EDS and FT-IR. The SEM, EDS and FT-IR studies confirmed the formation of calcium phosphate layer on the surface of the both chitin membranes. These results indicate that the prepared chitin membranes were bioactive. Cell adhesion studies were also carried out using MG-63 osteoblast-like cells. The cells were adhered and spread over the membrane after 24 h of incubation. These results indicated that the chitin membranes could be used for tissue-engineering applications.     

Evidence of α fluctuations in myoglobin's denaturation in the high temperature region: Average relaxation time from an Adam–Gibbs perspective

In this work, we derive an analytical expression for the relaxation time τ as a function of temperature T for myoglobin protein (Mb, PDB:1MBN) in the high temperature limit (T > T_g = 200 K). The method is based on a modified version of the Adam–Gibbs theory (AG theory) for the glass transition in supercooled liquids and an implementation of differential geometry techniques. This modified version of the AG theory takes into account that the entropic component in protein's denaturation has two major sources: a configurational contribution ΔS_c due to the unfolding of the highly ordered native state N and a hydration contribution ΔS^hyd arising from the exposure of non-polar residues to direct contact with solvent polar molecules. Our results show that the configurational contribution ΔS_c is temperature-independent and one order of magnitude smaller than its hydration counterpart ΔS^hyd in the temperature range considered. The profile obtained for log τ(T) from T = 200 K to T = 300 K exhibits a non-Arrhenius behavior characteristic of α relaxation mechanisms in hydrated proteins and glassy systems. This result is in agreement with recent dielectric spectroscopy data obtained for hydrated myoglobin, where at least two fast relaxation processes in the high temperature limit have been observed. The connection between the relaxation process calculated here and the experimental results is outlined.     

α-phenyl-tert-butyl-nitrone inhibits free radical release in brain concussion

Traumatic brain injury (TBI) is one of the important causes of mortality and morbidity. The pathogenesis of the underlying brain dysfunction is poorly understood. Recent data have suggested that oxygen free radicals play a key role in the primary and secondary processes of acute TBI. We report direct electron spin resonance (ESR) evidence of hydroxyl (·OH) radical generation in closed-head injury of rats. Moderate brain concussion was produced by controlled and reproducible mechanical, fixed, closed-head injury. A cortical cup was placed over one cerebral hemisphere within 20 min of the concussion, perfused with artificial cerebrospinal fluid (aCSF) containing the spin trap agent pyridyl-N-oxide-tert-butyl nitrone (POBN, 100 mM), and superfusate samples collected at 10 min intervals for a duration up to 130 min post brain trauma. In addition, POBN was administered systematically (50 mg/kg body wt.) 10 min pretrauma and 20 min posttrauma to improve our ability to detect free radicals. ESR analysis of the superfusate samples revealed six line spectra (α_N = 15.4 and α^β_H = 2.5 G) characteristic of POBN-OH radical adducts, the intensity of which peaked 40 min posttrauma. The signal was undetectable after 120 min. Administration of α-phenyl-tert-butyl-nitrone (PBN), a spin adduct forming agent systemically (100 mg/kg body wt. IP 10 min prior to concussion) alone or along with topical PBN (100 mM PBN in aCSF),6significantly (P< 0.001) attenuated the ESR signal, suggesting its possible role in the treatment of TBI.     

Evidence for seasonal variation in δ13C and δ18O profiles of Baculites and implications for growth rate

The life histories of ammonites and the life strategies they employed are difficult to assess without robust modern analogues but placing constraints on ammonite growth rates provides a fundamental first step to understanding this abundant, but poorly understood, fossil group. Here we interpret periodic variations in carbon and oxygen stable isotope profiles from Campanian and Maastrichtian ammonites (Baculites) as seasonally driven and use these records to determine their rate of shell precipitation. Several of these samples are housed in museums and were originally prepared using sealants for display and preservation but testing of these sealants indicated no alteration of the isotopic values of treated carbonate. Diagenetic alteration, as determined by shell microstructure, affected the preservation of isotopic signals, resulting in the loss of seasonal variation in less well‐preserved specimens, and the δ¹³C signal is more robust than δ¹⁸O. The periodicity of isotopic profiles from Baculites shells presented here suggest that these organisms grew at rapid rates (c. 340 mm per year), which may imply an r‐type life strategy in which the animals reach maturity quickly, spawn large quantities of progeny, and die at a young age. Because of the potential mobility of Baculites, reconstructing palaeoenvironmental conditions from these isotopic records is challenging and should be conducted cautiously. Unfortunately, well‐preserved Baculites shells much longer than 350 mm are rarely recovered, which complicates the statistical treatment of potential periodicity in isotopic profiles.     

α3β1 integrin promotes cell survival via multiple interactions between 14-3-3 isoforms and proapoptotic proteins

Laminin-5 and α3β1 integrin promote keratinocyte survival; however, the downstream signaling pathways for laminin-5/α3β1 integrin-mediated cell survival had not been fully established. We report the unexpected finding of multiple interactions between 14-3-3 isoforms and proapoptotic proteins in the survival signaling pathway. Ln5-P4 motif within human laminin-5 α3 chain promotes cell survival and anti-apoptosis by inactivating Bad and YAP. This effect is achieved through the formation of 14-3-3ζ/p-Bad and 14-3-3σ/p-YAP complexes, which is initiated by α3β1 integrin and FAK/PI3K/Akt signaling. These complexes result in cytoplasmic sequestration of Bad and YAP and their subsequent inactivation. An increase in Akt1 activity in cells induces 14-3-3ζ and σ, p-Bad, and p-YAP, promoting cell survival, whereas decreasing Akt activity suppresses the same proteins and inhibits cell survival. Suppression of 14-3-3ζ with RNA-interference inhibits cell viability and promotes apoptosis. These results reveal a new mechanism of cell survival whereby the formation of 14-3-3ζ/p-Bad and 14-3-3σ/p-YAP complexes is initiated by laminin-5 stimulation via the α3β1 integrin and FAK/PI3K/Akt signaling pathways, thereby resulting in cell survival and anti-apoptosis.     

Simulation analysis of intracellular Na and Cl homeostasis during β1-adrenergic stimulation of cardiac myocyte

To quantitatively understand intracellular Na⁺ and Cl⁻ homeostasis as well as roles of Na⁺/K⁺ pump and cystic fibrosis transmembrane conductance regulator Cl⁻ channel (I_CFTR) during the β1-adrenergic stimulation in cardiac myocyte, we constructed a computer model of β1-adrenergic signaling and implemented it into an excitation-contraction coupling model of the guinea-pig ventricular cell, which can reproduce membrane excitation, intracellular ion changes (Na⁺, K⁺, Ca²⁺ and Cl⁻), contraction, cell volume, and oxidative phosphorylation. An application of isoproterenol to the model cell resulted in the shortening of action potential duration (APD) after a transient prolongation, the increases in both Ca²⁺ transient and cell shortening, and the decreases in both Cl⁻ concentration and cell volume. These results are consistent with experimental data. Increasing the density of I_CFTR shortened APD and augmented the peak amplitudes of the L-type Ca²⁺ current (I_CaL) and the Ca²⁺ transient during the β1-adrenergic stimulation. This indirect inotropic effect was elucidated by the increase in the driving force of I_CaL via a decrease in plateau potential. Our model reproduced the experimental data demonstrating the decrease in intracellular Na⁺ during the β-adrenergic stimulation at 0 or 0.5 Hz electrical stimulation. The decrease is attributable to the increase in Na⁺ affinity of Na⁺/K⁺ pump by protein kinase A. However it was predicted that Na⁺ increases at higher beating rate because of larger Na⁺ influx through forward Na⁺/Ca²⁺ exchange. It was demonstrated that dynamic changes in Na⁺ and Cl⁻ fluxes remarkably affect the inotropic action of isoproterenol in the ventricular myocytes.     

Environmental factors influencing the chaperone-like activity of α-crystallin

The effects of mild environmental changes (e.g. the addition of divalent cations or EDTA, as well as variations of buffer pH) on the heat stability and chaperone-like activity of native α-crystallin, and denatured–renatured α-crystallin in the native molar isoform ratio, have been investigated using circular dichroism (CD) spectropolarimetry and functional assays. The presence or absence of divalent cations has little or no effect on the secondary structure of renatured samples, although chaperone-like activity levels can vary widely; the only relevant spectral difference observed is a loss of some α-helical content in all the renatured samples relative to the native protein, but this change has no impact on function. The range of concentration over which the inhibitory Mg²⁺ effect is observed is 10-fold higher for dialyzed fresh protein than for protein renatured into buffers containing Mg²⁺, but for both sets of samples, the full effect is established below physiological Mg²⁺ concentrations. Renaturing into various pH buffers, in contrast, affects both heat stability and chaperone-like activity below pH 7.0, with essentially no functionality observed at pH 6.0. CD spectra of these samples indicate that acidic conditions lead to some degree of unfolding, and that this unfolding correlates directly with functionality. Similar results are obtained for fresh protein dialyzed against these pH levels. Overall, these results suggest that heat stability is a function of the protein's secondary structure and folding state, while chaperone-like activity is primarily a function of factors at the tertiary and quaternary levels of organization.     

Effects of 6-methoxy-2-benzoxazolinone on the germination and α-amylase activity in lettuce seeds

Germination of lettuce seeds was inhibited by 6-methoxy-2-benzoxazolinone (MBOA) at concentrations greater than 0.03 mmol/L. MBOA also inhibited the induction of α-amylase activity in the lettuce seeds at concentrations greater than 0.03 mmol/L. These two concentration–response curves for the germination and α-amylase indicate that the percentage of the germination was positively correlated with the activity of α-amylase in the seeds. Lettuce seeds germinated around 18 h after incubation and inhibition of α-amylase by MBOA occurred within 6 h after seed incubation. These results show that MBOA may inhibit the germination of lettuce seeds by inhibiting the induction of α-amylase activity.