A review of the use of isotopic and nuclear techniques in animal production

Isotopic and nuclear techniques play an important role in food and agriculture, health and industry. This paper discusses the use of these techniques and highlights potential for their use in the area of Animal Production. These techniques are discussed in two parts: (1) Isotopic methods and (2) non-isotopic nuclear methods. The isotopic techniques discussed are: stable- (¹⁵N) and radio-isotope (³⁵S or ³²P) incorporation methods for measuring microbial mass in vitro and in vivo; ¹²⁵I-labelled bovine serum albumin and ¹⁴C-labelled polyethylene glycol assays for measuring tannin in feeds; a method based on the feeding of isotope-labelled protein (¹⁵N or ¹²⁵I) complexed with tannin for ranking different tannins for their abilities to release protein for digestion in vivo; ¹⁴C-uric acid and ¹⁴C-allantoin infusion methods for development of models describing excretion of purine derivatives in urine and microbial protein supply to ruminants, which permit assessment of nutritional status of animals and determination of nutritional quality of feed resources; a ¹⁵N isotope dilution technique using ¹⁵N-leucine to distinguish feed and endogenous secretions at the ileum, for determination of true digestibility of protein-rich tree leaves and aquatic plants in pigs; progesterone radioimmunoassay (RIA) for enhancing reproductive efficiency of ruminants, and RIA based leptin and insulin like growth factor assays for assessing the nutritional status of animals; feeding of ¹⁵N enriched plant material to generate ¹⁵N-labelled excreta for research on the fate of excreta N in the environment; ¹⁵N, ¹³C and ³⁴S isotopic methods for nutrient budgeting and for following the nutrient pathways in the soil–plant–animal continuum; ³²P- or ³³P-labelled fertilizers for estimating the efficiency of P utilization in legume leaf production used for livestock feeding; double labelled water (¹⁸O and ²H labelled) method for estimating energy expenditures of grazing animals, body composition, basal metabolic rate, and milk output in cows with calves; NaH¹³CO₃/NaH¹⁴CO₃ infusion for estimation of the carbon dioxide production, which in turn is used to estimate energy expenditure in free-ranging animals; ³H- or ¹⁴C-labelled methane and ¹⁴C-labelled volatile fatty acids dilution technique for direct and indirect (using stoichiometry of carbohydrate fermentation) for determination of methane emission from livestock; ¹⁵N dilution technique requiring labeling the soil with ¹⁵N fertilizer (¹⁵N-ammonium sulphate or ¹⁵N-urea) for estimation of nitrogen fixation by leguminous trees and pastures.

The non-isotopic nuclear techniques that have been used or have the potential for use are: dual energy X-ray absorptionmetry and computer tomography for body composition determination; nuclear magnetic resonance techniques, fast atom bombardment mass spectroscopy, and mass ionisation spectroscopy for identification and structure determination of bioactive moieties of plant origin having potential for rumen manipulation or controlling internal parasites; gamma irradiation for inactivating antinutrients such as protease inhibitors, lectin, phytic acid, non-starch polysaccharides and oligosaccharides in feeds; induced mutations with gamma radiation, electron beam and fast neutrons for producing useful mutants of forage plants with improved yield, nutrient profiles and uptake.     

稻田与旱地土壤自养微生物同化碳在土壤中的矿化与转化特征

选择亚热带地区3种典型稻田和旱地土壤,应用碳同位素^14C-CO₂标记示踪技术结合室内模拟培养试验,研究自养微生物同化碳(“新碳”)在土壤碳库中的矿化和转化特征.结果表明: 在100 d的培养期内,“新碳”的矿化经历了先上升、10 d后缓慢下降、最后渐趋稳定的3个阶段.“新碳”的矿化比例为8.0%～26.9%,矿化速率为0.01～0.22 μg ¹⁴C·g^-1·d^-1,其中,稻田土壤为0.01～0.22 μg ¹⁴C·g^-1·d^-1,旱地土壤为0.01～0.08 μg ¹⁴C·g^-1·d^-1,而原有有机碳的矿化比例为1.6%～5.7%,矿化速率为1.3～25.66 μg C·g^-1·d^-1.土壤活性碳库\[可溶性有机碳(DOC)、微生物生物量碳(MBC)\]中,¹⁴C-DOC在培养初期(0～10 d)先上升,升高幅度达0.3 mg·kg^-1,10～30 d又迅速下降,下降幅度达0.42 mg·kg^-1,至30 d后缓慢下降.¹⁴C-MBC的波动与¹⁴C-DOC不同,在培养初期(0～10 d)先迅速下降,10～30 d又迅速上升,至40 d后缓慢下降并趋于稳定.水稻土¹⁴C-DOC/DOC的转化更新速率明显大于旱地,而旱地¹⁴C-MBC/MBC的转化更新速率大于水稻土.
     

The effect of exogenous gibberellic acid on gibberellin biosynthesis by Gibberella fujikuroi

The addition of gibberellic acid and some other gibberellins to cultures of Gibberella fujikuroi suppresses the incorporation of [2-¹⁴C]MVA and ¹⁴C-labelled ent-kaurene into the gibberellin metabolises.     

表层和下层免耕黑土有机碳矿化速率及激发效应

激发效应是调控土壤有机质分解的重要机制之一,而土层与激发效应的关系还不清晰.本研究通过室内培养试验,采用¹³C葡萄糖标记和动态碱液吸收的方法,探究免耕农田黑土表层土壤(0～10 cm)和下层土壤(30～40 cm)有机碳矿化速率及其激发效应.结果表明: 表层与下层土壤以单位有机碳表示的矿化速率并未发现显著差异.添加葡萄糖使表层土壤原有机质分解加快36.7%(正激发),但使下层土壤原有机质分解减慢12.4%(负激发).在整个培养期间(30 d),表层和下层土壤的累积激发碳量分别为3.14和-1.24 mg C·g^-1 SOC,但由于新碳(葡萄糖)的补偿作用,即使在产生显著正激发的表层土壤中,仍表现为有机碳净积累.说明外源碳输入使不同土层土壤有机质分解的幅度甚至方向产生明显差别.这为今后免耕和秸秆还田等保护性耕作措施的实践提供了重要的理论基础.     

Monitoring Anaerobic Natural Attenuation of Petroleum Using a Novel In Situ Respiration Method in Low-Permeability Sediment

Assessing petroleum biodegradation rates is an important part of predicting natural attenuation in subsurface sediments. Monitoring carbon dioxide (CO₂) and methane (CH₄) produced in situ, and their radiocarbon ¹⁴C), stable carbon (¹³C) and deuterium (D). signature provide a novel method to assess anaerobic microbial processes. Our objectives were to: (1) estimate the rate of anaerobic petroleum hydrocarbon (PH) mineralization by monitoring the production of soil gas CH₄ and CO₂ in the vadose zone of low-permeability sediment, (2) evaluate the dominant microbial processes using δ¹³C and δD, and (3) determine the proportion of CH₄ and CO₂ attributable to anaerobic mineralization of PH using ¹⁴C analysis. Argon was sparged into the subsurface to dilute existing CO₂ and CH₄ concentrations. Vadose zone CO₂, CH₄, oxygen, total combustible hydrocarbons, and argon concentrations were measured for 75 days. CO₂ and CH₄ samples were collected on day 86 and analyzed for ¹⁴C, δ¹³C, and δD. Based on CH₄ soil gas production, the anaerobic biodegradation rate was estimated between 0.017 to 0.055 mg/kg soil-d. CH₄ ¹⁴C (2.6 pMC), δ¹³C (-45.64‰), and δD (-316‰) values indicated that fermentation of PH was the sale source of CH₄ in the vadose zone. CO₂ ¹⁴C (62 pMC) indicated that approximately 47% of the total CO₂ was from PH mineralization and 53% from plant root respiration. Although low-permeability sediment increases the difficulty of completely replacing in situ soil gas and assuring anaerobic conditions, this novel respiration method distinguished between anaerobic processes responsible for PH degradation.     

Feeding of Achelia echinata Hodge (Pycnogonida) on marine algae

Field observations of Achelia echinata Hodge in Southampton Water suggested that it may be feeding on Griffithsia and Enteromorpha, although this pycnogonid was not known to be algivorous. This possibility was experimentally tested by maintaining the pycnogonid on ¹⁴C-labelled weeds, whence they were found to take up activity in proportion to the concentration of ¹⁴C in the weed. The experimental design precluded sea water, bacteria or any passive uptake as a source of the ¹⁴C in the pycnogonids, and comparisons between Enteromorpha and Griffithsia eliminated epiphytes as the source. It is concluded that Achelia echinata actively feeds on these two species of seaweed, possibly more readily on Enteromorpha. The feeding behaviour and its significance are discussed.     

Spatio-temporal variability in benthic mineralization processes in the eastern English Channel

The effect of phytodetritus derived from Phaeocystis sp. bloom on benthic mineralization processes has been determined at four intertidal stations along the French coast of the eastern English Channel. Sites were chosen to offer a diversity of sediment types, from permeable sandy beach to estuarine mudflats. Sediment Oxygen Demand (SOD) as well as total fluxes of Dissolved Inorganic Nitrogen (DIN) at the sediment–water interface were determined by using whole core incubation technique and diffusive fluxes were predicted from interstitial water concentrations. In the absence of phytodetritus deposits, a marked gradient of granulometric characteristics and organic matter contents were observed, and resulted in more intensive mineralization processes in muddy sediments. Highly significant correlations (P < 0.05) were evidenced between SOD and porosity, bacterial biomass, Organic Carbon and Organic Nitrogen, evidencing the direct link between sediment texture, organic matter accumulation and microbial activity. The spring bloom led to a massive input of organic matter in surficial sediments and mineralization rates significantly increased while higher DIN release towards the water column was observed. A modification of the mineralization pathways was evidenced but clearly depended on the sediment type. With a global view, benthic mineralization processes in the intertidal zone provided significant a part of DIN inputs in the coastal zone while water column was depleted in nutrients.     

草甸草原土壤与植物系统自然丰度氮稳定同位素的年际变化及其指示作用

氮是陆地生态系统生产力的首要限制性养分,利用自然丰度δ¹⁵N(¹⁵N/¹⁴N)可以有效指示生态系统氮循环过程。本试验研究了内蒙古草甸草原土壤与植物系统自然丰度δ¹⁵N、土壤净氮矿化潜势的年际变化。结果表明: 2017—2020年,土壤NO₃^--N含量(9.83～14.79 mg·kg^-1)均显著高于NH₄⁺-N含量(3.92～5.00 mg·kg^-1);土壤NH₄⁺的δ¹⁵N值(13.3‰～18.3‰)显著高于NO₃^-的δ¹⁵N值(3.76‰～6.14‰),土壤NO₃^-的δ¹⁵N值与土壤NO₃^-含量呈显著负相关;干旱年NH₄⁺的δ¹⁵N值相对较高,降水较高或较低年NO₃^-的δ¹⁵N值显著降低。干旱年土壤净氮矿化速率、净氨化速率显著高于湿润年,而土壤硝化速率与年降水量无显著相关性。植物δ¹⁵N值与土壤δ¹⁵N值无显著相关性,但与植物N含量呈显著负相关;豆科植物与非豆科植物δ¹⁵N值、N含量均呈显著正相关,在一定程度上表明豆科植物对非豆科植物的N吸收具有促进作用。研究结果可为草原土壤-植物系统氮循环过程及其对降水变化的响应提供数据支撑。     

水分对武夷山草甸土壤有机碳激发效应的影响

水分是影响土壤有机碳激发效应的重要因子,但水分如何影响山地草甸土有机碳激发效应尚不清楚.本试验以武夷山高海拔(2130 m)山地草甸土为研究对象,通过室内添加13C标记的葡萄糖结合控制土壤水分(30％FWC和60％ FWC,FWC为田间持水量),进行为期126 d的室内培养试验,定期测定CO2浓度和13C-CO2丰度值...     

Measurement of bacterial production in stream-bed sediments via leucine incorporation

Abstract: The leucine incorporation technique was evaluated and optimised for measuring bacterial production in stream-bed sediments. The original procedure was modified in order to obtain reliable production estimates in this habitat. This included the use of higher leucine concentrations (50 μmol l⁻¹) for obtaining substrate saturation, and an enhanced protein extraction procedure after sample fixation. The leucine method was combined with a perfused core technique. Water containing ¹⁴C-labelled leucine was perfused up through sediment cores, enabling the measurement of bacterial production in an experimental situation resembling natural conditions in the stream bed. Bacterial production in the Breitenbach, a small upland stream in Central Germany, showed a high degree of spatial variability in the sandy stream bed. It was related closely to sediment organic matter content, whereas varying perfusion rates had less influence. Annual bacterial production was estimated at about 200 g C m⁻², demonstrating the potential for bacteria to act as a food resource for benthic fauna in this stream.     

Liposomes as carriers of C-labelled penicillin and I-labelled albumin through the cell wall of Pseudomonas aeruginosa

The use of liposomes in overcoming the cell wall barrier of Pseudomonas aeruginosa to certain antibiotics has been studied. Negatively charged liposomes labelled with ¹²⁵I-labelled albumin or ¹⁴C-labelled penicillin were used. The distribution of the labelled compounds in the cellular subfractions of the bacteria show that more than half of both ¹²⁵I-labelled albumin and ¹⁴C-labelled penicillin passed the cell wall and were found either bound to the cytoplasmic membranes or in the 160 000 g supernatant.     

Structuring factors in a marine soft bottom community during eutrophication—an experiment with radio-labelled phytodetritus

The quantitative development and uptake of radio-labelled phytodetritus in benthic macro- and meiofauna was studied in a 5-month experiment in two mesocosms, one of which received a single large nutrient (N and P) addition, while the other served as control. In reponse to the 12-fold increase in phytoplankton biomass noted after 2 weeks and the resulting enhanced accumulation of fresh phytodetritus, the abundance and biomass of the polychaetes Mediomastus ambiseta and Polydora ligni and the mud anemone Cerianthiopsis americanus increased significantly in the enriched tank. The abundances of P. ligni and M. ambiseta increased 37-fold and 12-fold, respectively, within the first two months of the experiment. No other macrofaunal or meiofaunal taxa showed any consistent positive quantitative response to the increased input of phytodetritus. In the control tank no considerable change in the benthic community structure was noted. The measurements of radio-label uptake within the benthic fauna showed that the quantitatively most successful species utilized fresh phytodetritus highly. However, a high degree of utilization of fresh detritus was also shown by taxa that did not respond quantitatively within the 5 month of the experiment, and almost all taxa showed a preference for fresh detritus over older organic material. Within the benthic meiofauna, kinorhynchs and especially foraminiferans showed a remarkably low preference for fresh detritus. A budget calculation comparing the total amounts of labelled organic carbon bound in animal tissue and in the sediment indicated that at any time at least 75% of this carbon was available for assimilation by deposit feeders. These results suggest that factors other than the availability of food, such as competition for space by a few opportunistic macrofauna species, limited the response of other species within this benthic community to the increased input of phytodetritus.     

The effect of diamphenethide on protein synthesis by the liver fluke, Fasciola hepatica

The effect of the deacetylated (amine) metabolite of diamphenethide (DAMD, 10 μg ml⁻¹) on the uptake and incorporation by adult Fasciola hepatica of radioactively labelled precursors of DNA, RNA and protein synthesis ([³H]thymidine, [³H]uridine and [³H] leucine, respectively) was measured by liquid scintillation counting. Comparison was made between the effects of DAMD and those of specific inhibitors of DNA, RNA and protein synthesis, namely, 5-fluorouracil, cordycepin and cycloheximide, respectively. DAMD caused a significant decrease in the overall uptake and incorporation of [³H]uridine by F. hepatica, decreased the incorporation of [³H] leucine and also caused a significant decrease in the overall protein content of the flukes. The effect of DAMD was similar to that of cycloheximide (1 × 10⁻³M), a potent inhibitor of protein synthesis, which also caused a significant decrease in the incorporation of [³H] leucine by the fluke and a decrease in the overall protein content of the fluke. Cordycepin (100 μg ml⁻¹) caused a significant decrease in the protein content of the fluke, but had no effect on the uptake or incorporation of [³H]uridine. 5-Fluorouracil (1 × 10⁻⁴ ) did not affect the uptake or incorporation of [³H]thymidine, nor did it decrease the protein content of the fluke. The results indicate that DAMD inhibits protein synthesis by F. hepatica, possibly by inhibiting RNA synthesis. The results are also consistent with previous morphological investigations involving DAMD.     

红壤和风沙土添加不同化学结构有机碳对外源碳去向及累积贡献的影响

植物凋落物碳输入显著影响陆地生态系统土壤CO₂排放和有机碳(SOC)形成,然而,针对不同质地土壤添加不同化学结构外源碳去向依然不清楚。本研究将¹³C标记的葡萄糖、淀粉和纤维素添加至红壤和风沙土,比较2种质地土壤添加不同化学结构外源碳在土壤释放的CO₂、SOC、可溶性有机碳(DOC)和微生物生物量碳(MBC)库的净累积量、回收率及贡献比例上的差异。结果表明: 添加外源有机碳显著提高了CO₂、SOC、DOC和MBC的δ¹³C值,且随着外源有机碳化学结构复杂性的增加,CO₂的δ¹³C峰值依次延迟出现;外源有机碳种类、土壤类型和培养时间均显著改变外源碳去向及其在各碳库的贡献比例;在风沙土中,外源有机碳更多被矿化为CO₂,且CO₂库的外源碳净累积量和回收率大小依次为葡萄糖>淀粉>纤维素;红壤添加外源碳转变为SOC的累积量和回收率显著高于风沙土,且红壤SOC库的外源碳净累积量和回收率大小顺序也为葡萄糖>淀粉>纤维素。可见,外源有机碳化学结构和土壤质地共同调控外源碳去向及累积贡献。     

THE BIOSYNTHESIS OF CHOLESTEROL AND OTHER STEROLS BY BRAIN TISSUE

Abstract— The distribution of ¹⁴C into several subcellular fractions of adult rat brain was studied as a function of time, following intracerebral injection of [2-¹⁴C]mevalonic acid. As expected from previous studies, the microsomal fraction was indicated as the site of sterol biosynthesis. The myelin fraction showed a marked and early uptake of ^I4C-labelled, digitonin-precipitable material. This was assumed to be a non-enzymic uptake of sterol intermediates. The mitochondrial fraction exhibited a rapid uptake of ¹⁴C-labelled, nonsaponifiable material, but a very slow accumulation of ¹⁴C-labelled, digitonin-precipitable product. Examination of the nonsaponifiable ¹⁴C-fractions by TLC showed a rapid appearance of labelled 4-desmethyl sterols in the microsomal fraction. The myelin fraction selectively retained 4,4'-dimethyl sterol but seemed to release this with time, possibly to be further metabolized by the microsomes. Examination of [¹⁴C]digitonin-precipitable material by the dibromide method showed that although labelled 4-desmethyl sterol appeared quite early, cholesterol itself was formed slowly in all fractions.     

基于多组织稳定同位素比值的热带大西洋4种鲨鱼营养生态位分化

不同代谢速率组织间的碳、氮稳定同位素比值(δ¹³C和δ¹⁵N)可以反映生物不同时间尺度的摄食信息,对探讨物种间摄食、栖息地利用和营养生态位的变化具有重要的指示作用。本研究以在大西洋热带海域兼捕的大青鲨、长鳍鲭鲨、拟锥齿鲨和尖吻鲭鲨为对象,通过测定其肌肉、肝脏和血液的δ¹³C和δ¹⁵N值,探讨4种鲨鱼营养生态位分化。结果表明: 与长鳍鲭鲨相比,尖吻鲭鲨、拟锥齿鲨和大青鲨的δ¹⁵N值相似且相对较高;大青鲨与其他鲨鱼存在摄食隔离,表现出独特的营养生态位;尖吻鲭鲨营养生态位宽幅最大,摄食食物种类和(或)栖息环境类型更多样化,其与拟锥齿鲨的营养生态位重叠度最高,说明两种鲨鱼具有潜在的资源竞争关系。尖吻鲭鲨、拟锥齿鲨和大青鲨组织间的δ¹³C、δ¹⁵N差值与其叉长均无显著相关关系,说明3种鲨鱼近期内无明显摄食变化;而长鳍鲭鲨的肝脏、血液和肌肉组织的δ¹⁵N差值与叉长显著相关,说明长鳍鲭鲨在短期内存在摄食变化。肝脏和血液的δ¹³C、δ¹⁵N值的相似性反映了两种组织整合摄食时间周期相近,其较高的代谢速率可以反映相对短时间周期的摄食信息。     

山东东营和烟台潮间带海草床食物网结构特征

为了探明海草床内主要生物类群间的营养关系以及食物网结构, 作者于2018年8月分别在东营黄河口潮间带和烟台西海岸潮间带海草床采集大型底栖生物样品, 采用δ ¹³C和δ ¹⁵N稳定同位素方法, 对生物样品的碳、氮同位素组成进行了测定和分析。结果表明: 东营海草床内生物的δ ¹³C、δ ¹⁵N值范围分别为-21.99‰至-12.13‰和5.23‰-11.05‰, 烟台海草床内生物的δ ¹³C、δ ¹⁵N值范围分别为-18.11‰至-14.06‰和6.60‰-10.22‰。东营海草床主要生物的营养级范围为2.00-3.85, 烟台海草床主要生物的营养级范围为2.00-3.15。根据δ ¹⁵N值计算所得的营养级图分析可知两区域海草床内初级消费者主要为滤食性双壳类和多毛类, 次级消费者为植食性或杂食性甲壳类,肉食性鱼类和腹足类。与近海海域大型底栖生物食物网相比, 海草床内底栖生物的营养级均值普遍较低。     

Transport of silver in virgin and lactating rats and relation to copper

Virgin and lactating Sprague Dawley rats were used to determine whether the pathways of silver transport to tissues and milk resemble those for copper. Rats were injected i.p. with small amounts of ¹¹⁰AgNO₃. Blood and tissues were examined at various times thereafter for total radioactivity and for incorporation into copper binding proteins in plasma and milk. As with ⁶⁷Cu, much of the ¹¹⁰Ag was rapidly incorporated into the liver. Skeletal muscle, spleen, mammary gland, ovaries, uterus and adrenals also were significant initial accumulation sites, with or without lactation. Lactation enhanced uptake by the mammary gland, and radioactivity rapidly entered the milk and milk ceruloplasmin. In the plasma, most of the ¹¹⁰Ag bound to a single component of apparent molecular weight 800 k throughout the 52 h period examined. A small proportion was also incorporated into plasma ceruloplasmin, as determined by immunoprecipitation and native gel electrophoresis. There was little or no association of ¹¹⁰Ag with albumin or transcuprein. The binding of ¹¹⁰Ag to the 800 kDa protein was tight. Off rates during pH 7 dialysis were <2.5%/day even in the presence of 100 M histidine or Cu(II), but were accelarated by mercaptoethanol. Subunits of 145 and 45 kDa in virtually pure peak fractions were those of ₁-macroglobulin. We conclude that silver resembles copper in aspects of its tissue distribution, response to lactation, and incorporation into ceruloplasmin. However its main plasma carrier appears to be ₁-macroglobulin, a different macroglobulin than that involved in copper transport.     

Enhanced benthic activity in sandy sublittoral sediments: Evidence from 13C tracer experiments

In situ and on-board pulse-chase experiments were carried out on a sublittoral fine sand in the German Bight (southern North Sea) to investigate the hypothesis that sandy sediments are highly active and have fast turnover rates. To test this hypothesis, we conducted a series of experiments where we investigated the pathway of settling particulate organic carbon through the benthic food web. The diatom Ditylum brightwellii was labelled with the stable carbon isotope ¹³C and injected into incubation chambers. On-board incubations lasted 12, 30 and 132 h, while the in situ experiment was incubated for 32 h. The study revealed a stepwise short-term processing of a phytoplankton bloom settling on a sandy sediment. After the 12 h incubation, the largest fraction of recovered carbon was in the bacteria (62%), but after longer incubation times (30 and 32 h in situ) the macrofauna gained more importance (15 and 48%, respectively), until after 132 h the greatest fraction was mineralized to CO₂ (44%). Our findings show the rapid impact of the benthic sand community on a settling phytoplankton bloom and the great importance of bacteria in the first steps of algal carbon processing.     

Measurements of Seasonal Rates and Annual Budgets of Organic Carbon Fluxes in an Antarctic Coastal Environment at Signy Island, South Orkney Islands, Suggest a Broad Balance between Production and Decomposition

We report here the first comprehensive seasonal study of benthic microbial activity in an Antarctic coastal environment. Measurements were made from December 1990 to February 1992 of oxygen uptake and sulfate reduction by inshore coastal sediments at Signy Island, South Orkney Islands, Antarctica. From these measurements the rate of benthic mineralization of organic matter was calculated. In addition, both the deposition rate of organic matter to the bottom sediment and the organic carbon content of the bottom sediment were measured during the same period. Organic matter input to the sediment was small under winter ice cover, and the benthic respiratory activity and the organic content of the surface sediment declined during this period as available organic matter was depleted. On an annual basis, about 32% of benthic organic matter mineralization was anoxic, but the proportion of anoxic compared with oxic mineralization increased during the winter as organic matter was increasingly buried by the amphipod infauna. Fresh organic input occurred as the sea ice melted and ice algae biomass sedimented onto the bottom, and input was sustained during the spring after ice breakup by continued primary production in the water column. The benthic respiratory rate and benthic organic matter content correspondingly increased towards the end of winter with the input of this fresh organic matter. The rates of oxygen uptake during the southern summer (80 to 90 mmol of O₂ m^-2 day^-1) were as high as those reported for other sediments at much higher environmental temperatures, and the annual mineralization of organic matter was equally high (12 mol of C m^-2 year^-1). Seasonal variations of benthic activity in this antarctic coastal sediment were regulated by the input and availability of organic matter and not by seasonal water temperature, which was relatively constant at between -1.8 and 0.5°C. We conclude that despite the low environmental temperature, organic matter degradation broadly balanced organic matter production, although there may be significant interrannual variations in the sources of the organic matter inputs.