Further studies of a spring phytoplankton bloom in an enclosed experimental ecosystem

A detailed characterization is presented of the spring diatom bloom which occurred in the enclosed experimental ecosystem bags at Loch Ewe, Scotland, during March–April 1983. The nutrient condition and bacterial biomass of the water column, phytoplankton species distribution, gross biochemical composition and detailed lipid composition (lipid class, fatty acid and free sterol) of the phytoplankton are reported throughout the bloom period. The results are compared with results from previous years. The conclusions are that major changes take place in the biochemical composition of a rapidly growing diatom population which affect both the gross composition and also the more detailed lipid composition. Such changes can take place over a matter of days and appear to be very dependent upon available growth conditions. Both carbohydrate and lipids levels increase towards the end of the bloom as nitrate and silicate levels are depleted in the water. Neutral lipids are shown to be important lipid components of the phytoplankton populations and long-chain ω3 polyunsaturated fatty acids are found to be only minor components of the structural polar lipids. The fatty acid and sterol data are discussed in relation to present knowledge concerning phytoplankton lipid composition.     

Studies of a spring phytoplankton bloom in an enclosed experimental ecosystem. II. Changes in the component fatty acids and sterols

The spring diatom bloom in Loch Ewe (N.W. Scotland) during 1980 has already been the subject of a detailed study. As an extension of this work the component fatty acids and sterols of the diatom lipids have been analysed throughout the bloom period. The results confirm that detailed changes occur in the lipid composition of diatoms during their normal growth. In addition, the data are discussed in relation to published analyses of diatom lipids and suggestions made as to reasons for the considerable variation in reported fatty acid composition.     

Short-term changes in polysaccharide utilization mechanisms of marine bacterioplankton during a spring phytoplankton bloom

Spring phytoplankton blooms in temperate environments contribute disproportionately to global marine productivity. Bloom-derived organic matter, much of it occurring as polysaccharides, fuels biogeochemical cycles driven by interacting autotrophic and heterotrophic communities. We tracked changes in the mode of polysaccharide utilization by heterotrophic bacteria during the course of a diatom-dominated bloom in the German Bight, North Sea. Polysaccharides can be taken up in a ‘selfish’ mode, where initial hydrolysis is coupled to transport into the periplasm, such that little to no low-molecular weight (LMW) products are externally released to the environment. Alternatively, polysaccharides hydrolyzed by cell-surface attached or free extracellular enzymes (external hydrolysis) yield LMW products available to the wider bacterioplankton community. In the early bloom phase, selfish activity was accompanied by low extracellular hydrolysis rates of a few polysaccharides. As the bloom progressed, selfish uptake increased markedly, and external hydrolysis rates increased, but only for a limited range of substrates. The late bloom phase was characterized by high external hydrolysis rates of a broad range of polysaccharides and reduced selfish uptake of polysaccharides, except for laminarin. Substrate utilization mode is related both to substrate structural complexity and to the bloom-stage dependent composition of the heterotrophic bacterial community.     

Ecological studies on the phytoplankton of Korsfjorden, western Norway. The dynamics of a spring bloom seen in relation to hydrographical conditions and light regime

The investigation was carried out at one station in Korsfjorden,a typical deep silled fjord of western Norway. During 14 cruisesfrom 4 February to 30 June 1977 ATP, chlorophll a, phaeopigmenta, and in situ ¹⁴C-assimilation were measured in the net (>30µm), nano and ultraplankton (<5 µm). Sampleswere collected from five light depths within euphotic zone.The impact of hydrographical conditions and light regime onthe bloom dynamics was also studied. In the periods 4 February-7 March and 13 April-30 June, ultraplankton contributed >60%to the total primary production while net and nanoplankton dominatedfrom 7 March to 13 April. The diatoms Skeletonema costatum,Chaetoceros compressits and C. debilis, and Rhizosolenia hebetatavar. semispina made up the main part of the biomass on 21 March,28 March and 4 April respectively. A shade adapted diatom societywas located at the top of the nutricline in late June with S.costatum, Chaetoceros spp., and Thalassiosira spp. as the dominantspecies. The highest assimilation number of eight for the netplankton and four for the ultraplankton were found at the depthof 32% light intensity on 28 March and 24 May respectively.Linear relationships were found between chlorophyll a and ATPfor the different size fractions with regression slopes rangingfrom 4.3 to 5.8. The total primary production for the periodof investigation was calculated to 74 g C m^–2. Light regimeand water column stability were decisive factors for the outburstof the first diatom bloom in late March. Grazing on net planktondiatoms increased during late March-early April. Changes inthe longshore wind-stress component were found to be essentialfor the understanding of the bloom dynamics.     

Cultivation of particle-associated heterotrophic bacteria during a spring phytoplankton bloom in the North Sea

Seawater contains free-living and particle-attached bacteria. Only a small fraction is cultivable on plates. As free-living and particle-associated bacteria differ in their physiological traits, their cultivability on plates may coincide with particle association. Using filtration and Imhoff sedimentation cones, particles were collected during a spring phytoplankton bloom off Helgoland (North Sea) in order to obtain particle-associated bacteria as inocula. Direct dilution plating resulted in 526 strains from 3 µm filtration retentates and 597 strains from settled particles. Motile Gammaproteobacteria from the genera Pseudoalteromonas, Shewanella, Psychrobacter, Vibrio and Colwellia, as well as particle-attached Flavobacteriia affiliating with the genera Tenacibaculum and Gramella, were frequently isolated. As a result, a diverse collection comprised of 266 strains was deposited. Two strains were most likely to represent novel genera and 78 strains were probably novel species. Recently, a high-throughput cultivation study from the same site using seawater as an inoculum had retrieved 271 operational phylogenetic units (OPUs) that represented 88% of the 4136 characterized strains at the species level. A comparison of 16S rRNA gene sequences revealed that the collection obtained matched 104 of the 271 seawater OPUs at the species level and an additional 113 at the genus level. This large overlap indicated a significant contribution of particle-associated bacteria to the cultivable microbiome from seawater. The presence of 49 genera not identified in the larger seawater study suggested that sample fractionation was an efficient strategy to cultivate rare members of the planktonic microbiome. The diverse collection of heterotrophic bacteria retrieved in this study will be a rich source for future studies on the biology of particle-associated bacteria.     

High-throughput cultivation of heterotrophic bacteria during a spring phytoplankton bloom in the North Sea

On-going studies of phytoplankton-bacterioplankton interactions at the long-term ecological research site Helgoland Roads have indicated that many of the heterotrophic bacterial taxa have not yet been cultivated. A high-throughput approach combining whole cell matrix-assisted laser desorption ionization – time of flight mass spectroscopy with 16S rRNA gene sequencing was applied to the spring bloom of 2016. Aiming at an assessment of cultivability during a spring bloom, cultivation on solid marine media had to be used since dilution to extinction would not have been feasible for a high-throughput approach, as performed in this study. A total of 5023 isolates were obtained from nine weekly samples on eight different solid media between the early-bloom and post-bloom periods. Most of the 4136 strains identified affiliated with Bacteroidetes (13.3%), Gammaproteobacteria (26.9%), Alphaproteobacteria (40.6%) and Actinobacteria (6.7%). Of the 271 operational phylogenetic units (OPUs) identified, 13 are likely to represent novel genera and 143 novel species. A comparison with 16S rRNA gene tag data indicated that most of the isolates were rather rare in surface waters, with the exception of five OPUs affiliating with Rhodobacteraceae, Polaribacter, Psychromonas and Pseudoalteromonas. The effort yielded many novel isolates, yet most of the abundant heterotrophic bacteria still remained elusive. The large strain collection obtained will not only provide insights into the succession of the cultivable fraction of the bacterioplankton, but also enable fine-tuned taxonomic and physiological follow-up studies for improving our knowledge on heterotrophic bacteria in North Sea waters.     

Candidatus Prosiliicoccus vernus,a spring phytoplankton bloom associated member of the Flavobacteriaceae

Microbial degradation of algal biomass following spring phytoplankton blooms has been characterised as a concerted effort among multiple clades of heterotrophic bacteria. Despite their significance to overall carbon turnover, many of these clades have resisted cultivation. One clade known from 16S rRNA gene sequencing surveys at Helgoland in the North Sea, was formerly identified as belonging to the genus Ulvibacter. This clade rapidly responds to algal blooms, transiently making up as much as 20% of the free-living bacterioplankton. Sequence similarity below 95% between the 16S rRNA genes of described Ulvibacter species and those from Helgoland suggest this is a novel genus. Analysis of 40 metagenome assembled genomes (MAGs) derived from samples collected during spring blooms at Helgoland support this conclusion. These MAGs represent three species, only one of which appears to bloom in response to phytoplankton. MAGs with estimated completeness greater than 90% could only be recovered for this abundant species. Additional, less complete, MAGs belonging to all three species were recovered from a mini-metagenome of cells sorted via flow cytometry using the genus specific ULV995 fluorescent rRNA probe. Metabolic reconstruction indicates this highly abundant species most likely degrades proteins and the polysaccharide laminarin. Fluorescence in situ hybridisation showed coccoid cells, with a mean diameter of 0.78 mm, with standard deviation of 0.12 μm. Based on the phylogenetic and genomic characteristics of this clade, we propose the novel candidate genus Candidatus Prosiliicoccus, and for the most abundant and well characterised of the three species the name Candidatus Prosiliicoccus vernus.     

Comparison of phosphorus deficiency indices during a spring phytoplankton bloom in a eutrophic reservoir

1. Phosphorus limitation was studied along the eutrophic, canyon-type ?ímov reservoir (Czech Republic) during a spring phytoplankton bloom. Concentration of soluble reactive phosphorus (SRP), C:P molar ratio in seston, extracellular alkaline phosphatase activity (APA), and P limitation (bioassay) were used as indices for phosphorus deficiency in the phytoplankton. 2. SRP, C:P, APA, and P limitation indicated a moderate P deficiency in the downstream, but not upper, part of the reservoir. 3. Significant correlations between these parameters were found in the downstream part. Chlorophyll a concentration correlated with APA and P limitation in the upper part. 4. APA was significantly enhanced in the phosphorus-deficient phytoplankton. However, APA was apparently not related to total biomass or species composition of the phytoplankton. 5. Generally, APA was closely correlated with pH in the reservoir. However, extracellular alkaline phosphatases, with a pH optimum above 9.0, were induced and active only during the phytoplankton bloom, whereas low background activity of extracellular phosphatases was found at low chlorophyll a concentrations (winter, clear-water phase).     

Short-term changes in phosphorus storage in an oligotrophic Everglades wetland ecosystem receiving experimental nutrient enrichment

Natural, unenriched Evergladeswetlands are known to be limited by phosphorus(P) and responsive to P enrichment. However,whole-ecosystem evaluations of experimental Padditions are rare in Everglades or otherwetlands. We tested the response of theEverglades wetland ecosystem to continuous,low-level additions of P (0, 5, 15, and30 g L^–1 above ambient) in replicate,100 m flow-through flumes located in unenrichedEverglades National Park. After the first sixmonths of dosing, the concentration andstanding stock of phosphorus increased in thesurface water, periphyton, and flocculentdetrital layer, but not in the soil or macrophytes. Of the ecosystem components measured, total P concentration increased the most in the floating periphyton mat (30 g L^–1: mean = 1916 g P g^–1, control: mean =149 g P g^–1), while the flocculentdetrital layer stored most of the accumulated P(30 g L^–1: mean = 1.732 g P m^–2,control: mean = 0.769 g P m^–2). Significant short-term responsesof P concentration and standing stock wereobserved primarily in the high dose (30 gL^–1 above ambient) treatment. Inaddition, the biomass and estimated P standingstock of aquatic consumers increased in the 30and 5 g L^–1 treatments. Alterationsin P concentration and standing stock occurredonly at the upstream ends of the flumes nearestto the point source of added nutrient. Thetotal amount of P stored by the ecosystemwithin the flume increased with P dosing,although the ecosystem in the flumes retainedonly a small proportion of the P added over thefirst six months. These results indicate thatoligotrophic Everglades wetlands respondrapidly to short-term, low-level P enrichment,and the initial response is most noticeable inthe periphyton and flocculent detrital layer.     

Impact of whitefish on an enclosure ecosystem in a shallow eutrophic lake: changes in nutrient concentrations,phytoplankton and zoobenthos

Large bag-type (75 m³) and tube-type (105 m³) enclosures were set up in the shallow eutrophic Lake Suwa and were each stocked with exotic planktivorous whitefish (Coregonus lavaretus maraena). The release of whitefish caused the increase in nutrient concentration in the tube-type enclosure whereas no such increase was observed in the bag-type enclosure. Bottom sediment seemed to be an important source of chironomid food for whitefish. The proportion of phytoplankton measuring<10μm and 20–40μm, which respectively corresponded toOchromonas spp. andCryptomonas sp., were lower in the fish enclosures than in the control, which might have been caused by high grazing pressure by rotifers. The predation by whitefish might have affected the species composition of phytoplankton through reducing copepod predation on rotifers, not through reducing the densities of cladocerans which directly feed on phytoplankton as many investigators have reported. The phytoplankton biomass was not affected much by the release of fish. Possible reasons are that the increase in density of rotifers reduced the biomass of available phytoplankton and also that inedible Cyanophyceae were in the decreasing phase of their seasonal succession and could not increase successfully in spite of elevated nutrient levels.     

Earlier onset of the spring phytoplankton bloom in lakes of the temperate zone in a warmer climate

The decoupling of trophic interactions is potentially one of the most severe consequences of climate warming. In lakes and oceans the timing of phytoplankton blooms affects competition within the plankton community as well as food–web interactions with zooplankton and fish. Using Upper Lake Constance as an example, we present a model‐based analysis that predicts that in a future warmer climate, the onset of the spring phytoplankton bloom will occur earlier in the year than it does at present. This is a result of the earlier occurrence of the transition from strong to weak vertical mixing in spring, and of the associated earlier onset of stratification. According to our simulations a shift in the timing of phytoplankton growth resulting from a consistently warmer climate will exceed that resulting from a single unusually warm year. The numerical simulations are complemented by a statistical analysis of long‐term data from Upper Lake Constance which demonstrates that oligotrophication has a negligible effect on the timing of phytoplankton growth in spring and that an early onset of the spring phytoplankton bloom is associated with high air temperatures and low wind speeds.     

Long-term changes in the phytoplankton of large lakes in response to changes in nutrient loading

In Sweden the recovery process of the four largest lakes (<500 km²) has been followed since the mid-1970's when the phosphorus loading was reduced by approximately 50%. A ten-year investigation period before that acts as a basis of comparison. The response of the dominating species in the phytoplankton communities in the eutrophic Lake Mälaren and the oligotrophic Lake Vättern is discussed also in relation to a pristine state of the lakes. The long-term investigations with monthly sampling make a natural phytoplankton biomass variation range possible to establish - a range that is mainly due to effects of weather fluctuations. In order to get a tool for water management where disturbing and highly disturbing total phytoplankton volumes can be anticipated from a certain phosphorus concentration, a model is suggested based on experiences from more than 50 Swedish lakes investigated during a series of years.     

Production of viruses during a spring phytoplankton bloom in the South Pacific Ocean near of New Zealand

Lagrangian studies of virus activity in pelagic environments over extended temporal scales are rare. To address this, viruses and bacteria were examined during the course of a natural phytoplankton bloom in the pelagic South Pacific Ocean east of New Zealand. Daily samples were collected in a mesoscale eddy from year days 263-278 (September 19th-October 4th, 2008). The productive bloom transitioned from a diatom to a pico- and nanoplankton-dominated system, resulting in chlorophyll a concentrations up to 2.43?μg?L(-1) . Virus abundances fluctuated c.?10-fold (1.8?×?10(10) -1.3?×?10(11) L(-1) ) over 16?days. The production rates of virus particles were high compared with those reported in other marine systems, ranging from 1.4?×?10(10) to 2.1?×?10(11) L(-1) day(-1) . Our observations suggest viruses contributed significantly to the mortality of bacteria throughout the bloom, with 19-216% of the bacterial standing stock being lysed daily. This mortality released nutrient elements (N, Fe) that likely helped sustain the bloom through the sampling period. Parametric analyses found significant correlations with both biotic (e.g. potential host abundances) and abiotic parameters (e.g. nutrient concentrations, temperature). These observations demonstrate that viruses may be critical in the extended maintenance of regeneration-driven biological production.     

The sensitivity of phytoplankton in Loch Leven (U.K.) to changes in nutrient load and water temperature

1. Loch Leven is a shallow, eutrophic lake in Scotland, U.K. It has experienced much change over the 30 years that it has been studied; this has primarily been due to reduced nutrient loads to the lake through active catchment management. Its recovery has been slow and, therefore, we used a phytoplankton community model (PROTECH) to test its sensitivity to changing nutrient loads and water temperature.
2. PROTECH was initialized to simulate the observed phytoplankton community in 1995 and was then repeatedly run through a combination of step-wise changes in water temperature and nutrient load (two treatments were simulated for nutrient load: one changing both nitrate and phosphorus, and one changing just phosphorus). The effect on total chlorophyll- a concentration, cyanobacteria abundance and phytoplankton diversity was examined.
3. Whilst changes in temperature had little effect, variations in the nutrient load produced a range of responses. Increasing only the phosphorus load caused a large increase in Anabaena abundance and total chlorophyll- a concentration. However, the opposite response was recorded when nitrate load was changed as well, with Anabaena increasing its biomass under reduced nutrient load scenarios.
4. The key factor determining the type of response appeared to be nitrogen availability. Anabaena , a nitrogen fixer, could exploit the phosphorus resource of Loch Leven under limiting nitrogen conditions, allowing it to dominate under most of the scenarios tested apart from those supplying extra nitrogen to the lake. The model predictions agree with the observed data, which show that Anabaena continues to dominate the summer phytoplankton bloom in Loch Leven despite the considerable reduction in phosphorus supply from the catchment. This research provides a possible explanation for this.     

Change in the concentrations of iron in different size fractions during a phytoplankton bloom in controlled ecosystem enclosures

To observe micronutrient dynamics in the plankton ecosystem, controlled ecosystem enclosure (CEE) experiments were conducted in Saanich Inlet, B.C., Canada. Two CEEs (2.5 m in diameter, 16 m in length, one for Fe studies and the other for biological studies) were launched for the period 22 July to 5 August 1996 and enriched with 10 μM nitrate and 5.2 nM Fe (13% of total Fe) on day 1. Sampling from three integrated depths, intervals 0-4, 4-8 and 8-12 m, was performed on days 0, 1, 2, 3, 4, 5, 7, 9 and 11. Iron concentrations were measured for five size fractions: >25 μm particles, 2-25 μm particles, 0.2-2 μm particles, 0.2 μm-200 kDa small colloidal particles and <200 kDa soluble species. The sediment in the Fe enclosure was also collected on every sampling day after day 2 and its Fe was determined. Size-fractionated particulate organic carbon and total chlorophyll-a were also analyzed.The Fe in small colloidal particles (200 kDa-0.2 μm) comprised 78% of the traditionally defined dissolved phase (<0.2 μm) on day 1. Of all the size fractions of Fe, the small colloidal particulate fraction decreased most significantly during the phytoplankton bloom. In the dissolved fraction (<0.2 μm), the small colloidal particle fraction comprised 79% of the decrease. The decrease in concentration of Fe in small colloidal particles was larger than that of total Fe from day 1 to day 4. In contrast, the >25 μm Fe particles increased over the same period. These results suggest that Fe in small colloidal particles changed to >25 μm Fe particles during phytoplankton growth. A large amount of Fe was kept in the surface layer with the phytoplankton, and transported to the deep layer by phytoplankton sedimentation, at the end of the bloom. From these results, the small colloidal particulate Fe seems to be the most dynamic size fraction and a high percentage of Fe in small colloidal particles changed to large particles due to chemical/physical aggregation and/or physical adsorption to suspended particles such as phytoplankton cells.     

Preliminary investigation of the contribution of fast-ice algae to the spring phytoplankton bloom in Ellis Fjord,eastern Antarctica

 Algae released from fast-ice in Ellis Fjord, eastern Antarctica, made little contribution to subsequent phytoplankton growth. Dominant taxa in the interior ice community included Nitzschia cylindrus (Grun) Hasle, Navicula glaciei V.H. and a dinoflagellate cyst. Diatom mortality within the ice was high. The algal contribution to the phytoplankton from the fast ice was estimated by calculating the difference between algal biomass in ice cores taken on 14 November with those taken on 18 December 1992. The biomass of sedimenting phytoplankton was estimated using sediment traps; weekly cell counts of water were used to monitor net phytoplankton growth. The low contribution from the fast-ice of Ellis Fjord to the phytoplankton is similar to results from other Antarctic fast-ice communities but is not necessarily reflective of processes occurring within either Antarctic or Arctic pack ice communities. An algal mat growing on the base of the fast-ice had a carbon standing crop of between 0.231 gC m^-2 and 0.022 gC m^-2. Much of this was delivered to the water column as the ice melted while the remainder was exported. Received: 15 March 1995/Accepted: 4 September 1995     

Description of phytoplankton and nutrient in spring in the western North Atlantic Ocean

Abundance of diatoms in the northern Sargasso Sea in springhas been observed in a 4-year period between 1981 and 1985 andthen again in 1987. A theory is presented that if stratificationblocks get-through of deep nutrients to the surface, as in thesouthern Sargasso, then in-situ cycling via non-diatoms andammonia dominates. The theory is that if in-situ cycling doesnot dominate, as northward, then stratification does not blockget-through of deep nutrients to the surface, which, in combinationwith the marked growth capacity of diatoms, produce an abundanceof cells. This abundance consumes nitrate, phosphate and silicateat the surface and ultimately this nutrient-depleted water arrivesin the southern Sargasso via the gyre circulation. Thus thenutrient-depleted water of the western Atlantic gyre is consideredto be primarily achieved only by diatoms, in spring and in thenorthern Sargasso. A transect during April 13–16, 1985,north from the Virgin Islands along 63°–64°W showsa great change in the diatom species plus Emiliania huxleyifrom negligible concentrations in the southern half of the sectionto large concentrations in the northern half. This unevennessof distribution can be rephrased by indicating that these speciesare narrow-niched with regard to nutrient availability. Theother species, coccolithophores and dinoflagellates, are evenlydistributed at low concentrations south-north (though some diminishslightly) and so they are broad-niched with respect to nutrient.High species diversity depends on broadness of nutrient nicheand equilibrium conditions of hydrographically stable water(i), implying that when non-equilibrium conditions occur (ii),when niche breadth is less (iii) or both (iv), then diversityis less marked, (i) is confirmed by broad-niched species southward,(ii) is confirmed by broad-niched species northward, (iii) isconfirmed by narrow-niched species southward and (iv) by narrow-nichedspecies northward.     

The influence of integral solar radiation on the spring bloom of phytoplankton in the Ucha Reservoir

The results of the study of the quantitative relationships between solar radiation (integral radiation and PAR), the content of nutrients, and the spring bloom parameters in the Ucha Reservoir are presented. Positive significant correlations between the date of peak bloom and the sum of light intensity over the period from the 35the to the 40th days (the upper reaches of the reservoir, station Pestovo) and the period from the 44th to the 49th days (the lower reaches of the reservoir, station Listvyanka) were determined on the basis of a retrospective analysis of the data from the period of 1993–2003. Regression equations were derived, which permit forecasting the start of phytoplankton growth in spring according to the results of solar radiation measurements. The sum of light intensity over the course of 50 calendar days in each years correlate positively with the phytoplankton abundance in spring (the highest daily number of algae and integral estimation of algae number in spring).     

Dynamics in bacterial surface properties of a natural bacterial community in the coastal North Sea during a spring phytoplankton bloom

The hydrophilic and hydrophobic properties of single cells of natural bacterioplankton communities were determined using a recently developed staining method combined with confocal laser scanning microscopy and advanced image analysis. On an average, about 50% of the bacterial cell area was covered by hydrophobic and only 16% by hydrophilic properties, while about 72% was covered by the genome. However, the size of these properties was independent of the bacterial cell size. Bacterial hydrophobicity was positively correlated with ambient NH(4)(+) concentrations and negatively correlated with overall bacterial abundance. The expression of hydrophilicity was more dynamic. Over the spring phytoplankton bloom, the bacterioplankton ratio(phil/phob) repeatedly reached highest values shortly before peaks in bacterioplankton abundance were observed, indicating a direct and fast response of bacterial surface properties, especially hydrophilicity, to changing environmental conditions. Compared to bacterial strains, recently studied with the same method, cells of marine bacterioplankton communities are much smaller and less frequently covered by hydrophobic or hydrophilic properties. While the percentage area covered by the genome is essentially the same, the percentage area covered by hydrophobic or hydrophilic properties is much smaller.     

Quantifying spatiotemporal changes in a sagebrush ecosystem in relation to energy development

Energy development has been occurring in the intermountain western United States for over a century, yet few studies have attempted to spatially quantify the impacts of this disturbance on native ecosystems. We used temporal remotely sensed data for the Pinedale Anticline Project Area (PAPA) in western Wyoming, a region that has experienced increased natural gas development within the past 10 yr, to quantify the spatiotemporal distribution of Wyoming big sagebrush Artemisia tridentata, natural gas development, and other landcover types. Our analyses included 5 Landsat Thematic Mapper (TM) images of the PAPA over a 22‐yr period (1985–2006). We determined whether Wyoming big sagebrush spatiotemporal patterns were associated with natural gas development or other landcover types. We also developed a footprint model to determine the direct and indirect impacts of natural gas development on the distribution of Wyoming big sagebrush habitats. Over the 22‐yr period, we observed an inverse relationship between the amount of Wyoming big sagebrush habitat and natural gas development. During this time, Wyoming big sagebrush habitat declined linearly at a rate of 0.2% yr^?1 (4.5% total net loss), whereas natural gas development increased exponentially at a rate of 20% yr^?1 (4800% total net increase). Our evaluation indicated that, by 2006, natural gas development directly impacted 2.7% (1750 ha) of original Wyoming big sagebrush habitat. Indirect impacts, quantified to account for degraded habitat quality, affected as much as 58.5% (assuming 1000‐m buffers) of the original Wyoming big sagebrush habitat. Integrating assessments of the direct and indirect impacts will yield a better elucidation of the overall effects of disturbances on ecosystem function and quality.