Salt spray and edaphic factors maintain dwarf stature and community composition in coastal sandplain heathlands

North American coastal sandplain heathlands are unique in species composition and vegetation, but the extent to which edaphic factors influence the structure of these communities is currently debated. It was hypothesized that salt spray and edaphic factors maintain the dwarf stature and community composition of heathlands by limiting plant growth and excluding competitively dominant woody species close to the ocean. Field surveys were carried out to investigate the spatial patterns of salt spray accumulation, soil salt and soil moisture. High salt spray correlated significantly with increased leaf necrosis and water stress in Myrica pensylvanica and with decreased plant height. Plant community composition changed across a salt spray and soil gradient, as well. Distinctive sub-communities were identified that separated according to soil salt and soil moisture but salt spray was the main factor affecting sites occupied only by heathland vegetation. Results from this study suggest that salt spray suppresses the growth of heathland plants in close proximity to the ocean, and therefore maintains the low stature in these dwarf shrublands. This research also demonstrates that the physical environment influences the community structure in heathlands, particularly by limiting tree species from growing in high salt spray, low water availability sites.     

Use of cryostat sections for measurement of Ca2+ uptake by sarcoplasmic reticulum.

Calcium uptake of cardiac muscle and fast-twitch and slow-twitch skeletal muscle of rabbit was measured in 10-μm thin sections. Ca²⁺ uptake showed K⁺, Mg²⁺, Ca²⁺, and oxalate dependence and required ATP. The contribution of mitochondria to the Ca²⁺ uptake could be ruled out, since inclusion of ruthenium red or sodium azide in the medium did not show inhibition. The method, which avoids unphysiological fragmentation of the sarcoplasmic reticulum, has the added advantage of requiring only 0.1 to 0.3 g of muscle and permitting simultaneous histochemical studies from the same muscle block.     

The Possible Importance of Primary Amino Nitrogen in Nitrogen Regeneration by Coastal Marine Sediments in Buzzards Bay,Massachusetts

To investigate the role of primary amino nitrogen (PAN) in nitrogen regeneration by marine sediments, the distribution and fluxes of PAN in organic-rich coastal sediments off Massachusetts (USA) were investigated. Decreases with depth in the sediment of total organic carbon, organic nitrogen, and PAN contents indicate that organics with C to N ratios of about 6, such as primary amines, are selectively consumed. Near the sediment surface, dissolved PAN (DPAN) accumulates and supports a large DPAN flux into the water column and this flux greatly exceeds the inorganic nitrogen flux. Consumption of C, N, and PAN was investigated using diagenetic equations describing their exponentially decreasing distributions with depth and which included the effects of sediment mixing, sediment accumulation, and consumption, considered to be a first-order reaction rate. Calculations showed that the reaction rate constant for PAN was between 5.1 and 26.1 times faster than that for the utilizable organic N and the depth-integrated consumption of PAN accounted for between 8.6 and 43.9% of the N disappearance rate. These ranges are estimated when sediment accumulation dominates over sediment mixing (the lower values) and when mixing dominates over accumulation (the upper values). Although the magnitude of D is unknown, these calculations indicate that PAN, which comprises less than 2% of the organic N, has an important role in sedimentary nutrient dynamics because of its enhanced reactivity.     

Terrestrial Passive Integrated Transponder Antennae for Tracking Small Animal Movements

ABSTRACT Measuring terrestrial movements of small animals poses a substantial technological challenge. We developed very long (up to 130 m) passive integrated transponder (PIT) detectors with which we tracked salamanders (Caudata) migrating from breeding ponds to their upland habitat >200 m away. In all 60 trials, salamanders were detected when released near the antennae. In a second test, we tracked 7 of 14 tagged marbled salamanders (Ambystoma opacum) migrating >65 m, well beyond the area protected by existing wetland buffer regulations in Massachusetts, USA. The mean rate of movement for these salamanders (x̄ = 0.9 m/min; SE = 0.1 m/min) was substantially higher than rates of movement reported for related salamanders with radio-implants. These PIT antennae offer researchers a means to study small animal movements with less disruption of the animals’ natural movement patterns than is caused by other available techniques.     

Bird migration times, climate change, and changing population sizes

Past studies of bird migration times have shown great variation in migratory responses to climate change. We used 33 years of bird capture data (1970–2002) from Manomet, Massachusetts to examine variation in spring migration times for 32 species of North American passerines. We found that changes in first arrival dates – the unit of observation used in most studies of bird migration times – often differ dramatically from changes in the mean arrival date of the migration cohort as a whole. In our study, the earliest recorded springtime arrival date for each species occurred 0.20 days later each decade. In contrast, the mean arrival dates for birds of each species occurred 0.78 days earlier each decade. The difference in the two trends was largely explained by declining migration cohort sizes, a factor not examined in many previous studies. We found that changes in migration cohort or population sizes may account for a substantial amount of the variation in previously documented changes in migration times. After controlling for changes in migration cohort size, we found that climate variables, migration distance, and date of migration explained portions of the variation in migratory changes over time. In particular, short-distance migrants appeared to respond to changes in temperature, while mid-distance migrants responded particularly strongly to changes in the Southern Oscillation Index. The migration times of long-distance migrants tended not to change over time. Our findings suggest that previously reported changes in migration times may need to be reinterpreted to incorporate changes in migration cohort sizes.     

Mechanical Land Clearing to Promote Establishment of Coastal Sandplain Grassland and Shrubland Communities

The decline in grasslands and other species‐rich early successional habitats on the coastal sandplains of the northeastern United States has spurred management to increase the area of these declining plant communities. We mechanically removed overstory oak and applied seed from a nearby sandplain grassland on the island of Martha’s Vineyard, Massachusetts, to evaluate this technique for creating an open oak community able to support sandplain herbaceous species. We compared vegetation structure and composition before and after clearing in an area of total tree removal (clearcutting), an area where 85% of tree basal area was removed (savanna cutting), and in adjacent coastal oak forest. Plant responses to clearcutting and savanna cutting were similar. Sandplain herbs colonized at high frequencies after seeding and increased herbaceous cover from less than 7% before clearing to 22–38% three growing seasons later. Pennsylvania sedge (Carex pensylvanica) increased in cover approximately 6‐fold, accounting for 84–90% of the increased herbaceous cover. Other native ruderals and exotic herbs reached 2 and less than or equal to 1%, cover, respectively, after three years. Species richness across cleared treatments increased from 30 to 79 species. All forest species were retained. Forest shrubs and trees initially declined from their dominant cover but rebounded after three years. Tree clearing plus seeding appeared to be a viable management practice for increasing cover of herbaceous sandplain species while causing minimal increases in exotic herbaceous cover. The long‐term persistence of sandplain herbs may require periodic disturbances that limit woody regrowth.