Microconchid tubeworms (Class Tentaculita) from the Joggins Formation (Pennsylvanian), Nova Scotia, Canada

2014 ◽  
Vol 51 (7) ◽  
pp. 669-676 ◽  
Author(s):  
Michał Zatoń ◽  
Melissa Grey ◽  
Olev Vinn

Microconchids have been described from the classic Pennsylvanian locality at Joggins, Nova Scotia. These encrusting tentaculitoid tubeworms have previously been mentioned and described from Joggins under the polychaete genus Spirorbis. Detailed morphological and microstructural investigation revealed that they belong to the species Microconchus carbonarius Murchison, confirming the previous tentative assignment (as Spirorbis carbonarius) made by Sir J. William Dawson in the nineteenth century. The occurrence of the same species in Upper Carboniferous deposits of England provides evidence supporting a connection between England and Nova Scotia in the Late Carboniferous (Pennsylvanian). Migration of the species could have been possible via brackish seas connecting both areas during maximum sea level during the Pennsylvanian. The species inhabited retrograding poorly drained coastal plain and open-water brackish environments, encrusting bivalve shells and plant remains in both sandstone and limestone deposits. Their high density (up to 19 individuals/cm2) may have resulted from their aggregative behaviour, high fecundity, and a lack of any competition with other skeleton-bearing encrusters. The large number (34%) of regenerated tubes indicates that microconchids were often preyed upon by associated animals, most probably fishes, which could graze on their dense encrusting aggregations.

2016 ◽  
Author(s):  
Robert K. Poirier ◽  
◽  
Thomas M. Cronin ◽  
Thomas M. Cronin ◽  
Miriam E. Katz ◽  
...  

Geology ◽  
1985 ◽  
Vol 13 (9) ◽  
pp. 661 ◽  
Author(s):  
Alan Ruffman ◽  
Ann A. L. Miller ◽  
David B. Scott

1994 ◽  
Vol 68 (3) ◽  
pp. 217-224 ◽  
Author(s):  
Irene C. Wisheu ◽  
Cathy J. Keddy ◽  
Paul A. Keddy ◽  
Nicholas M. Hill

2020 ◽  
Vol 12 (2) ◽  
pp. 331-335
Author(s):  
Morris W. Foster ◽  
Emily E. Steinhilber

AbstractThe nineteenth-century experiences of yellow fever epidemics in New Orleans and Norfolk present historical parallels for how those cities, and others, are experiencing existential threats from climate change and sea level rise in the twenty-first century. In particular, the nineteenth-century “sanitary reform” movement can be interpreted as a model for challenges facing twenty-first-century “climate resilience” initiatives, including denialism and political obfuscation of scientific debates as well as tensions between short-term profit and the cost of long-term infrastructure investments and between individualism and communitarianism. The history of sanitary reform suggests that, at least in the United States, climate resilience initiatives will advance largely on a regional basis through extended local debates around these and other challenges until resilient infrastructure and practices are taken for granted, much as sanitary waterworks and sewers are today.


2021 ◽  
Vol 9 ◽  
Author(s):  
Grace D. Molino ◽  
Zafer Defne ◽  
Alfredo L. Aretxabaleta ◽  
Neil K. Ganju ◽  
Joel A. Carr

Coastal salt marshes, which provide valuable ecosystem services such as flood mitigation and carbon sequestration, are threatened by rising sea level. In response, these ecosystems migrate landward, converting available upland into salt marsh. In the coastal-plain surrounding Chesapeake Bay, United States, conversion of coastal forest to salt marsh is well-documented and may offset salt marsh loss due to sea level rise, sediment deficits, and wave erosion. Land slope at the marsh-forest boundary is an important factor determining migration likelihood, however, the standard method of using field measurements to assess slope across the marsh-forest boundary is impractical on the scale of an estuary. Therefore, we developed a general slope quantification method that uses high resolution elevation data and a repurposed shoreline analysis tool to determine slope along the marsh-forest boundary for the entire Chesapeake Bay coastal-plain and find that less than 3% of transects have a slope value less than 1%; these low slope environments offer more favorable conditions for forest to marsh conversion. Then, we combine the bay-wide slope and elevation data with inundation modeling from Hurricane Isabel to determine likelihood of coastal forest conversion to salt marsh. This method can be applied to local and estuary-scale research to support management decisions regarding which upland forested areas are more critical to preserve as available space for marsh migration.


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