Dataset: 2018 Salt Pond
Data Citation:
Gast, R. J., Edgcomb, V. P., Pachiadaki, M. G. (2023) Environmental observations and infected host and dinospore counts in Salt Pond, Falmouth, Massachusetts, USA from 2018 through 2019. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2020-03-10 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.805612.1 [access date]
Terms of Use
This dataset is licensed under Creative Commons Attribution 4.0.
If you wish to use this dataset, it is highly recommended that you contact the original principal investigators (PI). Should the relevant PI be unavailable, please contact BCO-DMO (info@bco-dmo.org) for additional guidance. For general guidance please see the BCO-DMO Terms of Use document.
DOI:10.26008/1912/bco-dmo.805612.1
Spatial Extent: N:41.54482 E:-70.62723 S:41.54482 W:-70.62723
Temporal Extent: 2018-03-19 - 2019-08-09
Project:
Principal Investigator:
Rebecca J. Gast (Woods Hole Oceanographic Institution, WHOI)
Co-Principal Investigator:
Virginia P. Edgcomb (Woods Hole Oceanographic Institution, WHOI)
Maria G. Pachiadaki (Woods Hole Oceanographic Institution, WHOI)
Contact:
Virginia P. Edgcomb (Woods Hole Oceanographic Institution, WHOI)
BCO-DMO Data Manager:
Mathew Biddle (Woods Hole Oceanographic Institution, WHOI BCO-DMO)
Version:
1
Version Date:
2020-03-10
Restricted:
No
Validated:
Yes
Current State:
Final no updates expected
Environmental observations and infected host and dinospore counts in Salt Pond, Falmouth, Massachusetts, USA from 2018 through 2019
Abstract:
Salt Pond is a shallow, seasonally stratified coastal salt pond located in Falmouth, Massachusetts, USA and it is proximal to the labs at Woods Hole Oceanographic Institution (WHOI). This estuarine system is tidally influenced by Vineyard Sound and receives inputs of freshwater primarily from groundwater. Seasonal abiotic factors and nutrient availability in the seasonally stratified water column influence the growth and abundance of diverse microbial taxa within this system, providing an ideal setting to study syndinian parasites and host diversity temporally and across oxygen gradients. Salt Pond has anoxic waters that come within 2-3 meters of the water surface in summer and bottom waters that become increasingly sulfidic due to bacterial sulfate reduction as seasonal stratification intensifies.