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Horseshoe crab spawning in the Delaware Bay: a potential response to sea surface

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TitleInfo
Title
Horseshoe crab spawning in the Delaware Bay: a potential response to sea surface
Name (type = personal)
NamePart (type = family)
Thatcher
NamePart (type = given)
Sean
NamePart (type = date)
1990-
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Sean Thatcher
Role
RoleTerm (authority = RULIB)
author
Name (type = personal)
NamePart (type = family)
Lathrop
NamePart (type = given)
Richard G
DisplayForm
Richard G Lathrop
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Advisory Committee
Role
RoleTerm (authority = RULIB)
chair
Name (type = personal)
NamePart (type = family)
Schneider
NamePart (type = given)
Laura
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Laura Schneider
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Advisory Committee
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RoleTerm (authority = RULIB)
internal member
Name (type = personal)
NamePart (type = family)
Robinson
NamePart (type = given)
David
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David Robinson
Affiliation
Advisory Committee
Role
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internal member
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NamePart
Rutgers University
Role
RoleTerm (authority = RULIB)
degree grantor
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NamePart
School of Graduate Studies
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school
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Text
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theses
Genre (authority = ExL-Esploro)
ETD graduate
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2020
DateOther (type = degree); (qualifier = exact); (encoding = w3cdtf)
2020-10
Language
LanguageTerm (authority = ISO 639-3:2007); (type = text)
English
Abstract (type = abstract)
The American horseshoe crab Limulus polyphemus (HSC) spawns in their greatest densities in the Delaware Bay; however, over-harvests have reduced their population size by 90% in the late 20th century and climate change is degrading their spawning habitat. Because their eggs are an important food source for threatened shorebird species and adjust the timing they spawn due to ocean temperatures efforts were made to understand sea surface temperatures (SSTs) throughout the Bayshore area, patterns of egg cluster abundances and surface densities, identify a SST threshold for peak spawning activity, and use physical characteristics related to specific sites identified as increasing egg abundances. The highest egg abundances – specifically clusters – were in the southern region and decreased northward, while SSTs showed the opposite pattern. Surface egg densities were also the most abundant in the Southern region but are believed to be transported widely within and between regions. The CART analysis identified that the five-day moving average for SST of 17° C when abundance shifted from pre-peak to post-peak and currently occurs between May 29 and June 5. This temperature threshold was determined to have advanced by several days for all regions and beaches with the Northern region experiencing the most significant advancement, suggesting that a potential does exist for a mismatch to develop if HSCs spawn earlier to match this advancement. Beach nourishment activities will be important for the continued existence of suitable habitat for HSC spawning in the Bayshore area and should focus on increasing the physical parameters that increase cluster abundance such as having sand depth of at least 40 cm and beach width of at least 22 m. As climate change continues to alter the physical habitat in the Bayshore area, continued monitoring of when HSCs are spawning as a response to SST will be important to understand if this mismatch is developing, potentially jeopardizing the recovering red knot population. The MUR dataset is a useful and time and cost-efficient way to monitor SSTs in the Bayshore area for both beaches and regions, allowing it to be implemented in surveying HSC spawning to identify more specific temperature patterns.
Subject (authority = RUETD)
Topic
Geography
Subject (authority = local)
Topic
Sea surface temperature
Subject (authority = LCSH)
Topic
Limulus polyphemus
RelatedItem (type = host)
TitleInfo
Title
Rutgers University Electronic Theses and Dissertations
Identifier (type = RULIB)
ETD
Identifier
ETD_11271
PhysicalDescription
Form (authority = gmd)
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application/pdf
InternetMediaType
text/xml
Extent
1 online resource (xiii, 91 pages) : illustrations
Note (type = degree)
M.S.
Note (type = bibliography)
Includes bibliographical references
Subject (authority = lcsh/lcnaf)
Geographic
Delaware Bay (Del. and N.J.)
RelatedItem (type = host)
TitleInfo
Title
School of Graduate Studies Electronic Theses and Dissertations
Identifier (type = local)
rucore10001600001
Location
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NjNbRU
Identifier (type = doi)
doi:10.7282/t3-ntxd-ym59
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Rights

RightsDeclaration (ID = rulibRdec0006)
The author owns the copyright to this work.
RightsHolder (type = personal)
Name
FamilyName
Thatcher
GivenName
Sean
Role
Copyright Holder
RightsEvent
Type
Permission or license
DateTime (encoding = w3cdtf); (qualifier = exact); (point = start)
2020-10-01 08:11:19
AssociatedEntity
Name
Sean Thatcher
Role
Copyright holder
Affiliation
Rutgers University. School of Graduate Studies
AssociatedObject
Type
License
Name
Author Agreement License
Detail
I hereby grant to the Rutgers University Libraries and to my school the non-exclusive right to archive, reproduce and distribute my thesis or dissertation, in whole or in part, and/or my abstract, in whole or in part, in and from an electronic format, subject to the release date subsequently stipulated in this submittal form and approved by my school. I represent and stipulate that the thesis or dissertation and its abstract are my original work, that they do not infringe or violate any rights of others, and that I make these grants as the sole owner of the rights to my thesis or dissertation and its abstract. I represent that I have obtained written permissions, when necessary, from the owner(s) of each third party copyrighted matter to be included in my thesis or dissertation and will supply copies of such upon request by my school. I acknowledge that RU ETD and my school will not distribute my thesis or dissertation or its abstract if, in their reasonable judgment, they believe all such rights have not been secured. I acknowledge that I retain ownership rights to the copyright of my work. I also retain the right to use all or part of this thesis or dissertation in future works, such as articles or books.
Copyright
Status
Copyright protected
Availability
Status
Open
Reason
Permission or license
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Technical

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DateCreated (point = end); (encoding = w3cdtf); (qualifier = exact)
2020-10-01T16:17:56
DateCreated (point = end); (encoding = w3cdtf); (qualifier = exact)
2020-10-01T16:17:56
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