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Locality & Methods Shells dredged from two offshore sites (10m, 30m) Each site is similar in sedimentological and other physical characteristics 10 m 30 m Grain size distribution by site Gravel (%) Very coarse sand (%) Coarse sand (%) Medium sand (%) Fine sand (%) Very fine sand (%) Mud (%) Weight Percent Site 1: 30 m Site 9: 10 m 10 m site30 m site % carbonate25 Temperature (°C)21.4*21.2* Salinity (‰)35*34* *Mean annual measurements Barbour Wood et al. (2006) Quaternary Research
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Age Mixing Among Sympatric Bivalves Age Mixing Among Sympatric Bivalves and Brachiopods from the Brazilian and Brachiopods from the Brazilian
South AtlanticSouth AtlanticRichard A. Krause Jr.1, Susan L. Barbour-Wood2, Michał Kowalewski1, Marcello G. Simões3, Darrell Kaufmann4,
Christopher S. Romanek5, and John F. Wehmiller6
1Virginia Polytechnic Institute and State University2Colby College
3Universidade Estadual Paulista4Northern Arizona University
5Savannah River Ecology Laboratory, University of Georgia6University of Delaware
Introduction
How does time averaging compare among two very different organisms collected from the same environment?
Part 1:Comparisons of age-frequency distributions among brachiopods and bivalves
Part 2:Investigation of the relationship between depth and time averaging duration
Locality & Methods
• Shells dredged from two offshore sites (10m, 30m)
• Each site is similar in sedimentological and other physical characteristics
10 m
30 m
Grain size distribution by site
0
10
20
30
40
50
60
Gra
vel (
%)
Ver
y co
arse
san
d (%
)
Coa
rse
sand
(%)
Med
ium
san
d (%
)
Fine
san
d (%
)
Ver
y fin
e sa
nd (%
)
Mud
(%)
Wei
ght P
erce
nt
Site 1: 30 m Site 9: 10 m
10 m site 30 m site
% carbonate 25 25
Temperature (°C) 21.4* 21.2*
Salinity (‰) 35* 34*
*Mean annual measurements
Barbour Wood et al. (2006) Quaternary Research
Physical Characteristics
10 mm
Semele casaliBouchardia rosea
Semele casali
- thin shell- low organic content- aragonitic*infaunal life habit
Bouchardia rosea
- robust shell- high organic content- calcitic*epifaunal life habit
Amino Acid Racemization DatingAmino Acid Racemization Dating
• 178 shells dated in this study
• D/L aspartic acid ratios calculated in several replicates for each shell
• Calibrated with 19 AMS radiocarbon dates
Samples taken from hinge area to minimize intrashell variability (Brigham, 1983; Carroll et al., 2003)
Age CalibrationAge Calibration
Brachiopods 30 m
0.000
0.100
0.200
0 2 4 6 8
Brachiopods 10 m
0.000
0.100
0.200
0 2 4 6
Bivalves 10 m
0.000
0.010
0.020
0 1 2 3
Bivalves 30 m
0.0000.0100.0200.0300.040
0 1 2 3
(D/L
Asp
2.7 )
(D/L
Asp
2.7 )
(D/L
Asp
2.7 )
(D/L
Asp
2.7 )
Calibrated kyrs
Calibrated kyrs
Calibrated kyrs
Calibrated kyrs
Adj. r2 = 0.970 p = 0.0014
Adj. r2 = 0.915p = 0.0287
Adj. r2 = 0.971 p = 0.0096
Adj. r2 = 0.978 p = 0.0001
0000232.0
0225.07.2AspAge
0000084.0
0019.07.2AspAge
0000106.0
00005.07.2AspAge
0000487.0
0044.07.2AspAge5 14C dated shells
4 14C dated shells
4 14C dated shells
6 14C dated shells
Barbour Wood et al. (2006) Quaternary Research
Wilcoxon two-sample testZ=-1.89, p=0.0582Kolmogorov-Smirnov testD=0.186, p=0.0996
0
5
10
15
20
25
0
5
10
15
20
1 2 3 4 5 6 7 8 9 100Age (kyrs)
1 2 3 4 5 6 7 8 9 100Age (kyrs)
Freq
uenc
yFr
eque
ncy
Age-Frequency Distribution ComparisonsAge-Frequency Distribution Comparisons
Brachiopods, n=103
Bivalves, n=75
Wilcoxon two-sample testZ=5.04, p<0.0001Kolmogorov-Smirnov testD=0.409, p<0.0001
0
5
0
5
10
15
20
25
30
35
30 m site, n=69
1 2 3 4 5 6 7 8 9 100Age (kyrs)
1 2 3 4 5 6 7 8 9 100Age (kyrs)
Freq
uenc
yFr
eque
ncy
Age-Frequency Distribution ComparisonsAge-Frequency Distribution Comparisons
10 m site, n=109
0
5
0
50
5
10
15
20
Brachiopods 30m, n = 32
0
5
10
15
20Brachiopods 10 m
n = 71
Age-Frequency Distribution ComparisonsAge-Frequency Distribution ComparisonsBrachiopods, between-sitesWilcoxon two-sample testZ=5.49, p<0.0001Kolmogorov-Smirnov testD=0.625, p<0.0001
Bivalves, between-sitesWilcoxon two-sample testZ=2.38, p=0.017Kolmogorov-Smirnov testD=0.472, p=0.0005
Bivalves 10 mn = 38
Bivalves 30 mn = 37
1 2 3 4 5 6 7 8 9 100
1 2 3 4 5 6 7 8 9 100Age (kyrs)
Age (kyrs)
Freq
uenc
yFr
eque
ncy
30m site, between-speciesWilcoxon two-sample testZ=4.21, p<0.0001Kolmogorov-Smirnov testD=0.625, p<0.0001
10m site, between-speciesWilcoxon two-sample testZ=-1.04, p=0.300Kolmogorov-Smirnov testD=0.188, p=0.344
Brachiopods 30m (n=32)Brachiopods 10m (n=71)
Bivalves 30m (n=37)Bivalves 10m (n=38)
Brachiopods (103)Bivalves (n=75)
0 1 2 3 4Standard Deviation (kyrs)
0 1 2 3 4Semi-Quartile Range (kyrs)
10m site (n=109)30m site (n=69)
Summary of the Data
-Brachiopods and bivalves exhibit similar duration of time averaging when sites are pooled
- Site-to-site variation can impose significant differences, even in the same oceanographic province
95% Confidence intervals from separate 5000 (SQR) and 1000 (SD) iteration bootstrap simulations.
1
2
nxx
SD 213 QQSQR
Exploring the Relationship Between Time Averaging Magnitude and Depth
0
10
20
30
40
0 1 2 3 4 5 60
10
20
30
40
0 1 2 3 40
10
20
30
40
0 1 2 3 4kyrs
Dep
th (m
) Meann = 21
Standard Deviation (SD)n = 21
Semi-quartile Range (SQR)n = 21
Meta-analysis restricted to siliciclastic-dominated inner-shelf settings, but a variety of depositional systems and oceanographic settings were included
Meta-analysis data sources:Bahia la Choya, Gulf of California, Mexico (Flessa et al. 1993)Bahia Concepcion, Gulf of California, Mexico (Meldahl et al. 1997)Colorado Delta, Gulf of California, Mexico (Kowalewski et al. 1998)Ubatuba Bay, Brazil (Carroll et al. 2003; This study)Caribbean Coast of Panama (Kidwell et al. 2005)
kyrskyrs
Possible Factors: sea level history; sedimentation rate; many others...
An increase in time averaging duration with increasing depth?
Exploring the Relationship Between Time Averaging Magnitude and Depth
0
10
20
30
40
0 1 2 3 4 5 60
10
20
30
40
0 1 2 3 40
10
20
30
40
0 1 2 3 4kyrs
Dep
th (m
)
Age
Dep
th
Age
Dep
th
Age
Dep
th
Age
Dep
th
kyrskyrs
Null Models
Linear Logarithmic Directional Trend Passive TrendDirect Relationships Indirect Relationships
Meann = 21
Standard Deviation (SD)n = 21
Semi-quartile Range (SQR)n = 21
0
0.5
1
0 10 20 30 40
Threshold sample size
-1-0.5
00.5
1
0 10 20 30 40
-0.5
0
0.5
1
0 10 20 30 40
0.01
0.1
1
0 10 20 30 40
0.01
0.1
1
0 10 20 30 40
0.01
0.1
1
0 10 20 30 40
Threshold sample size
Adj. r2
Mean
SD
SQR
Adj. r2
Adj. r2
pMean
SD
SQR
p
p
Determination of adequate sample size using regression
PreferredThreshold Sample Size = 4
Age (kyrs)
Dep
th (m
)
Age
Dep
th
Age (kyrs) Age (kyrs)
0
10
20
30
40
0 1 2 3 4 5 60
10
20
30
40
0 1 2 3 40
10
20
30
40
0 1 2 3 4
Direct Relationships
Mean SD SQR
Linear
Adj. r2 = 0.326p = 0.019
Adj. r2 = 0.245p = 0.041
Adj. r2 = 0.332p = 0.018
Mean SD SQR
Adj. r2 = 0.296p = 0.026
Adj. r2 = 0.159p = 0.088*
Adj. r2 = 0.373p = 0.016
Age
Dep
th
Logarithmic
Meann = 14
Standard Deviation (SD)n = 14
Semi-quartile Range (SQR)n = 14
Age (kyrs)
Dep
th (m
)
Age (kyrs) Age (kyrs)
0
10
20
30
40
0 1 2 3 4 5 60
10
20
30
40
0 1 2 3 40
10
20
30
40
0 1 2 3 4
Age
Dep
th
Age
Dep
th
Directional Trend Passive Trend
Indirect Relationships
More difficult to test for these models
More data are needed from a variety of environments
Meann = 14
Standard Deviation (SD)n = 14
Semi-quartile Range (SQR)n = 14
Conclusions: Part 1
1. Brachiopod and bivalve age-frequency distributions vary between sites1. No clear trend in differences between sites: indicates stochastic variation in taphonomic
processes
2. When pooled, brachiopods and bivalves have very similar duration of time averaging
3. Biological properties (shell mineralogy, life habit etc.) may not be as important as the frequency and intensity of taphonomic processes in determining time averaging duration for these two groups
Conclusions: Part 2
1. For pooled data, there is a suggestion of a relationship between time averaging duration and depth
1. Time averaging duration generally increases with depth
2. This putative relationship holds for bivalves and brachiopods
3. Relationship may be direct or indirect, more data is needed