Discordance between living and death assemblages as evidence for anthropogenic ecological change

Kidwell. 10.1073/pnas.0707194104

Supporting Information

Files in this Data Supplement:

SI Table 1
SI Figure 4
SI Text
SI Figure 5
SI Figure 6
SI Figure 7
SI Table 2
SI Figure 8




SI Figure 4

Fig. 4. Scatterplots of 73 large (at least 20 live and 20 dead individuals) estuarine data sets, coded by AE, showing lack of variation in taxonomic similarity (Jaccard-Chao index; Left) and rank-order correlation of species abundances (Spearman rho; Right), as a function of (A and B) number of stations pooled to generate each habitat-level data set; (C and D) number of live species in the data set, which is proportional to the log of live individuals sampled, and is usually smaller than the number of dead species and individuals; (E and F) ratio of dead: live individuals; (G and H) mesh size in mm; and (I and J) bottom habitat type, coded as 1 = mud (<10% sand), 2 = sandy mud (<50% sand), 3 = muddy sand (<50% mud), 4 = clean sand (<~ 5% mud), 5 = shell or lithic gravel, gravelly sediments of any kind, 6 = grassbed. Data sets from AE1 and especially AE2 settings typically have smaller sample sizes and none were processed using mesh >1.5 mm, but AE0 data sets commonly have the same characteristics and yet yield on average higher fidelity.





SI Figure 5

Fig. 5. Scatterplot of raw proportional abundance of the opportunistic bivalve Mulinia lateralis in data sets from Gulf of Mexico lagoons and bays. Coarse-mesh data sets are from Tabasco and Veracruz, Mexico, and from Laguna Madre, southern Texas. Fine-mesh data sets are from northern Texas. Mulinia is relatively rare both alive and dead among pristine lagoons (all but one data set have proportional abundances <10%), with good live-dead agreement in proportional abundance. Mulinia ranges up to ~ 60% alive and 75% dead in AE ≥ 1 lagoons and is commonly among the most abundant or is the most abundant species, consistent with greater stress, such as from episodic hypoxia associated with AE. Death assemblages in AE ≥ 1 settings are not, however, consistently enriched in Mulinia compared to the living community, in part because of the dead-abundance of grass-dwellers and other relictual species.





SI Figure 6

Fig. 6. Same plot as Fig. 2, but for 34 open shelf data sets. Solid line connects mean values for each AE category with 95% confidence intervals on the standard error. (Upper) J-C declines significantly with increasing AE score, based both on comparison of means (solid line, 95% confidence intervals on the standard error of the mean) and medians (Kruskal-Wallis H = 14.0, P = 0.0009). The three pristine AE0 data sets having lowest J-C values are from the Amazon (fine-mesh, high nutrients from upwelling) and Yucatan (coarse-mesh, oligotrophic). The five AE1 data sets having highest J-C values are from three different shelves (fine-mesh Milazzo and Galveston, coarse-mesh Eddystone), and the five AE1 data sets having the lowest J-C values are from four different shelves (fine-mesh Milazzo, Brucoli; coarse-mesh Livorno, Eddystone). (Lower) Spearman rho declines significantly with severe AE2, based both on comparison of means and medians (Kruskal-Wallis H = 6.6, P = 0.0369). Summary statistics for pristine shelves (n = 18): mean J-C = 0.89 ± 0.06, with 95% confidence intervals calculated on the standard error; median = 0.92. The range of rank-order agreement is broad, but all correlations are positive and most are significantly so (61% of rhos positive at P < 0.05, 39% at P < 0.01, following sequential Bonferroni correction; mean rho = 0.41 ± 0.08, median = 0.38). For AE ≥ 1 shelves (n = 16): mean J-C = 0.51 ± 0.16, median = 0.42. The range of rank-order agreement is very broad, from -0.58 to 0.53, with 75% significant at P < 0.05 and 56% significant at P < 0.01; mean rho = 0.19, median = 0.33.





SI Figure 7

Fig. 7. Scatterplots of 34 large (at least 20 live and 20 dead individuals) data sets from open shelves, coded by AE, showing lack of variation in taxonomic similarity (Jaccard-Chao index; Left) and rank-order correlation of species abundances (Spearman rho; Right), as a function of (A and B) number of stations pooled to generate each habitat-level data set; (C and D) number of live species in the data set, which is proportional to the log of live individuals sampled, and is usually smaller than the number of dead species and individuals; (E and F) ratio of dead: live individuals; (G and H) mesh size in mm; and (I and J) bottom habitat type, coded as 1 = mud (<10% sand), 2 = sandy mud (<50% sand), 3 = muddy sand (<50% mud), 4 = clean sand (<~ 5% mud), 5 = shell or lithic gravel, gravelly sediments of any kind, 6 = grassbed. Data sets from AE1 and especially AE2 settings typically have smaller sample sizes and none were processed using mesh >1.5 mm, but AE0 data sets commonly have the same characteristics and yet yield on average higher fidelity. Study areas and sources listed in SI Table 2.





SI Figure 8

Fig. 8. Same scatterplots as Fig. 1, but with rectangles outlining ± 1 (solid line) and ± 2 (dotted line) standard deviations of the population mean of Jaccard-Chao and Spearman rho for pristine data sets. In A and B, the larger pair of rectangles indicate the SD1 and SD2 boxes if the outlying pristine data set is included, and the smaller pair of rectangles exclude the outlier. If the broader SD2 and SD1 rectangles are used, the false-negative rate for AE ≥ 1 estuarine data sets increases from the 43 and 29% values given in the text to 76 and 42% respectively. A. Among the pristine estuarine data sets, the low-fidelity outlier is an unvegetated silty sand in Smuggler's Bay, Virgin Islands (1). This area receives some allochthonous material from adjacent seagrass beds during major storms (2), perhaps contributing to its low taxonomic similarity, but an alternate or contributing factor might be taphonomic inertia to a recent loss of seagrass from natural or anthropogenic processes other than AE, or perhaps greater time-averaging owing to intense, deeply penetrating burrowing by callianassid shrimp (A. I. Miller, personal communication). (C) Among the pristine open-shelf data sets, the two data sets with lowest J-C and rho are from the Amazon shelf (relictual sand habitat) and Yucatan (open sea habitat), which are from opposite ends of the nutrient-level spectrum and mesh-size spectra (0.5 and 3 mm); both shelves are tropical, wide, and had no bottom-trawling. The third nearby data set (J-C~ 0.55, rho ~ 0.4) is a firm muddy-sand habitat from the Amazon shelf. These three data sets thus do not distinguish themselves from the other pristine data sets in terms of physical environmental or methodological variables. (D) Among open-shelf AE1 data sets, the low-J-C, low-rho outlier is from sandy patches within a seagrass-rich area (Livorno); the death assemblage contains abundant dead specimens of seagrass-dwellers, probably reflecting a combination of small-scale postmortem transportation of grass-dwellers and short-term stochastic variation in sand-grassbed boundaries. This portion of the cross-plot is otherwise occupied only by AE >1 data sets.

1. Miller AI (1988) Paleobiology 14: 91-103.

2. Miller AI, Llewellyn G, Parsons KM, Cummins H, Boardman MR, Greenstein BJ, Jacobs DK (1992) Geology 20:23-26.





Table 1. Estuaries and lagoons with studies reporting the quantitative composition of both living and dead shelled mollusks, organized by extent of anthropogenic eutrophication (AE) at the time of sampling (year)

Pristine (Score 0)

Year sampled

N datasets

Mesh, mm &Author

Other human impacts

Mugu Lagoon, CA

1963-64, 1969-71

3 (3)

3 Warme, 2 Peterson

none

Islas Cancun & Contoy, QR

1971

2 (2)

3 Ekdale

none

Mannin Bay, Ireland

1972

5 (5)

0.5 Bosence

none

Doboy Sound, GA

1977-78

1 (1)

1.5 Henderson

SFm (shrimp)

Lag. La Mancha, VZ

1978

4 (4)

1.5 Reguero

SFa (mollusks)

Smuggler's Bay, USVI

1979-80

3 (3)

5 Miller

none

Lag. Madre, TX

1981-82, 1984

6 (6)

0.5 Staff, 5 Smith

Dr, Sal

Mljet Island, Croatia

late 1990s

4 (3)

5 Peharda

none

Possibly AE (Score 0.5)

 

 

 

 

Tomales Bay, CA

1959

5 (4)

1.5 Johnson

SFm (oysters), Tox

Tijuana Slough, CA

1969-71

1 (1)

2 Peterson

SFa (bait)

Mild or diffuse AE (Score 1)

 

 

 

 

Hamana Lake, Japan

1956

3 (2)

1 Tsuchi

Sal, SFa

Chesapeake Bay, MD

1966

3 (2)

1 Jackson

SFm (oysters)

West Bay, TX

1976-77

6 (5)

1 White

Dr, SFm

Copano Bay, TX

1976, 1981-82

7 (7)

1 Calnan, 0.5 Staff

SFm (oysters), Tox

Lag. Carmen-Machona, TB

1979

6 (5)

1.5 Reguero

Sal, SFa (mollusks), Tox, Dr

Lag. Mandinga-Larga, VZ

1980

2 (1)

1.5 Reguero

SFa (mollusks), Tox

Lag. Sontecomapan, VZ

1980

3 (2)

1.5 Garcia-Cubas

SFa (mollusks)

Lag. Chica-Grande, VZ

1980

3 (2)

1.5 Garcia-Cubas

SFa (mollusks)

Lag. Camaronera, VZ

1980

1 (1)

1.5 Reguero

SFa (mollusks)

Possibly severe AE (Score 1.5)

 

 

 

 

East & Galveston Bays, TX

1976

5 (4)

1 White

Tox, SFm (oysters), Dr

Trinity Bay, TX

1976

4 (1)

1 White

Tox, SFm (oysters)

 

 

 

 

 

Severe AE (Score 2)

 

 

 

 

Lag. Mecoacan, TB

1979

2 (1)

1.5 Reguero

SFa (mollusks), Tox

Lag. Alvarado, VZ

1980

2 (2)

1.5 Reguero

SFa (mollusks), Sol, Tox

Lag. Pueblo Viejo, VZ

1980

2 (2)

1.5 Reguero

SFa (mollusks), Tox, Sol

Lag. Tampamachoco,

VZ

1980

2 (2)

1.5 Reguero SFa (mollusks), Tox

Lag. Tupilco-Ostion, TB

1980

2 (2)

1.5 Reguero

SFa (mollusks), Tox, Sal

 

 

 

 

 

Uncertain AE

 

 

 

 

Heta Bay, Japan

1950s

3 (3)

1 Tsuchi

no information

Arari Bay, Japan

1950s

3 (1)

1 Tsuchi

no information

Total number of habitat-level data sets, with number of large data sets in parentheses (at least 20 live and 20 dead individuals after pooling all samples for a given sedimentary bottom type in that study area). Mesh size in mm, with only the first author identified; for full references including unpublished data, see SI Text. Other human modification in the study area, active either at the time of sampling or in preceding decades, but not necessarily directly impacting all habitats are as follows: SFa, artisanal shellfishing; SFm, mechanical shellfishing or bottom-trawling; Sol, solid sediment runoff; Dr, dredging and/or spoil dumping; Tox, toxic pollution; Sal, salinity change from inlet cutting or pumping. U.S. and Mexican states: CA, California; TX, Texas; GA, Georgia; MD, Maryland; QR, Quintana Roo; TB, Tabasco; VZ, Veracruz.





Table 2. Open shelf study areas and habitat-level data sets used here

Study area

Latitude

Shelf width

Year sampled

N of censuses

Mesh size

AE

Trawling

Habitat

Live N

Dead N

Total species

Source

Eddystone, English Channel, UK

50° N

350

1931

1

1.5

AE0

T

lithic gravel

54

672

24

Smith 1932

Eddystone, English Channel, UK

50° N

350

1931

2 (2 mo)

1.5

AE0

T

shell gravel

34

1322

22

Smith 1932

Eddystone, English Channel, UK

50° N

350

1931

1

1.5

AE0

T

sandy gravel

21

1067

23

Smith 1932

Eddystone, English Channel, UK

50° N

350

1980-81

4 (6 mo)

2

AE1

T

shell gravel

96

13543

62

Carthew & Bosence 1986 +

Stoke Point, English Channel, UK

50° N

350

1980-81

4 (6 mo)

2

AE1

T

shell gravel

118

3466

59

Carthew & Bosence 1986 +

Plymouth Sound (outer), UK

50° N

350

1980-81

4 (6 mo)

2

AE1

T

shell gravel

4841

17847

72

Carthew & Bosence 1986 +

San Juan Islands, Washington, USA

48.5

30

2002

1

2.3

AE0

None

shell gravel

1659

5232

86

Kowalewski et al. 2003 +

Livorno, Tuscany, Italy

43° N

50

pre-1978

1

1

AE1

T

rocky sand within grassbed

163

9093

140

Biagi & Corselli 1978, Corselli 1981

Golfo Milazzo, Sicily

38° N

2.5

1985

1

0.5

AE1

T

sandy silt

85

1828

87

Giacobbe & Leonardi 1985 +

Golfo Milazzo, Sicily

38° N

2.5

1985

1

0.5

AE1

T

silty sand

56

415

56

Giacobbe & Leonardi 1985 +

Golfo Catania, Sicily

37° N

5

1980

1

1

AE1.5

T

silt

98

5501

112

Di Geronimo & Giacobbe 1983 +

Capo Campolato, Sicily

37° N

3

1980

1

1

AE1

T

mobile sandy silt on rocky ground

54

2852

129

Di Geronimo & Giacobbe 1983 +

Rhodes Island, Aegean Sea, Greece

36° N

3.5

1983-84

2 (9 mo)

0.5

AE2

T

shell gravel

67

113

53

Pancucci-Papadopoulou et al. 1999, Zenetos & van Aartsen 1995 +

Rhodes Island, Aegean Sea, Greece

36° N

3.5

1983-84

4 (9 mo)

0.5

AE2

T

silty sand

157

509

121

Pancucci-Papadopoulou et al. 1999, Zenetos & van Aartsen 1995 +

Chihama shelf, Japan

35° N

11

1958

1

1

AE0

T

shoreface sand

167

496

80

Tsuchi 1959

Oi River mouth, Suruga Gulf, Japan

35° N

5

1958

1

1

AE1.5

T?

offshore clayey mud

17

6

9

Tsuchi 1960

Oi River mouth, Suruga Gulf, Japan

35° N

5

1958

1

1

AE1.5

T?

shoreface sand

21

28

12

Tsuchi 1960

Tago-no-ura, Suruga Gulf, Pacific Japan

35° N

2

1958

1

1.2

AE2

T?

offshore mud

12

67

34

Tsuchi 1966

Tago-no-ura, Suruga Gulf, Pacific Japan

35° N

2

1958

1

1.2

AE2

T?

nearshore gravelly mud

43

29

18

Tsuchi 1966

Sapelo Island, Georgia, Atlantic USA

31° N

130

pre-1986

1

1.5

AE0

None

longshore channel shell gravel

15

24551

63

Henderson & Frey 1986 +

Sapelo Island, Georgia, Atlantic USA

31° N

130

pre-1986

1

1.5

AE0

None

shoreface sand

19

1545

17

Henderson & Frey 1986 +

Galveston, Texas, Gulf of Mexico, USA

29.5° N

180

1976-77

1

0.5