# Ecosystem-Wide Impacts of Deforestation in Mangroves: The Urabá Gulf (Colombian Caribbean) Case Study

Authors: J. F. Blanco; E. A. Estrada; L. F. Ortiz; L. E. Urrego
Journal: ISRN Ecology
 (2012)

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## Abstract

Mangroves are ecologically important and extensive in the Neotropics, but they are visibly threatened by selective logging and conversion to pastures in the Southern Caribbean. The objective of this paper was to summarize the impacts of both threats on forest structure, species composition, aboveground biomass and carbon reservoir, species introgressions, and benthic fauna populations by collating past and current data and by using an interdisciplinary approach in the Urabá Gulf (Colombia) as a case study. Mangroves in the Eastern Coast have been decimated and have produced unskewed tree-diameter (DBH) distributions due to the overexploitation ofRhizophora mangle for poles (DBH range: 7–17 cm) and of Avicennia germinans for planks and pilings (DBH >40 cm). Selective logging increased the importance value of the light-tolerant white mangrove Laguncularia racemosa, also increasing biomass and carbon storage in this species, thus offsetting reductions in other species. Introgressions (cryptic ecological degradation) by L. racemosa and Acrostichum aureum (mangrove fern) and low densities of otherwise dominant detritivore snails (Neritina virginea) were observed in periurban basin mangroves. Finally, basin mangroves were more threatened than fringing mangroves due to their proximity to expanding pastures, villages, and a coastal city.


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## Body

## 1. Introduction

Mangroves dominate tropical coasts and provide important services to humans, yet they are one of the most threatened ecosystems partially due to deforestation [1–3]. Mangroves offer provisioning, regulating, supporting, and cultural services [4–6]. Provisioning services are the most commonly appreciated and include sources of timber, fibers and nonwoody products, fuels (firewood and charcoal), food (fisheries), biochemical products, and freshwater; however, the role of mangroves in climatic and hydrologic modulation, erosion control, protection against natural hazards, soil formation, and nutrient cycling has been recently recognized. In addition, different mangrove types (e.g., riverine, fringing, basin) provide specific services and support coastal fisheries to a different extent [6, 7], but they may also provide differential carbon capture capabilities [8–11].Despite the many services offered by mangroves worldwide, deforestation as a consequence of overexploitation of woody products and land reclamation is the most important threat [1–3], although a great local variation is observed [12, 13]. Deforestation rates in mangroves are four times greater than those in terrestrial tropical rain forests. South American mangroves exhibit the lowest rates compared to Asia, Africa, Northern and Central America; however, a high regional variability is observed, and hotspots do exist [13].Colombia, located in the northernmost corner of South America, with coasts in both the Caribbean and the Pacific, exhibits the largest annual deforestation rate out of the eight South American countries with mangroves [13]. With 18% of the region’s mangrove cover, deforestation rate in this country (1.1 and 0.6%) exceeded the South American average (0.69 and 0.18%) in estimates for 1980–1990 and 2000–2005. These figures may be more variable and dramatic at a subcountry level, bearing in mind that coarse-scale inventories using satellite imagery tend to overestimate mangrove cover due to low spatial resolution and heavy cloud cover (as observed in many areas of the Pacific coast and the Urabá region in the Caribbean coast) [14].Colombia’s Caribbean Coast harbors 88250 ha of mangroves strongly threatened by human activities [15–18]. These mangroves have been converted to agricultural lands, shrimp aquaculture ponds, and urban development (mostly for tourism). In addition, extraction of woody and nonwoody products has degraded many mangrove areas thus translating in low stature and slim diameter development [19–21]. Mapping this change has been, however, elusive despite the publication of mangrove cover and conservation status maps by the National Mangrove Inventory Project during the nineties [17, 18] and the fine-scale efforts conducted by state-level environmental boards afterwards [21]. Yet most of the information about deforestation remains as grey literature [15–18, 21], and, unfortunately, quantitative assessments of mangrove deforestation (using both follow-up remote sensing and field inventories) at a subnational level are scant and limited to strategic ecoregions such as the Ciénaga Grande de Santa Marta [22]. Mangrove deforestation drivers in the Colombian Caribbean coast may be similar to the observed in the Greater Caribbean Basin [16, 23], although rates seem to be lower than the few published examples from México and Panamá, two major Latin American hotspots [13]. For instance, in Quintana Roo (México) an annual deforestation rate of 0.85% (1995–2007) for fringing mangroves was mostly driven by low-density human settlements and road construction [24]. Despite the tourism activities of the region, this region may be considered a cold spot of deforestation compared to the national average computed during the same period (1.3%, according to [13]). In the Caribbean region, mangroves have been cleared at a rate of ≈1% yr−1, but figures are greater in mainland than in insular sites (≈1.7 and 0.2% yr−1, resp. [23]).In addition to the limited information about rates and drivers of mangrove deforestation, there is a lack of understanding on how specific activities such as selective logging and mangrove reclamation have impacted forest structure, faunal diversity, and services to humans, particularly in the Neotropics. Most of the reliable current knowledge about mangrove change has been obtained by combining coastal land mapping and field surveys in Indopacific locations (e.g., [25–27]). Yet few studies have been able to make historical reconstructions [24, 25, 28, 29]. An ethnoecological approach has also proven to be useful for understanding the drivers of deforestation [6, 29–32], while ecological economics have helped to account for the costs of mangrove conversion to other uses in a few case studies (e.g., [33]). Dahdouh-Guebas and Koedam [34] proposed that a transdisciplinary approach is required in order to advance in the knowledge of complex issues such as deforestation and climate change in mangroves.The objective of this paper was to answer the following questions. (a) To what extent has deforestation impacted mangrove structure, species composition, biomass, and carbon reservoirs? (b) Does deforestation promote proliferation of invasive species such as the white mangroveLaguncularia racemosa and the mangrove fern Acrostichum aureum?, and (c) Is deforestation a driver of declines of keystone benthic fauna? As a case study, we used the Urabá Gulf (Colombian Caribbean), an ecologically important yet threatened ecoregion located in the northern part of the Biogeographic Chocó biodiversity hotspot [35, 36]. Historical information about mangrove cover and structure and detailed data obtained during a recent scientific survey were summarized. The ultimate goal of this summary was to contribute insights on the sustainability of current practices of mangrove exploitation.


## 2. The Urabá Gulf Mangroves and Deforestation

The Urabá Gulf (also known as the Darién Ecoregion) is the southernmost location of mangroves in the Caribbean basin (Figure1), where presumably well-developed and extensive mangrove stands are found, exceeding the figures observed along the Caribbean coasts of Costa Rica, Panamá, and Southern Colombia [18, 37, 38]. Mangrove development is probably boosted by the large freshwater discharge of the Atrato River (Q= 4,155 m3/s, the second largest in the Caribbean Coast of Colombia, after the Magdalena River), fed by the heavy rain of the Chocó Region, one of the world’s highest. The most extensive mangroves develop on the deltaic fan of the Atrato River, although smaller areas are found in smaller deltas. This region remained poorly explored by ecologists during most of the 20th century due to public order issues, and mangrove forest inventories were limited to specific areas of interest [35]. These early inventories evidenced that mangroves in the Urabá Gulf were dominated by the red mangrove Rhizophora mangle in most locations while Laguncularia racemosa(white mangrove) and Avicennia germinans (black mangrove) coexisted at lower relative densities. A. germinans formed nearly monospecific stands in the interior (basin) of the Eastern Coast mangroves. These structural and floristic features are more alike to the mangroves in the Pacific coast than to the Caribbean coast of Colombia, probably due to the large freshwater discharge they receive from the Atrato River.(a) Location of the Urabá Gulf in Colombia and the Caribbean region (mangrove and coastal flood plain wetlands are shown). (b) Location of mangrove areas in the Urabá Gulf: Atrato River Delta, Rionegro Cove, and the Eastern Coast (Turbo Municipality is shown). Mangrove physiographic types are indicated.
(a)
(b)Quantification of deforestation rates and land cover and land use transitions has been impeded by the lack of robust mangrove cover maps. By 2003, it was estimated that 6993 ha of mangroves existed in the Urabá Gulf using satellite images [17, 42]. The most recent inventory conducted as part of the Urabá Gulf Mangrove Expedition [35, 36] updated mangrove extent and structure using color-high-resolution aerial photographs (1 : 10,000, pixel size 30 × 30 cm) taken along a 609 km coastline, accompanied with field surveys in 79 circular 500 m2-plots during 2009 (Figure  1 and Table  1 in [39]). According to this effort, mangrove cover was estimated in 4908 ha, thus suggesting a reduction in 2085 ha (29.8%) between 2003 and 2009 (estimated annual rate: 4.9%). Although this reduction was evidently influenced by deforestation in the region, it was seemly biased by differences in the remote sensing techniques employed in both surveys. Nonetheless, there is no doubt that this region is a deforestation hotspot in the Caribbean coast of Colombia, as evidenced by the field inventory, and observed human uses (see Section 3). While mangroves located in the Atrato River Delta (3846 ha) and the Rionegro Cove (342 ha), the most extensive areas, have seemly experienced little change in extent during more than two decades, mangroves settled along the Eastern Coast (León River and Punta Coquito: 192 ha; Guadualito and Currulao rivers: 214 ha; Punta Yarumal and Turbo Bay: 145 ha; Caimán Nuevo River: 103 ha) have been dramatically shrunk due to expanding agricultural and pasture lands and urban areas, particularly near the Turbo Municipality (247 638 inhabitants). Annual population growth rate (1993–2005) in this municipality (7.2%) is threefold compared to state- and national-level figures [43]. Population density in 2005 also exceeded national-level values (52 and 41 inhab./km2, resp.). Such a population growth has been powered by the profitable banana industry comprising 50359 ha of plantations and exports scoring 55.1 millions of cases [44]. In addition, cattle ranching has been a major economic activity since the early 20th century. For this reason, coastal plain native forests (5048 ha including mangroves) have been decimated and replaced by urban (1499 ha), agriculture (67802 ha), and pasture (142385 ha) [43]. In addition, mangroves along Eastern Coast and the northeastern vicinity of Urabá Gulf have probably shrunken as a consequence of the steady coastline retreat experienced (1–50 m/yr; [45]).


## 3. Forest Structure, Species Composition,and Deforestation

Deforestation alters forest structure and species composition [13]. In the Urabá Gulf, selective logging and land reclamation, in addition to coastline erosion, have reduced mangrove area, but it has particularly altered natural patterns of forest structure and species composition. The early inventories conducted in the most pristine areas (Atrato River Delta and Rionegro Cove) revealed that self-thinning was the most evident driver of structure in red mangrove stands (r2=0.58, P<0.0001) however, a weak self-thinning effect was observed in most transformed areas due to selective logging in the Eastern Coast (r2=0.21, P<0.008, based on data from [42, 50]). Recently, Urrego et al. [39] reported on the impact of selective logging in suburban mangroves (Table 1). As a reference, R. mangle tree diameter was logarithmically skewed towards small values, with a few trees with diameter at breast height (DBH) > 30 cm, in isolated fringing mangroves (Atrato River delta, Rionegro Cove, and Puerto Cesar-Punta Coquito). In contrast, the suburban mangroves located in the vicinity of the Turbo Municipality (Punta Yarumal-Las Vacas) exhibited fewer trees than expected in the DBH 7–17 cm range, and individuals >40 cm were lacking (Figure 2). This forest also exhibited the lowest mean tree diameter and mean density (Table 1), a pattern promoted by selective logging of R. mangleand A. germinans, the species with greater importance value (IVI) in the Eastern Coast (Figure 3). Selective logging and mangrove reclamation indirectly increased the IVI of L. racemosa in suburban basin mangroves (see discussion in Section 5), in contrast to the observed in isolated mangroves (Figure 3).Table 1
Area and structure parameters (mean values) for mangroves in the Urabá Gulf. Mangrove species: Rm:Rhizophora mangle, Lr: Laguncularia racemosa, Ag: Avicennia germinans, Pr: Pelliciera rhizophorae. Modified from Urrego et al. [39].
Location
Mangrove type
Area (ha)
Diameter (cm)
Height (m)
Basal area (m2/ha)
Density (ind./ha)
Mangrove species
Atrato River Delta
Fringing
3846
17.1
7.8
26.2
494
Rm, Lr, Ag, Pr
Puerto Cesar-Punta Coquito
Fringing
406
9.0
7.6
12.5
464
Rm, Lr, Ag, Pr
Punta Yarumal-Punta Las Vacas
Fringing
48
5.6
6.7
32.2
220
Rm, Lr, Ag
Basin
98
5.4
7.3
20.7
182
Rm, Lr, Ag
Rionegro Cove
Fringing
53
10.4
13.0
11.5
324
Rm, Lr
Riverine
241
15.3
9.8
13.0
309
Rm, Lr, Ag
Early succession
50
19.2
9.5
6.0
129
RmDistribution of mangrove tree diameter at breast height in four locations and four mangrove physiographic types (modified from Urrego et al. [39]). Sampling effort (500 m2 circular plots): Atrato River Delta (n=25), Rionegro Cove (n=30), Puerto Cesar-Punta Coquito (n=10), and Punta Yarumal-Punta Las Vacas (n=19). Note that total abundance is independent of sampling effort.
(a)
(b)
(c)
(d)Importance value index (IVI) for mangrove species in four locations and four mangrove physiographic types (modified from Urrego et al. [39]).
(a)
(b)
(c)
(d)In the Urabá Gulf, selective logging has been traditionally conducted by fishermen for direct households and small-scale commerce in Turbo (Figure4). R. mangle is predominantly exploited for poles, but their commerce is poorly attractive [42], as evidenced by the piles commonly abandoned in informal markets, streets, or even in the field. On the other hand, charcoal production is a common practice, but it is time consuming and poorly rewarded, because a sack is sold at 4 USD (COP 8,000), although it requires logging and burning 20 trees (Figure 4). A. germinans trees are not commonly marketed, but they are logged on demand for construction pilings and planks (Figure 4). In addition to selective logging, basin mangroves are cleared for understory cattle ranching and for establishing pastures (Figure 4). Such practices in mangroves and coastal-plain forests are responsible for high annual deforestation rates (1.9% [51]) exceeding those observed in Colombian terrestrial forest hotspots [52].Impacts of selective logging and mangrove reclamation in the Urabá Gulf. Exploitation of mangrove wood (a–e). Mangrove reclamation for rural low-density housing (f-g). Mangrove conversion to pastures (h–j). Examples of cryptic ecological degradation (k-l).  Extraction of red mangrove (R. mangle) poles (a-b) and planks from a large black mangrove (A. germinans). Artisan ovens (d) for burning mangrove charcoal. Each sack of charcoal required felling 10–20 trees; this pile nearly exploited 200 trees, equaling one hectare from Punta Yarumal (e). Recent mangrove reclamation for rural settlement, noting the deadwood left in place (f). Reclaimed periurban mangrove showing abundant resprouting (g). Examples of mangrove clear cutting and digging desiccation drainages (H) for establishing active pastures (i); note the few standing black mangrove trees. Black mangrove stand with a cleared understory for cattle ranching (note the fencing) (j). White mangrove (Laguncularia racemosa) resprouting in a cleared area (k).  Introgression by Acrostichum aureum (l). Photos: E. A. Estrada and A. Taborda.
(a)
(b)
(c)
(d)
(e)
(f)
(g)
(h)
(i)
(j)
(k)
(l)Contrary to the observed in many places, mangroves in the Urabá Gulf are exploited for a few uses, and, in general, they are disregarded as a source of goods and services. Uses and sizes for a given mangrove species may differ from one place to another even within a single region in many parts of the world [29, 32]. Extraction of poles from R. mangletrees with DBH < 15 cm has also been reported from Venezuela [53]. Recently, as overexploitation of R. mangle has reduced the available DBH, loggers are extracting L. racemosa. It is in contrast with the observed in some areas of Mexico, where L. racemosa is preferably exploited for woody products over A. germinans and R. mangle, species that are mostly used for nonwoody products (i.e., medicine and leather dying), while no wood is burned for charcoal production [29]. Therefore, it is important to understand the objectives of selective logging to explain patterns in terms of sizes exploited, level of exploitation, degree of mechanization, and spatial distribution as influenced by access from towns and villages [6, 25, 32]. Although ethnoecological studies have been instrumental for reconstruction of past uses of mangroves and impacts derived [8, 46, 47, 54], more studies are urged for the Neotropics because a few case studies exist (e.g., Mexico: [55], Venezuela: [53]) and most of the examples concentrate in the Indopacific [6].


## 4. Estimated Biomass and Carbon Reservoirs as Influenced by Deforestation

Mangrove biomass was traditionally appreciated as a major ecosystem good, but its importance in the coastal carbon budget has been recently highlighted [10, 11, 49, 56, 57]. It is intuitively accepted that deforestation depletes aboveground carbon reservoirs. However, as stated by Bouillon et al. [10], “…information (if any) about carbon losses associated to clear-falling are [sic] difficult to obtain since this activity is illegal in most countries; actual records of total biomass extracted to use mangrove area for other purposes (e.g., roads, urban development) is also rare making it difficult to determine this component in global estimates of carbon sequestration.” In order to account for the impact of selective logging on biomass and carbon reservoirs in the vicinity of the Turbo municipality, we combined forest structure data [39] and published allometric equations [58, 59]. Fringing mangroves at the Atrato River Delta stored the greatest amount of aboveground carbon (89.3 Mg C/ha) in comparison to the Eastern Coast mangroves (Table 2). The selective logging in the suburban mangroves in the vicinity of Turbo (48.3 MgC/ha) did not significantly reduce total C storage compared to other locations. Nonetheless, the low total aboveground C reservoir in basin mangroves in Punta Las Vacas-Punta Yarumal (17.5 MgC/ha) and the relatively high proportion stored in L. racemosa (5.2 MgC/ha = 30% of total reservoir) may reflect a strong pressure by selective logging and pasture expansion. Regardless of the mangrove location, R. manglecontributed most of the carbon reservoir but in the suburban basin mangroves L. racemosa contributed a similar amount (Table 2). Therefore, selective logging seems to unbalance carbon allocation among species rather than promoting a net loss in total reservoir. In contrast to selective logging, a major impact is predicted from mangrove conversion to pasture as the entire above-ground reservoir is translocated to the ground as dead wood, in situ decomposed, and gradually washed away or emitted to the atmosphere [60].Table 2
Aboveground (area-weighed) carbon and biomass in mangroves in the Urabá Gulf. Computed from structure data from Urrego et al. [39] and allometric equations from [46, 47].
Location
Mangrove type
Mangrove species
Mean relative abundance (%)
Above-ground carbon (Mg C/ha)
Above-ground biomass (Mg/ha)
Atrato River Delta
Fringing
R. mangle
83.0
83.7
167.4
A. germinans
1.0
0.7
1.3
L. racemosa
9.5
5.0
9.9
Total
89.3
178.7
Puerto Cesar-Punta Coquito
Fringing
R. mangle
43.3
13.1
26.2
A. germinans
21.6
4.3
8.6
L. racemosa
19.9
3.5
6.9
Total
20.8
41.7
Punta Yarumal-Punta Las Vacas
Fringing
R. mangle
76.5
25.9
51.8
A. germinans
12.9
2.9
5.8
L. racemosa
10.6
2.0
4.0
Total
30.8
61.6
Basin
R. mangle
43.5
10.1
20.2
A. germinans
14.7
2.3
4.5
L. racemosa
39.5
5.2
10.4
Total
17.5
35.1
Rionegro Cove
Fringing
R. mangle
67.2
8.9
17.8
A. germinans
0.0
0.0
0.0
L. racemosa
21.3
1.7
3.4
Total
10.6
21.3
Riverine
R. mangle
86.4
20.3
40.6
A. germinans
3.4
0.5
1.1
L. racemosa
8.6
1.1
2.2
Total
21.9
43.9
Early succession
R. mangle
91.4
15.4
30.9
Total
15.4
30.9Observed above-ground carbon reservoirs in the Urabá Gulf are within the range observed in the Tropics [10, 11, 49, 56, 57]. Compared to worldwide above-ground biomass data (as a proxy of carbon storage), mangroves in the Atrato River delta represent a significantly high reservoir, but Eastern Coast mangroves lay below the average (Tables 2 and 3; [48, 49]). Therefore, conservation efforts should prevent clearing mangroves in the Atrato River delta in order to avoid releasing significant amounts of carbon to the atmosphere and to the ocean, thus negatively impacting the Gulf’s budget. Smaller reservoirs may be locally important  but seem to contribute little to the Gulf’s total budget.Table 3
Above-ground biomass for mangrove forests worldwide.
Location
Above-ground biomass (Mg/ha)
Neotropics1
Dominican Republic
195.4
Dominican Republic
349.4
Florida
56.0
Florida
72.0
Florida
22.3
Florida
56.0
Guadeloupe
47.0
Guadeloupe
56.0
Guadeloupe
99.0
Hawaii
279.0
Mexico
135.0
Mexico
120.0
Puerto Rico
62.9
Neotropics Mean
119.2
Old World tropics1
Indonesia
93.7
Malaysia
409.0
Malaysia
216.4
Sri Lanka
71.0
Sri Lanka
71.0
Thailand
158.0
Western Australia
246.7
Western Australia
45.8
Australia
711.0
Old World Mean
224.7
Pacific Islands2
Airai. Palau
225.0
Ruunuw. Yap. FSM
363.0
Pacific Islands Mean
294
D
1ata from Sherman et al. 2003 [48].
D
2ata from Kauffman et al. 2011 [49].


## 5. Selective Logging as a Driver of SpeciesIntrogressions and Extinctions

Clearing mangrove areas due to natural disturbances such as hurricanes has resulted in introgressions by fast-growing mangrove and nonmangrove species [61–65], and it is likely that selective logging and clear cutting may produce similar outcomes [46]. Moreover, the codominance of secondary mangrove species or antagonistic distributions can be indicators of cryptic ecological degradation (Dahdouh-Guebas et al. [46]). In the Urabá Gulf, we recently documented that the IVI of R. mangle and L. racemosa were inversely correlated (Figure 5), because selective logging upon the first promoted overgrowth of latter (Figure 4(k)), otherwise a secondary species, thus supporting the hypothesis of cryptic degradation. A similar proliferation of L. racemosa was observed in Panamian suburban mangroves as a consequence of reclamation [28]. No correlation was observed between the selective logging of A. germinans and the IVI of L. racemosa in basin mangroves, contrary to the observed in Belizean [64] and Puerto Rican [66] mangroves. In the surroundings of Turbo City (Punta Las Vacas), the mangrove fern Acrostichum aureum also invaded extensively cleared fringing mangroves (Figure 4(l)), and it has become a major barrier for natural recovery, as observed elsewhere [8, 25, 46, 67]. In other areas such as Punta Yarumal where mangrove trees have been selectively logged, A. aureumformed clumps in the understory. It is known that this fern proliferates in compacted, saline, and alkaline soils after mangrove clear cutting or hurricane-induced mass mortality [64, 68]. A recent study in Cispatá Lagoon System (Caribbean coast of Colombia) agreed that the high proportion of Laguncularia pollen may indicate the prevalence of anthropogenic disturbances on mangrove stands otherwise dominated by Rhizophora or Avicennia[69]. Nonetheless, Lagunculariapollen and Acrostichum spore records underscore the prevalence of human and natural disturbances in Caribbean mangroves, because pollen and spores are widespread distributed by water and air [70]. Conversely, A. aureumwas also reported naturally occurring as an understory plant in A. germinans stands in La Mancha (Gulf of Mexico [71]. Interestingly, both L. racemosa and A. aureum, otherwise mangrove intrograders, also coexisted naturally with the swamp bloodwood Pterocarpus officinalis,and other two mangrove species in coastal forests developed in very low salinities in the southern part of the Urabá Gulf (e.g., Punta Coquito-Puerto Cesar). The association Pterocarpus-Acrostichum-Lagunculariahas been well documented in Puerto Rico [66, 67].Figure 5
Negative regression betweenR. mangle and L. racemosa importance value index (IVI) in the Eastern Coast of the Urabá Gulf. Sampling point-centered quadrats are shown for five mangrove locations (outlining). Data from a master’s thesis in progress by E. A. Estrada.The basin mangrove physiognomy and the dominant species (A. germinans) are also threatened, because, in contrast to the rest of the Caribbean, only small patches exist naturally at the Eastern Coast of the Urabá Gulf. Along this coast, entire basin mangroves have been converted to pastures, thus locally decimating mangrove patches along with the dominant A. germinans (Figures 4(i) and 4(j)), similarly to the reported patch shrinking and species extinctions in periurban mangroves in Mombasa (Kenya) [47]. Finally, selective logging might be responsible for local extinction of the vulnerable mangrove species Pelliciera rhizophorae (Figure 3: Puerto Cesar-Punta Coquito and Atrato River Delta; but recently recorded in Punta Las Vacas). P. rhizophorae is found in the Caribbean only in a few locations in Colombia, contrary to its codominance along the Pacific coast of Central and South America [72–74].Extinctions and invasions in species-poor mangrove in the Neotropics are expected to bring notorious ecosystem-wide effects [75]. In addition, since specific ecosystem services are provided by particular mangrove species and physiognomies [7], the observed patterns and rates of selective logging and reclamation in the Urabá Gulf will probably produce negative feedbacks in human populations deriving direct and indirect services from mangroves.


## 6. Impacts of Selective Logging and Mangrove Reclamation on Benthic Fauna

Deforestation negatively affects benthic communities; however, there are a few accounts on the direct and indirect impacts and mechanisms. At an ecoregional scale, we observed thatLittorinopsis angulifera(Gastropoda: Littorinidae) and Neritina virginea (Gastropoda: Neritidae), two iconic species in Caribbean mangroves, lacked adults or individuals at all, respectively, in small mangrove patches seemly shrinking due to deforestation and coastal erosion, along the northern and eastern coasts of the Urabá Gulf [76]. At a landscape scale, we also reported that both selective logging and mangrove reclamation were responsible for reduced density in N. virginea (as well as in Melampus coffeus-Ellobiidae, a typical mangrove pulmonate gastropod) in Punta Yarumal in the vicinity of Turbo [40]. Selective logging promoted canopy gaps, alteration of forest structure, and sediment trampling, while mangrove conversion to pastures promoted increased soil temperature and desiccation and eliminated hard substrates (trees, prop roots, seedlings, and pneumatophores) (Figure 4, Figures 6(a), and 6(d)). Given the clumped distribution of N. virginea, the percent of sampling quadrats with snails was a reliable indicator of impact due to selective logging and of “edge effect” in the mangrove-pasture transition (Figures 6(b) and 6(c); [41]). Such reductions seemed to be primarily mediated by changes in surface sediment properties (e.g., pH, temperature, organic matter content) and microhabitat complexity (trees, prop roots, and pneumatophores). Selective logging may indirectly affect climbing gastropods (i.e., L. angulifera and M. coffeus) by eliminating their preferred habitats because they crawl on the trees during flooding tides [40, 77]. In contrast, the bottom-dwelling and numerically dominant gastropod N. virginea moves extensively along the intertidal zone covered by mangroves due to their diadromous behavior [40, 78, 79], and, therefore, selective logging and clearing promote population fragmentation because they cannot venture out of the flooded areas, particularly into the newly established pastures [40, 41]. We hypothesized that, as a consequence of N. virginea decline, sediment bioturbation and mangrove litter decomposition would be reduced. This species is a grazer and a facultative detritivore, and given its high density and biomass (range: 16–100 ind./m2; 11.9–74.3 g/m2; [40]), it seems to be responsible for the rapid processing of black mangrove (A. germinans) leaflitter (A. Taborda and J. F. Blanco in preparation). Gastropods in the Caribbean and elsewhere have been pointed as key detritivores and sediment grazers, even outweighing the role of crabs [80–82].Figure 6
Occurrence of dominant gastropods (Neritina virginea) along a mangrove-pasture transition in Punta Yarumal (Turbo River Delta). (a) Gastropod occurrence (%) relative to mangrove type and selective logging (b) and to mangrove-pasture edge (c, d). Data from  [40, 41].Available assessments on the impacts of mangrove deforestation on benthos report that vegetation provides support and physical habitat that may reduce predation and desiccation (Asia: [83, 84]; Africa: [85, 86]; Australia: [87]). For instance, clearing pneumatophores in small-scale deforestations for building walkways and trails was correlated with a decline in density and species richness in the entire community, particularly on gastropods [87]. In addition, community and population metrics, otherwise uncorrelated with physicochemical variables under natural conditions [84], became significantly explained by temperature and pH in deforested mangroves [86].


## 7. Conclusions

Selective logging and conversion to pastures have negative effects in forest structure and species composition, above-ground biomass and carbon reservoir, invasiveness, and benthic fauna in the Urabá Gulf mangroves. Mangroves settled in the Eastern Coast have been decimated, contrary to the observed in Atrato River Delta and the Rionegro Cove. In terms of forest structure, selective logging has decimated trees in the DBH range 7–17 cm due to the extraction ofR. manglepoles. A lack of A. germinanstrees of DBH > 40 cm evidenced the extraction for planks and pilings. Selective logging increased the IVI of L. racemosa, an opportunistic species, invading canopy gaps, and recently cleared mangroves. In addition to selective logging, clear cutting of basin-type mangroves is a common practice for establishing pastures, thus extracting most of tree biomass and leaving a few standing A. germinans trees. Selective logging seems to reduce total mangrove biomass and carbon, particularly in basin mangroves, but more importantly it is clearly altering allocation among species by reducing the storage in R. mangle and A. germinans and increasing the L. racemosa reservoir. Selective logging of R. mangle and clear-cutting of basin mangroves promoted introgressions by L. racemosa and the mangrove fern A. aureum in periurban sites, and they were a clear sign of cryptic ecological degradation. It is suspected that selective logging may also drive rare species such as P. rhizophorae to local extinction. Finally, selective logging and mangrove conversion to pastures were responsible for density declines of dominant gastropods (N. virginea) in mangrove canopy gaps and edges, and it is hypothesized that cascading effects may consequently occur in sediment bioturbation and leaflitter processing. Employing an interdisciplinary approach proved to be useful to demonstrate that basin mangroves are the most threatened physiognomy by deforestation due to their proximity to expanding pastures and villages. In conclusion, selective (noncommercial and unplanned) logging in Urabá Gulf mangroves, particularly in the Eastern Coast, already shows signs of unsustainability, and it is worsened by the rapid mangrove conversion to pastures.



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*Source: 958709-2012-07-31.xml*