Spatial distribution of pollen grains and spores in surface sediments of Guanabara Bay , Rio de Janeiro , Brazil

Aiming to investigate the deposition of pollen grains and spores in Guanabara Bay, Rio de Janeiro State, 61 surface sediment samples were analyzed. The results showed that the current deposition of palynomorphs in surface sediments of Guanabara Bay represents the regional vegetation of this hydrographic basin. The differential distribution of palynomorphs followed a pattern influenced by bathymetry, tidal currents speed, discharge of numerous rivers, and by human activity. The dominance of representatives of Field Vegetation reflects the changes of the original flora caused by intense human activities in the region. The continued presence and richness of pollen types of rain forest in the samples indicates that their source area might be the vegetation from riparian border of rivers in the western sector of the Bay, where the mangrove vegetation is being preserved. The large amount of damaged palynomorphs may be related to abrasion that occurs during river transport, indicating removal or reworking from their areas of origin.


INTRODUCTION
Palynological studies are important tools for interpreting the past environments and elucidating questions related to paleoclimates and paleoecology (Ybert et al. 1992, Salgado-Labouriau 2001).However, it is neces sary to understand the present environments and the dynamics that controls the deposition of pollen grains and spores before one attempts to interpret the fossil record.
The Palynological analysis of Quaternary sediments has provided important information about the past environment in the coastal region of SE Brazil.Studies have elucidated questions related to sea level oscillation and climate changes as well as to alterations of the natural vegetation as a result of intensive human activities during the Holocene (Toledo et al. 1994, Luz et al. 1999, Barth et al. 2001, 2004, Coelho et al. 1999, Santos et al. 2000).However, pollen studies on surface sediments in lakes and bays that demonstrate the patterns of modern Anais da Academia Brasileira de Ciências ( 2012) 84(3): 627-643 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 www.scielo.br/aabcCINTIA F. BARRETO, CLAUDIA G. VILELA, JOSé A. BAPTISTA-NETO and ORTRUD M. BARTH pollen deposition and vegetation of this region have not been undertaken to a significant extent.Barreto et al. (2006) presented a palynological analysis of 27 surface sediment samples of Guanabara Bay and reported that the distribution and accumulation of palynomorphs in the bay were influenced by bathymetry, velocity tide and the intensity of fluvial inputs.Studying a lake with tributaries, Luz et al. (2005) verified that fluvial influx, wind action and lakes bathymetry influenced the spatial distribution of pollen grains, spores and algae; an additional control was palynomorph size.Toledo et al. (1994) verified that the deposition of palynomorphs was influenced by the bathymetry and wind direction in a lagoon without any tributaries in the northeastern region of the state of Rio de Janeiro.
It is necessary to understand the processes that control the preservation, transport and deposition of pollen grains and spores in aquatic environment in order to obtain an accurate interpretation of pollen occurrence.The present study offers a better resolution of environmental questions related to modern ecosystems and characterizes the processes of current dynamics that control the deposition and preservation of palynomorphs in distinct sectors of the Guanabara Bay, indicating the best areas to collect sediment cores for future palynological studies.

STUDY AREA
The Guanabara Bay is located in the coastal area of Rio de Janeiro State -Southeast Brazil, between 22°40' -23°00'S of latitude and 043°00' -043°20'W of longitude (Figure 1).It lies within a depressed and elongated tectonic band of Tertiary age known as "Baixada Fluminense" or Guanabara Rift, of the halfgraben type (Ruellan 1974, Ferrari 1990, Amador 1997).Its origin is also related to climatic and sea level changes that occurred during the Quaternary and that resulted in the drowning of a Pleistocene fluvial valley (Amador and Ponzi 1974, Ireland 1987, Amador 1992, 1997, Martin et al. 1997).
The Guanabara Bay extends in the SO-NE direction, reaching a maximal width of 28 km and a perimeter of 131 km; it possesses a narrow entrance of approximately 1.6 km width.The bay surface area, excluding its islands, currently measures 372 km 2 .Its hydrographic basin covers approximately 4,600 km 2 and includes the metropolitan regions of the cities of Rio de Janeiro, Duque de Caxias, Niterói and São Gonçalo.There are 45 rivers that discharge in the bay, the Macacu and Caceribu being the most important ones (Amador 1997(Amador , kjerfve et al. 1997)).The Guanabara Bay tides are classified as semidiurnal, with one complete tidal cycle of about 12.5 hours (Amador 1997).
The bathymetry of the Guanabara Bay is influen ced mainly by the tides.The narrow entrance of the bay is occupied by a big sandy bank that extends upwards from the bay floor to a height of 12 m.This bank promotes the channelization of water flow and is also an obstacle to the tidal circulation.The central channel of the bay has a S-N orientation starting at the bay entrance until the Governador Island and accounts for the deep depths in the bay (around 30 and 40 m deep).The dominant sediments in the channel are medium to very fine sands.The innermost part of the bay (i.e., the north region) has smooth, flat bathymetry (less than 10 m) and a high sedimentation rate.Its sediments are primarily silt/clay (Amador 1992, 1997, Dias and Quaresma 1996, V.S. Quaresma, unpublished data, kjerfve et al. 1997, L.F. Catanzaro unpublished data).
The climate of the Guanabara Bay region is tropical humid with a well -defined rainy season between December and April, and a dry season between June and August (Denemet 1992).The mean annual air temperature is 23.7°C, and the mean annual relative humidity is 78%, with an annual average precipitation higher than 2,000 mm over the Serra do Mar hills, and 1,000 to 1,500 mm in the lowlands (Baixada Fluminense region) (Amador 1997).The winds most frequently blow from the east (21% of the time), south (17%) and POLLEN DISTRIBUTION SEDIMENTS OF GUANABARA BAY north (14%), with a mean velocity of 3 m/s in the Santos Dumont Airport area (kjerfve et al. 1997).

FIELD WORk
In order to examine the patterns of palynomorph deposition across different areas of the Guanabara Bay, a total of 61 surface sediment samples were collected using a "Van-Veen"collector sampler.The samples were grouped into five sectors (Vilela et al. 2003) (Figure 1).Three samples were obtained in the sector next to the bay entrance and were composed of medium to fine sand.Thirteen samples were collected in the central sector, consisting of fine sand.The Fundão Island sector comprised eight samples of silty clay and argillaceous silt sediments, while fifteen samples were collected in the western sector and were also dominated by argillaceous silt.Twenty one samples, composed of muddy sediment with a predominance of clay, were collected in the eastern sector (Catanzaro unpublished data).

LABORATORY ANALYSIS
The samples were chemically treated according to the standard methodology for Quaternary sediments proposed by Ybert et al. (1992).This includes the use of 10% of HCl for the elimination of carbonates, followed by 40% HF for elimination of silicates, then the acetolysis and heavy liquid separation using a znCL2 (density = 2).To estimate the concentration of palynomorphs per volume of sediment, two tablets of exotic Lycopodium clavatum spores (about 11,670 spores per tablet) were introduced into each sample prior to processing (Stockmarr 1971).A minimum of three slides was prepared for each sample, and at least 200 pollen grains per sample were counted at 400x magnification.
Palynomorph counts were expressed as relative abundance (percent) and concentration.The percentage calculation was based upon the total sum of pollen grains (herbs, shrubs and trees), excluding algae and fern spores.The software Tilia and Tiliagraph (Grimm 1987) were used for the statistical analysis of the palynological data.The identified palynomorphs were grouped into the respective vegetation types according to Veloso et al. (1991).
Deteriorated pollen grains and spores were analyzed according to Moore et al. (1991).

Bay entrance sector
Three samples were analyzed, and 47 pollen types from the total of 96 pollen types were identified.The pollen of Grassland predominated in two samples taken near the bay entrance (maximum of 56 % in samples U2 and U3).The lowest pollen percentage of this group was observed in the most northerly sample, St58 (31%; Figure 2).Poaceae was the most important pollen type of Grassland (55% in sample U2), and additional pollen types such as Amaranthus/Chenopodiaceae, Borreria densiflora and Chamaesyce were recorded in very low percentages (Figure 3).The highest percentage of Ombrophilous Forest pollen occurred in sample St58 (31%), and it diminished to 12% near the entrance of the bay (sample U2; Figure 2).Alchornea, Arecaceae, Casearia, Celtis, Cupania, Hedyosmum, Ilex, Lecythidaceae, Rapanea, Sebastiania and Trema were the most important of Ombrophilous Forest pollen types (Figure 3).Montane Forest pollen types were recorded in only one sample with a very low percentage (sample St58 with less than 5%; Figure 2).Pollen types of the Mangrove vegetation, as well as algae, did not appear in samples of this sector (Figure 2).Hydrophyte pollen types presented a low percentage (less than 5%), and the highest percentage of exotic genera (more than 16% in samples U3) and fern spores (sample U3 with more than 59%) was observed in this section (Figure 2).
The lowest pollen grain and spore concentration was observed in this sector, with less than 4,500 palynomorphs/g in sample St58 and less than 1,500 in samples U2 and U3 (Figure 5).

Fundão island sector
Sixty-two pollen and spore types were identified in eight samples analyzed.The dominant Grassland taxa occurred in 90% of the samples (more than 50% in sample St52; Figure 2).Poaceae presented the highest percentages (more than 25% in all samples), followed by Amaranthus/Chenopodiaceae (maximum of 9% in sample St52), Brassica (more than 5% in all samples) and Borreria densiflora and Chamaesyce (percentages usually less than 5%; Figure 3).The highest percentages of Ombrophilous Forest pollen types occurred south of the Rio-Niterói Bridge, near its western end (sample St55 with 40%; Figure 2).Arecaceae, Celtis, Lecythidaceae, Rapanea and Trema contributed to the increase of percentages of the Ombrophilous Forest pollen type in sample St55 (Figure 3).Montane Forest plant taxa of low percentage (less than 5%) were recorded CINTIA F. BARRETO, CLAUDIA G. VILELA, JOSé A. BAPTISTA-NETO and ORTRUD M. BARTH in five samples (Figure 2).Pollen types representing the Mangrove vegetation were not observed in this sector (Figure 2), and Hygrophyte pollen presented low percentages in all samples (about 5%), with some increase in sample St55 (11%; Figure 2).Exotic genera were recorded in samples near the margins of Governador and Fundão Islands (samples St52, St49, St50 and St46), and in one sample collected near Rio-Niterói Bridge (sample St56, less than 9%; Figure 2).Fern spore percentages ranged between 5 and 40% in all samples (Figure 2).
The highest concentration of pollen grains and spores was observed in samples next to the Fundão Island (samples St49 -14,500 and U7 -17,000 palynomorphs/g) and in a sample between Rio-Niterói Bridge and the Cobras Island (sample St55, more than 4,500 palynomorphs/g).The other five samples presented in general low concentration values (less than 1,000 palynomorphs/g) (Figure 4).

Central sector of the bay
Eighty-eight pollen and spore types were identified in 14 samples analyzed from this area.The Grassland taxa dominated in almost all samples (more than 50% in sample U10; Figure 2).Poaceae percentage was the greatest (more than 15% in all samples), followed by Amaranthus/ Chenopodiaceae (maximum of 9% in sample St85) and Borreria densiflora; Brassica occurred in more than 70% of these samples, with abundances usually less than 10% (Figure 3).High percentages of Ombrophilous Forest pollen occurred in samples St44, St42, St39, St84 and St31 (more than 40% in sample St31; Figure 2).Alchornea, Arecaceae, Celtis, Hedyosmum, Lecythis, Rapanea and Trema presented their highest percentages.Other Ombrophilous Forest taxa, such as Anadenanthera, Lecythidaceae and Piper, were recorded in very low percentages (less than 6%; Figure 3).Podocarpus lambertii was the most common Montane Forest pollen type, with less than 3% (Figure 3).Mangrove taxa appeared ) near the southeastern margin of the bay, close to rivers, but represented less than 1% of the pollen sum (samples St34, St85 and St84; Figure 2).Rhizophora was the most common Mangrove pollen type.Hydrophyte plants presented low percentages (1 -9%; Figure 2).The highest percentage of fern spores was recorded in a sample south of Rio-Niterói Bridge (sample St57), and a very low percentage occurred near the southeast margin (sample St84, less than 5%).Other samples frequently contained 60% spores (Figure 2).
The sediments of the main canal south of Rio-Niterói Bridge (sample St57) and eastward the Governador Island (samples St44, St43, St42, U10 and St38) showed a low concentration of pollen grains and spores (less than 11,000 palynomorphs/g).Low concentration were also observed in samples St32 and St84 (less than 10,000 pollen grains/g of sediment).An increase of pollen grain concentration was observed only in the east margin of the bay near São Gonçalo city, with more than 18,000 palynomorphs/g (Figure 4).Ninety-seven of the 129 pollen grains and spore types were identified in the 21 samples analyzed from this area.Pollen types of Grassland predominated in almost all samples (more than 35%; Figure 2).Poaceae was the most important (20% to 70%), followed by Amaranthus/Chenopodiaceae (1% to 9%), Borreria densiflora (1% to 3%) and Chamaesyce (1% to 4.5%; Figure 3).The Ombrophilous Forest vegetation taxa presented the highest richness of pollen types (53 pollen types).The highest percentage of this group occurred in the northern margin near the rivers in the APA of Guapimirim area; abundances varied between 35 and 40% in samples St4, St5, St9 and St14 (Figure 2).Alchornea, Arecaceae, Cecropia, Celtis, POLLEN DISTRIBUTION SEDIMENTS OF GUANABARA BAY Hedyosmum, Lecythidaceae, Lecythis, Phyllanthus, Rapanea and Trema occurred in more than 50% of these samples (Figure 3).Montane Forest taxa presented lower percentages (1% -6%; Figure 2).Mangrove taxa were observed in samples located near the mangrove of the APA of Guapimirim and the northern margin of the bay, but with less than 5% relative abundance in seven samples (samples St83, St3, St5, St6, St10, St11 and St14; Figure 2).Rhizophora was the most common Mangrove pollen type (less than 5%), and Cyperaceae, Scoparia and Typha were the dominant Hydrophyte pollen types, though their percentages were less than 9.5% (Figure 4).Fern spore percentages were practically in all samples (Figure 2).
Three samples in this area (samples St9, St14 and St18) presented the highest pollen grain and spore concentration observed in the Guanabara Bay.The highest pollen concentration occurred next to the river inflows in the north margin of the bay (from more than 30,000 palynomorphs/g to a maximum of 49,199 palynomorphs/g).It decreased eastwards of the Paquetá Island (less than 12,000 pollen grains/g in samples St15, St16, St17, St28, St29 and St30) and in one sample of the northeastern margin near the Itaoca Island (less than 10,000 palynomorphs/g in samples St83).In the northeastern margin, near the APA of Guapimirim, approximately 20,000 palynomorphs/g (samples St2, St3, St4, St5, St6, St7, St8, St10, St11, St12 and St131) were observed (Figure 4).

WESTERN SECTOR OF THE INNERMOST PART OF THE BAY, NORTH OF GOVERNADOR ISLAND
Fifteen samples contained 86 types of pollen and spores identified.The highest percentage of the Grassland taxa (47%) was recorded in samples reco-vered near the Governador Island (samples St23, St24 and St25; Figure 2).Poaceae (more than 25% in all samples) and Amaranthus/ Chenopodiaceae (1% to 3.5%) were the most abundant taxa of this group (Figure 3).Pollen types of the Ombrophilous Forest also occurred (more than 10% in all samples); the highest percentages were observed in samples St19 (38%), St20 (33%) and in a sample collected near the mouth of Estrela river (sample St91, 36%; Figure 2).Alchornea, Anadenanthera, Arecaceae, Celtis, Hedyosmum, Lecythidaceae, Lecythis, Rapanea and Trema occurred in more than 50% of samples (Figure 3).Montanee forest taxa occurred in samples collected near the Governador Island (samples St20, St21, St22, St24, St25 and St26) and in one sample located next to the northwest margin of the bay; the abundance in each sample was less than 5% (Figure 2).Representative pollen types of the Mangrove vegetation were not observed in these samples.Among Hygrophytes, Cyperaceae, Typha and Scrophulariaceae presented less than 5% (Figure 4).The alga Botryococcus was observed in low abundance (less than 1%) in samples St20, St25, St92, St91 and St88 (Figure 4), and fern spores presented a significantly reduced frequency (Figure 2).
Except for St87, all six out of seven samples located near the northwest margin of the bay presented a high concentration of pollen grains and spores (samples St92, St91, St90, St89, St88 and St86).In two of these samples the highest concentration of pollen was more than 24,000 pollen grains/g of sediment.In an area located north of the Governador Island, the pollen concentration of sample St21 was 25,000 pollen grains/g, and there was a significant decrease near the rocks of the Governador Island (less than 7,500 pollen grains/g, samples St23 and St24) (Figure 5).St6,St7,St10 and St11).The western sector of the bay produced samples with the highest percentage of damaged palynomorphs (samples St21 (37%) and St26 (35%)).The damage degree decreased towards the bay margin (less than 10%; Figure 6).

DISCUSSION
PALYNOLOGICAL ANALYSIS/REGIONAL VEGETATION The palynological analyses carried out in the surface sediments showed that the pollen and spores deposition represented the integration of pollen types from a large source area, which corresponds to the Atlantic Forest vegetation (located on the mountain slopes and in forest reserves) and the openland plants and results from large deforested areas by intense human activities.The large area of the Guanabara Bay drainage basin (about 4.600 km 2 ) and the existence of many fluvial influxes (more than 40) provide a pollen signal of the regional vegetation as suggested by several studies that have demonstrated the relationship between the size of the catchment and the way in which pollen records reflect vegetational cover (Jackson 1990, Sugita 1993, Stebich et al. 2005).According to Jacobson and Bradshaw (1981), in a large aquatic environment, the pollen assemblage tends to be influenced by regional elements, while the majority of pollen grains deposited in smaller basins is dominated by those originated from local elements.Bennett (1986) suggested that most pollen grains arriving at a basin are carried by current water channels than by wind, as it was observed in the present study.
Nevertheless, pollen analysis of surface sediments in the Lagoa Salgada, north of Rio de Janeiro State, showed a strong influence of the wind direction in the pollen grain deposition (Toledo et al. 1994).
Herbaceous pollen is prevalent in the Guanabara Bay pollen assemblages.Poacea was the dominant pollen type of the Grassland, followed by Brassica, Amaranthus/Chenopodiaceae, Borreria densiflora and Chamaesyce (Figure 3).Inside the Fundão Island sector, as well as in the western sector, north of the Governador Island, the dominance of Grassland taxa was observed in 90% of the samples analyzed.This reflects the modern vegetation along the island (Fundão and Governador) margins.These plants were observed mainly in degraded areas of the bay and in river margins as well (Radambrasil 1983, Veloso et al. 1991, Amador 1997) (Figure 3).The northwest area of the Guanabara Bay is considered the most degraded area, receiving discharges from the most the polluted rivers of the bay (Baptista Neto et al. 2006), and presenting the lowest pollen grain input.
The largest enrichment and high values of the regional pollen types from the Ombrophilous Forest vegetation were observed mainly in sediments close POLLEN DISTRIBUTION SEDIMENTS OF GUANABARA BAY to the rivers from the APA of Guapimirim (eastern sector of the bay) and in the northern bay margin.In the western sector of the innermost part of the bay, north of the Governador Island, the Ombrophilous Forest pollen types also occurred (more than 10% in all samples); Alchornea, Anadenathera, Arecaceae, Celtis, Hedyosmum, Lecythidaceae, Lecythis, Rapanea and Trema were the most important ones.In accordance to Veloso et al. (1991), Alchornea, Arecaceae, Celtis, Hedyosmum, Meliaceae and Trema are significant trees of the Ombrophilous Forest vegetation growing in the low landscapes of Rio do Janeiro State.
Podocarpus lambertii, a species of the Montane Forest, was best represented at unique sample close to the northwestern margin of the bay (Figure 3).In accordance to Veloso et al. (1991) andRadambrasil (1983), this pollen type characterizes the vegetation of the Ombrophilous Dense Montane Forest located in the mountain hillsides.
Cyperaceae, Scrophulariaceae and Typha were the most important Hydrophyte pollen types.The increase of their percentages in samples near the APA of Guapimirim (Figure 4) may be associated to plants from flooded margins of rivers discharging into this sector of the bay (Araújo and Maciel 1979).The mangrove taxa recorded only in the samples of the southern bay margin in the central and eastern sector of the innermost part of the bay can be associated mainly with the proximity of the mangrove of the APA of Guapimirim.Rhizophora was the most common mangrove pollen type and a high pollen producer, while Avicennia is a low pollen producer, considering that Rhizophora is wind pollinated whereas Avicennia is insect pollinated.According to Jackson (1990), pollen grains dispersed by animals tend to be deposited next to the plant source and are not adapted to dispersion by the wind.Barreto et al. (2007) and Barth et al. (2004) studied Holocene sediments of a core located next to the Island of Paquetá (from about 8 km of the Guapimirim mangrove forest), where the presence of pollen types indicating mangrove in the sediment level of 4.210 years A.P. ago was not recorded.By analyzing a sediment core collected in the northeast portion of the bay next to the APA of Guapimirim, São-Thiago (2005) evidenced a composed floristic scenery for a dense mangrove and river bordering forest vegetation of the domain of Tropical Rainforest.
The largest percentages of exotic genera were observed mainly within the sector of the Bay entrance and in the Fundão Island.These regions were highly impacted by human activities.The Pinus pollen, which is an exotic genera, was more common, since it was used for the reforestation of the same areas of the Guanabara Bay highlighting the human activities in the region (Veloso et al. 1991) (Figure 4).Fern spores concentration was practically constant in all samples of this sector (Figure 5).The presence of Botryococcus (Algae) indicates the proximity of a freshwater source (Guy-Ohlson 1992) ( Figure 4).
The obtained pollen data represented very well the regional vegetation, and different pollen assemblages were observed in different bay sectors.Therefore, it was necessary to analyze separately each sector in order to a better understanding of the pattern distribution of palynomorphs in the bay sediments.

SPATIAL DISTRIBUTION OF POLLEN GRAINS AND SPORES
The variability of the pollen spectra in the sediments of different sectors of the Guanabara Bay reflects the hydrodynamic and bathymetryc characteristics and changes in the vegetation surrounding the bay (Sugita 1993, Traverse 1994, DeBusk 1997).The pollen spectra of samples from the bay entrance sector presented the lowest pollen grain and spore concentration (Figure 5).This may be explained by the increase of the tidal water speed due mainly to the narrow bay entrance and its bathymetry that does not the palynomorphs deposition, and induce its transport into the most internal sectors, in the S-N direction.The greatest values of tide speed CINTIA F. BARRETO, CLAUDIA G. VILELA, JOSé A. BAPTISTA-NETO and ORTRUD M. BARTH occur in this sector, near the Gragoatá Fort and the Santos Dumont Airport (kjerfve et al. 1997).
A low increase in the concentration values of pollen grains and spores was observed in samples taken next to the Fundão Island (samples St49 and U7) and in a sample between Rio-Niterói Bridge and the Cobras Island (Figure 5).It was due mainly to the low current energy in this area.The geomorphologic strait in the northwest portion of the Governador Island contributed to an increase in the tide current speed, even when dominated by low energy (Amador 1997).It possibly promoted the remobilization of palynomorphs previously deposited in other areas of this sector.According to Wilmshurst and McGlone (2005), lake sediment sources can include the inwash of secondary pollen and spores of mixed ages from eroded soils, river bank sediments and littoral sediments, as well as contemporaneous pollen and spores from aerial deposition, rain-out, surface runoff and inwash of debris from the catchment.The low concentration values of palynomorphs in these samples was related to the poorly covered areas of vegetation of the Governador and Fundão Islands, and next to Praça XV, which is highly impacted by the urban development.
The current intensity and deep depth in the main channel south of Rio-Niterói Bridge (sample St57) and east of the Governador Island (samples St44, St43, St42, U10 and St38) may be responsible for the low concentration of pollen and spores (Figure 5).The intensity of the current in the main channel of the bay decreases the accumulation of pollens in this sector, and allow the deposition of pollens in others areas of the bay.In these sectors an increase of pollen grain concentration was observed only in the east bay margin near to São Gonçalo city, where water current speed was reduced by the widening of the bay in alignment with Santos Dumont Airport -Gragoatá rocky coastal area (JICA 1994).
In the eastern sector of the innermost part of the bay, three samples presented the highest pollen and spore concentrations observed in the Guanabara Bay, with the maximal pollen concentration occurring next to the river mouths at the north margin of the bay (Figure 5).The ease of palynomorphs deposition in this area can be associated to the low energy level of water flows and the flat bathymetry, which result in mud sedimentation with the predominance of clay (kjerfve et al. 1997, Amador 1997, L.F. Catanzaro, unpublished data).With the exception of sample St87, all six samples located near the northwest margin of the bay presented high concentrations of pollen and spores.This may be associated to the low water energy and the flat bathymetry (Kjerfve et al. 1997, Amador 1997, L.F. Catanzaro, unpublished data).Numerous tributaries discharge into this sector, and contribute to the strong deposition of pollen grains and spores.

DIFFERENTIAL PRESERVATION OF PALYNOMORPHS
Pollen grains and spores preservation was generally excellent in surface sediment samples of the bay.An abundance of damages observed may be related to collisions occurring during the fluvial transport of palynomorphs, which indicates a removal from its source area (Tyson 1995).In accordance to Campbell (1991), pollen grains and spores damaged by erosion were found in many sedimentary basins and can be interpreted as a result of a new deposition after a period of exposition to the air, including cycles of humid and dry climates.
A high level of deterioration recorded in one sample located in the bay entrance, between Boa Viagem Beach and Santos Dumont Airport (sample U3), may be due mainly to the high energy of transport of different types of sediment, causing the rupture of pollen and spore exines.The geomorphology at northwest of the Governador Island contributes to an increase in the current speed of tides, promoting the remobilization of palynomorphs previously deposited in other areas of this sector.This fact may explain the high percentage of palynomorphs exhibiting damages observed in sample St54.On the other hand, in the POLLEN DISTRIBUTION SEDIMENTS OF GUANABARA BAY sector of the main channel, the highest percentages of deterioration were observed in samples St57 and St39.The increase of deposition of corroded pollen grains and spores was observed in samples St37, St39 and St33, indicating the exposition to the air.Following Wilmshurst and McGlone (2005), the process of corrosion must therefore occur some time after the pollen grains and spores were released from the source vegetation.In the eastern sector, in most parts of the bay, the high percentage of corroded palynomorphs observed in samples St5, St6, St7, St10 and St11 may be related to an intense action of microorganisms present in the mangrove.In the innermost samples of the eastern region in the bay, the maximal percentage of mechanical damages appeared in samples St21 and St26, decreasing towards the bay entrance.This pattern may be due to both tide currents and river inflows (Figure 6).

CONCLUSION
In summary, the patterns of modern pollen deposition in the Guanabara Bay surface sediments represent the regional vegetation of this hydrographic basin.Irregular spatial distribution of palynomorphs is related to the bay bathimery, the tide currents, the inflow of numerous rivers and human perturbation.The dominance of grassland taxa reflects the wideranging areas of human occupation.The presence of Ombrophylous Forest pollen grains in all analyzed samples should confirm the presence of forest segments in the low-lands, as well as the hillside and Montane Forest preservation.The damaged pollen grains and spores may be related to abrasion occurring during their fluvial transport, indicating removal and reworking from their source areas.
The present results also contribute to a predictive model for the core samples analysis, improving comparison of Recent and Holocene results, which are very important for the environment monitoring of the Guanabara bay.Palavras-chave: palinomorfos, sedimentos superficiais, deposição, preservação, Baía de Guanabara, Brasil.

Figure 1 -
Figure 1 -Map of the study area showing the location of the surface sediment samples and the different sectors of the Guanabara Bay (Vilela et al. 2003).
EASTERN SECTOR OF THE INNERMOST PART OF THE BAY, IN THE VICINITY REGION OF PAQUETÁ ISLAND AND IN THE APA OF GUAPIMIRIM

Figure 2 -Figure 3 -Figure 4 -
Figure 2 -Percentage palynodiagram of the ecological groups recognized in the surface sediment samples of the Guanabara Bay.

Figure 5 -Figure 6 -
Figure 5 -Map of total concentration of palynomorphs/g observed in surface sediment samples of the Guanabara Bay.