Marine Macroalgal Diversity Assessment of Saba Bank, Netherlands Antilles

Similar documents
The Effects of the 2004 Tsunami on the Seaweed and Seagrass Community at. Talibong Island and Nearby Trang province, Thailand

BENTHIC MARINE ALGAE FROM MARTINIQUE (LESSER ANTILLES)

Spatial patterns and response to wave exposure of shallow water algal assemblages across the Canarian Archipelago: a multi-scaled approach

Edwin A. Hernández-Delgado*

Relatively little hard substrate occurs naturally in the

Philip Kramer and Barbie Bischof

What creates a coral reef? Why are corals able to form huge reefs?

Earth / Environmental Science. Ch. 14 THE OCEAN FLOOR

Small area of the ocean that is partially surrounded by land. The Ocean Basins. Three Major Oceans. Three Major Oceans. What is a SEA?

SEASONALITY AND SPECIES COMPOSITION IN THE BENTHIC ALGAE OF CACIQUE REEF FLAT, CARIBBEAN COAST OF PANAMA

4 Marine Biology Notes. Multi-cellular Primary Producers: Seaweeds and Plants

Dynamics of shelf edge coral reef-associated macroalgae at La Parguera, Puerto Rico

Ecological mapping using satellite imagery: an Abu Dhabi case study Middle East Geospatial Forum 16 th February 2015

Bathymetry Measures the vertical distance from the ocean surface to mountains, valleys, plains, and other sea floor features

The United States & Canada. A Regional Study of Anglo America

Map Elements & The 5 Oceans

Chapter Overview. Bathymetry. Measuring Bathymetry. Measuring Bathymetry

Environmental Science

SW Florida Escarpment Mapping Area

Map shows 3 main features of ocean floor

ABSTRACT INTRODUCTION

CHAPTER IV THE RELATIONSHIP BETWEEN OCEANOGRAPHY AND METEOROLOGY

III. Acropora coral habitat distribution

Part II: Species and species groups. Chapter 7. Vulnerability of macroalgae of the Great Barrier Reef to climate change

Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore

CHAPTER 6 & 7 VOCABULARY

Objectives: Describe the structure of the ocean floor. Describe light intensity and temperature characteristics at different ocean depths.

Project 1.3.1: Improved knowledge of biota, habitats and risks. Project Leader: Dr Mick Haywood, CSIRO Division of Marine and Atmospheric Research

Name: Date: Class: Louisiana: Our History, Our Home Chapter 1: Louisiana s Geography - Section 2: Natural Regions Guided Reading

CLASSIC BOOKS OF OCEANOGRAPHY AND MARINE BIOLOGY: AN ANNOTATED BIBLIOGRAPHY. I. MARINE BOTANY

Because of the rapid degradation of tropical reefs worldwide, it is imperative that

National Marine Sanctuary Program

MODERN SEDIMENTARY ENVIRONMENTS, TWIN CAYS, BELIZE, CENTRAL AMERICA

Significant Ecological Marine Area Assessment Sheet

Seasonality in Algal Assemblages on Upwelling-influenced Coral Reefs in the Colombian Caribbean 1

The Economics of Ecosystems and Biodiversity on Bonaire. The value of citizens in the Netherlands for nature in the Caribbean

Won t you be my urchin? Featured scientist: Sarah W. Davies from University of Texas at Austin

FINMARINET: Inventories and Planning for the Marine Natura 2000 Network in Finland. A.2 Geological inventories of the seafloor Final Report

The Ocean Floor Chapter 14. Essentials of Geology, 8e. Stan Hatfield and Ken Pinzke Southwestern Illinois College

Marine biodiversity - PBBT102

Brief report on Belize carbonate environments field trip Feb. 2012

Geography 3202 Unit 4 S.C.O. 4.3 & 4.5. Primary Resource Activities Offshore Oil And Gas

NOAA Nautical Charts and Coastal and Marine Spatial Planning. Meredith Westington Chief Geographer NOAA/NOS/Office of Coast Survey

Name/ Affiliation: Ben Enticknap, Fishery Project Coordinator Alaska Marine Conservation Council Address: PO Box Anchorage, AK 99510

Marine Ecology Pacing Guide

An international research expedition assess the biodiversity and health of New Caledonia coral reefs

Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore

Adaptive Bathymetric System Mapping of Champagne Reef and Scott s Head

Biogeographic Approach to Coastal Assessments & Spatial Planning

3. The diagram below shows how scientists think some of Earth's continents were joined together in the geologic past.

Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore

Lab #5 Multicellular Marine Primary Producers. Part 1: Photosynthesis and Photosynthetic Pigments

M11/3/GEOGR/HP2/ENG/TZ0/XX/Q GEOGRAPHY HIGHER LEVEL PAPER 2. Friday 6 May 2011 (morning) 2 hours INSTRUCTIONS TO CANDIDATES

SEMESTER AT SEA COURSE SYLLABUS. Introduction to Oceanography

Earth s Continents and Seafloors. GEOL100 Physical Geology Ray Rector - Instructor

MARINE GEOLOGY & GEOGRAPHY

Marine Spatial Planning: A Tool for Implementing Ecosystem-Based Management

Remote Sensing of Episodic Rainfall Events Affecting Coral Reefs in Southwestern Puerto Rico

Coral reef degradation is not associated with local human population density

Lecture Outlines PowerPoint. Chapter 13 Earth Science 11e Tarbuck/Lutgens

8th Geography Pre-Test

Guided Reading Activity

Treasure Coast Science Scope and Sequence

Satellite Remote Sensing for Ocean

TAKE HOME EXAM 8R - Geology

Essential Question: How are the geological features that exist on land similar to the geological features on the ocean floor?

REVIEW OF ALTERNATE BALLAST WATER EXCHANGE ZONES FOR VESSEL TRAFFIC TO NEWFOUNDLAND AND LABRADOR AND THE CANADIAN ARCTIC

Ocean Floor. Continental Margins. Divided into 3 major regions. Continental Margins. Ocean Basins. Mid-Ocean Ridges. Include:

Agenda Item F.4.c Supplemental Public Comment 3 November 2016

M14/3/GEOGR/SP2/ENG/TZ0/XX/Q GEOGRAPHY STANDARD LEVEL PAPER 2. Monday 19 May 2014 (morning) 1 hour 20 minutes INSTRUCTIONS TO CANDIDATES

Marine Spatial Planning Leslie-Ann McGee Battelle Memorial Institute

IV. Distribution and Abundance of Acropora Corals

DIVERSITY ASSESSMENT ON MALAYSIAN BENTHIC MACROALGAE IN TIOMAN ISLAND AND TULAI CANDANG ISLAND, PAHANG

Background Information

MAINTENANCE DREDGE BENTHIC ASSESSMENT SUNSET POINT FARM LLC LONG POINT KEY MONROE COUNTY, FLORIDA. Prepared by:


Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa

"The Relationship Between Seagrass Cover and Species- richness of Invertebrates"

ARE YOU READY TO THINK? Look at the first slide THINK PAIR SHARE!

OCEANOGRAPHY. 13. Biological Productivity and Energy Transfer. Alessandro Grippo, Ph.D. part 2: Photosynthetic Marine Organisms

Why Do We Live Here? : A Historical Geographical Study of La Tabatiere, Quebec North Shore

Seagrass and algal abundance in the Whitsundays region. Status Report

Seabed knowledge In support of UN SDGs

Physical Geography: Patterns, Processes, and Interactions, Grade 11, University/College Expectations

CLIMAR-III Third JCOMM Workshop on Advances in Marine Climatology 6-9 May Gdynia, Poland

Most people used to live like this

Unit 7.2 W.E.D. & Topography Test

Protists: Algae Lecture 5 Spring Protist Phylogeny. Meet the algae. Primary & Secondary Endosymbiosis. Endosymbiosis. Secondary Endosymbiosis

Protists: Algae Lecture 5 Spring 2014

Economic Valuation of Goods and Services Derived from Coral Reefs. Results from the Tobago Cays Marine Park Reeffix Exercise

Unit 4 - Water. Earth s Interior. Earth s Interior. Continental Drift. Continental Drift. Continental Drift. Crust. Mantle. Core.

PLATE TECTONICS THEORY

Biological survey of species diversity of sea grass beds in selected sites of southern Sri-Lanka.

Topic 5: The Dynamic Crust (workbook p ) Evidence that Earth s crust has shifted and changed in both the past and the present is shown by:

MARINE GEOLOGY & GEOGRAPHY

GEOLOGY MEDIA SUITE Chapter 5

Coral Reef Algae. 1 Importance of Coral Reef Algae. Peggy Fong and Valerie J. Paul

Marine Science and Oceanography

Elementary Social Studies Content Area Assessment Task. Winter 2010 EDUC 203

Economic Valuation of the Montego Bay Marine Park

Transcription:

Marine Macroalgal Diversity Assessment of Saba Bank, Netherlands Antilles Mark M. Littler*, Diane S. Littler, Barrett L. Brooks Department of Botany, Smithsonian Institution, Washington, D. C., United States of America Abstract Background: Located in the Dutch Windward Islands, Saba Bank is a flat-topped seamount (20 45 m deep in the shallower regions). The primary goals of the survey were to improve knowledge of biodiversity for one of the world s most significant, but little-known, seamounts and to increase basic data and analyses to promote the development of an improved management plan. Methodology/Principal Findings: Our team of three divers used scuba to collect algal samples to depths of 50 m at 17 dive sites. Over 360 macrophyte specimens (12 putative new species) were collected, more than 1,000 photographs were taken in truly exceptional habitats, and three astonishing new seaweed community types were discovered. These included: (1) Field of Greens (N 17u30.6209, W 63u27.7079) dominated by green seaweeds as well as some filamentous reds, (2) Brown Town (N 17u28.0279, W 63u14.9449) dominated by large brown algae, and (3) Seaweed City (N 17u26.4859, W 63u16.8509) with a diversity of spectacular fleshy red algae. Conclusions/Significance: Dives to 30 m in the more two-dimensional interior habitats revealed particularly robust specimens of algae typical of shallower seagrass beds, but here in the total absence of any seagrasses (seagrasses generally do not grow below 20 m). Our preliminary estimate of the number of total seaweed species on Saba Bank ranges from a minimum of 150 to 200. Few filamentous and thin sheet forms indicative of stressed or physically disturbed environments were observed. A more precise number still awaits further microscopic and molecular examinations in the laboratory. The expedition, while intensive, has only scratched the surface of this unique submerged seamount/atoll. Citation: Littler MM, Littler DS, Brooks BL (2010) Marine Macroalgal Diversity Assessment of Saba Bank, Netherlands Antilles. PLoS ONE 5(5): e10677. doi:10.1371/ journal.pone.0010677 Editor: Stuart A. Sandin, University of California San Diego, United States of America Received May 6, 2009; Accepted January 24, 2010; Published May 21, 2010 This is an open-access article distributed under the terms of the Creative Commons Public Domain declaration which stipulates that, once placed in the public domain, this work may be freely reproduced, distributed, transmitted, modified, built upon, or otherwise used by anyone for any lawful purpose. Funding: Financial support for this study came from the Department of Environment and Nature of the Netherlands Antilles, Conservation International and the Smithsonian Marine Station at Ft. Pierce (SMSFP Contribution No. 810). The funding sources provided critical assistance in determining dive site locations but had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript. Competing Interests: The authors have declared that no competing interests exist. * E-mail: littlerm@si.edu Introduction Located in the Dutch Windward Islands about 250 km SE of Puerto Rico, Saba Bank is a flat-topped seamount rising 1.8 km from the surrounding sea floor (Figure 1). The dimensions of the Bank are extremely large for an atoll/seamount; the platform above the 200 m isobath is 65 km in length by 40 km in breadth, and it covers an area of 2,200 km 2. A large portion of the Bank (about 225 km 2 in area) lies between 12 and 20 m in depth and contains a rich assemblage of biota in varied habitats; most of the remainder of the summit is between 20 and 50 m in depth and remains virtually unexplored. Saba Bank meets the true definition of a seamount being isolated by deep water; in this case the nearest islands are Saba and St. Eustatius. Except for the fact that it does not break the water surface, Saba Bank is a classic atoll consisting of a submerged mountain crowned at the summit with a ring of actively growing coral reefs. Saba Bank is the largest atoll in the Atlantic Ocean Basin and one of the three largest atolls on earth [1]. Because of its distance from large land masses, Saba Bank is relatively free of the problems that are degrading many Caribbean reef systems, mainly sedimentary run off from poor farming practices or rapid construction, increased nutrient loading from an ever-increasing human population, and overfishing by local fisherman. There is little room for agriculture on Saba Island s five square miles; the,1,500 residents rely mainly on income from tourists that come to scuba dive. The fishing community also generates a significant income from fishing nearby Saba Bank. However, Saba Bank is threatened by the oil trans-shipment depot on nearby St. Eustatius Island. Supertankers stop there to transfer oil to tanks used to fill smaller ships that are able to enter countries without deep-water ports. Rather than pay mooring fees at St. Eustatius, tankers drop anchor on Saba Bank at no monetary cost (but often with detrimental biological damage). The immediate concerns for the Bank includes anchor damage, prop blast, and abrasion by large oil tankers maneuvering off the petroleum trans-shipment facilities on St. Eustatius, petroleum spillage and subsequent use of dispersants, possible overfishing for certain species, and exploration for petroleum reserves (so far unsuccessful). At the same time, the Bank s fisheries and dive operations are economically significant to the small community on Saba Island (about 1,500 residents) that has direct responsibility for its management. Although it ranks among the major topographic structures of the Caribbean, Saba Bank is one of the most poorly known. A PLoS ONE www.plosone.org 1 May 2010 Volume 5 Issue 5 e10677

Figure 1. Saba Bank. Bathymetric chart of Saba Bank in relation to Caribbean islands, showing the 17 collecting locations with the unique algal sites labeled as Field of Greens, Brown Town and Seaweed City. doi:10.1371/journal.pone.0010677.g001 series of interpretations of its structure and origin [2-4] has culminated in the view that the Bank essentially duplicates the atolls of the Pacific [5]. Small samples of fishes and possibly other organisms have been collected by passing research vessels (the R/ V Oregon in 1968 and 1969 and the R/V Pillsbury in 1969), and Macintyre and others carried out a preliminary survey in 1970 [6]. A Dutch expedition in 1974 utilized echo soundings, bottom sampling, and scuba to characterize the reef communities [5]. The hydrographic research vessel HNMNS Tydeman carried out a survey of the seafloor in 1996, which resulted in the current nautical charts. More recently in a post-hurricane rapid assessment, three sites on Saba Bank s eastern edge showed [7] average macroalgal biomass to be inversely related to that of herbivorous fishes., with turf algae and crustose coralline algae relatively more abundant (8 and 11 times more, respectively). Saba Bank was the focus of a joint program initiated by the Department of Environment and Nature of the Netherlands Antilles, Conservation International, and the Protocol for Specially Protected Areas and Wildlife (SPAW) of the Convention for the protection and development of the marine environment in the Wider Caribbean (Cartagena Convention), of the Caribbean Regional Seas Program under the United Nations Environmental Program (UNEP). The primary goals of the survey were to: improve knowledge of biodiversity for one of the world s most significant coral/algal-capped seamounts; increase basic information in support of improved management; provide data and analyses to support the development of a marine zoning plan; and contribute to a petition to the International Maritime Organization to designate appropriate parts of Saba Bank as Particularly Sensitive Areas. Much of the paucity of data stems from difficulties in logistics and hazardous sea conditions characteristic of Saba Banks. On some days, the small marine park patrol boats and fishing boat struggled more than 56 km to designated preselected dive sites in 4-m seas. Results Three hundred sixty specimens of macrophytes were collected by our team. Many of these include numerous other archived but uncounted species of epiphytes and smaller microscopic taxa. Our preliminary estimate of the number of macrophyte species collected from Saba Bank ranges upward from 150 to 200. A more precise number awaits long hours of microscopic and molecular examinations in the laboratory. However, the present annotated checklist of 98 taxa (Table 1) includes 43 Rhodophyta, 26 Chlorophyta, 26 Phaeophyceae, and 3 Cyanophyta (Cyanobacteria). The species accrual curve for these collections (Figure 2) [8] was steadily inclined after the 17 dive sites (Table 2), and showed no clear asymptote, indicating Saba Bank has many more species to be collected. It is important to note that there were few filamentous and thin sheet forms indicative of stressed or physically disturbed environments observed [9,10]. Three sites surveyed were dominated by previously unknown unique algal communities. These included: (1) Field of Greens PLoS ONE www.plosone.org 2 May 2010 Volume 5 Issue 5 e10677

Table 1. Annotated list of algae identified from Saba Bank arranged by major groups. Table 1. Cont. Bluegreens (Cyanobacteria) Species name Collection # Lyngbya polychroa (Meneghini) Rabenhorst D&ML 67418 Phormidium cf. dimorphum Lemmerman D&ML 67417 Symploca hydnoides (Harvey) Kützing D&ML 67420 Browns (Phaeophyceae) Species name Collection # Dictyopteris justii JV Lamouroux D&ML 67488 Dictyota cf. ciliolata Sonder ex Kützing D&ML 67439 Dictyota ciliolata Sonder ex Kützing D&ML 67451 Dictyota crispata JV Lamouroux D&ML 67500 Dictyota guineensis (Kützing) P & H Crouan D&ML 67491 Dictyota hamifera Setchell D&ML 67419 Dictyota humifusa Hörnig, Schnetter &Coppejans D&ML 67250 Dictyota menstrualis (Hoyt) Schnetter, Hörning & D&ML 67475 Weber-Peukert Dictyota mertensii (Martius) Kützing D&ML 67452 Dictyota pinnatifida Kützing D&ML 67300 Lobophora variegata (JV Lamouroux) Womersley ex Oliveira D&ML 67241 Sargassum hystrix J Agardh D&ML 67296 Sargassum platycarpum Montagne D&ML 67411 Sargassum polyceratium? Montagne D&ML 67454 Stypopodium zonale (JV Lamour.) Papenfuss D&ML 67414 Zonaria tournefortii (JV Lamour.) Montagne D&ML 67350 Greens (Chlorophyta) Species name Collection # Avrainvillea asarifolia Børgesen D&ML 67302 Caulerpa cupressoides (Vahl) C Agardh D&ML 67569 Caulerpa mexicana Sonder ex Kützing D&ML 67530 Caulerpa microphysa (Weber-van Bosse) J Feldmann D&ML 67499 Caulerpa prolifera (Forsskål) JV Lamour D&ML 67576 Caulerpa racemosa f. lamourouxii (Turner) Weber-van Bosse D&ML 67504 Caulerpa serrulata (Forsskål) J Agardh D&ML 67379 Caulerpa webbiana Montagne D&ML 67387 Codium taylorii PC Silva D&ML 67490 Dictyosphaeria cavernosa (Forsskål) Børgesen D&ML 67492 Halimeda cf. tuna f. platydisca (Decaisne) ES Barton D&ML 67274 Halimeda discoidea Decaisne D&ML 67460 Halimeda goreaui WR Taylor D&ML 67272 Neomeris annulata Dickie D&ML 67507a Neomeris mucosa MA Howe D&ML 67507b Penicillus capitatus Lamarck D&ML 67571 Penicillus dumetosus (JV Lamour.) Blainville D&ML 67529 Rhipocephalus phoenix (J Ellis & Solander) Kützing D&ML 67512 Udotea cyathiformis D&ML 67359 Udotea dotyi DS Littler & MM Littler D&ML 67575 Udotea occidentalis? A Gepp & ES Gepp D&ML 67573 Udotea spinulosa MA Howe D&ML 67574 Valonia macrophysa Kützing D&ML 67509 Reds (Rhodophyta) Species name Collection # Amphiroa tribulus (J Ellis & Solander) JV Lamouroux D&ML 67422 Asteromenia peltata (WR Taylor) Huisman & A Millar D&ML 67428 Champia parvula (C Agardh) Harvey D&ML 67331 Champia salicornioides Harvey D&ML 67342 Chondria dasyphylla (Woodward) C Agardh D&ML 67503 Chondrophycus corallopsis (Montagne) Nam D&ML 67566 Chrysymenia dickieana J Agardh D&ML 67541 Chrysymenia enteromorpha Harvey D&ML 67338 Cryptonemia crenulata (J Agardh) J Agardh D&ML 67511 Dasya antillarum (MA Howe) AJK Millar D&ML 67548 Dasya baillouviana (SG Gmelin) Montagne D&ML 67567 Dasya collinsiana MA Howe D&ML 67352 Dasya crouaniana J Agardh no number Dasya harveyi Ashmead ex Harvey D&ML 67542 Dasya mollis Harvey D&ML 67553 Dasya punicea (Zanardini) Meneghini ex Zanardini D&ML 67326 Dudresnaya bermudensis Setchell D&ML 67400 Eucheuma isiforme (C Agardh) J Agardh D&ML 67324 Galaxaura rugosa (J Ellis & Solander) JV Lamouroux D&ML 67423 Gelidiopsis intricata (C Agardh) Vickers D&ML 67510 Gracilaria cervicornis (Turner) J Agardh D&ML 67514 Gracilaria cylindrica Börgesen D&ML 67317 Griffithsia schousboei Montagne D&ML 67534 Halymenia floresii (Clemente y Rubio) C Agardh D&ML 67543 Hypoglossum hypoglossoides (Stackhouse) Collins & Hervey D&ML 67535 Jania capillacea Harvey D&ML 67501 Laurencia chondrioides Börgesen D&ML 67318 Laurencia intricata JV Lamouroux D&ML 67421 Laurencia lata MA Howe & WR Taylor D&ML 67539 Meristiella schramiai (Crouan & Crouan) Cheney & Gabrielson D&ML 67497 Neogoniolithon spectabile (Foslie) Setchell & Mason D&ML 67405 Peyssonnelia conchicola Piccone & Grunow D&ML 67517 Porolithon pachydermum (Foslie) Foslie no number Scinaia halliae (Setchell) Huisman D&ML 67537 Tricleocarpa fragilis (Linnaeus) Huisman & Townsend D&ML 67489 Wrangelia penicillata (C Agardh) C Agardh D&ML 67288 Wrightiella blodgettii (Harvey) F Schmitz D&ML 67322 doi:10.1371/journal.pone.0010677.t001 (N 17u30.6209, W 63u27.7079) characterized by an abundance by green seaweeds (Chlorophyta, Figure 3) as well as some filamentous reds, (2) Brown Town (N 17u28.0279, W 63u14.9449) dominated by large brown algae (Phaeophyceae, Figure 4), and (3) Seaweed City (N 17u26.4859, W 63u16.8509) with a diversity of spectacular fleshy red algae (Rhodophyta, Figures 5 and 6). Possibly 12 new species of brown algae (Figure 7) may be named following further scientific investigation. All of these macroalgae and their collection locations can be viewed as a virtual herbarium [11], where users can search for any combination of phylum, family, genus, species, infra-specific rank, PLoS ONE www.plosone.org 3 May 2010 Volume 5 Issue 5 e10677

Figure 2. Species accrual curve for algae on Saba Bank. Several undetermined species (spp.) not included in the check list were used in this graph. Sample based rarefaction curve shown in black is based on 17 dive sites. The Mau Tao estimator [8] of expected richness with 95% confidence intervals shown in blue. The curve reaches no asymptote, indicating a likelihood that many additional algal species remain to be found. doi:10.1371/journal.pone.0010677.g002 Table 2. Listing of site data. Site# Date Site Name Latitude Longitude Depth m 1 4-Jan-06 Poison Bank (Northeast Reef) 17u 28.756N 63u 13.600W 20-27 2 5-Jan-06 Small Bank South 17u 26.827N 63u 54.057W 37-42 3 5-Jan-06 Rhodolith Reef (middle area) 17u 25.832N 63u 40.962W 38 4 6-Jan-06 Redman Bulge 3 (Overall Bank) 17u 24.599N 63u 11.802W 35 5 6-Jan-06 Seaweed City 17u 26.485N 63u 16.850W 24 6 7-Jan-06 Grouper Bank 17u 33.085N 63u 28.847W 36 7 7-Jan-06 Rendezvous Hill 17u 34.873N 63u 24.450W 23 8 8-Jan-06 Butterfly Reef 17u 14.083N 63u 26.996W 22-37 9 9-Jan-06 Moonfish Bank (Fishpot Surprise) 17u 33.774N 63u 17.897W 19 10 10-Jan-06 Moonfish Bank (Lost Anchor) 17u 33.895N 63u 17.965W 25-28 11 10-Jan-06 Moonfish Bank 17u 33.900N 63u 18.221W 19 12 12-Jan-06 Poison Bank 17u 30.758N 63u 13.692W 29 13 12-Jan-06 Brown Town 17u 28.027N 63u 14.944W 20 14 13-Jan-06 Red Flats 17u 26.359N 63u 27.769W 28 15 13-Jan-06 Field of Greens 17u 30.620N 63u 27.707W 30 16 14-Jan-06 Coral Garden 17u 20.756N 63u 15.036W 23 30 17 14-Jan-06 Conch Valley 17u 21.184N 63u 15.121W 17 22 doi:10.1371/journal.pone.0010677.t002 PLoS ONE www.plosone.org 4 May 2010 Volume 5 Issue 5 e10677

Figure 3. Selected species from Field of Greens. A region (. one hectare) of Saba Bank (depth 25 m) that our group named Field of Greens because the vast sand plain was dominated by green algae (Chlorophyta). Top left: Udotea occidentalis. Top right: Caulerpa mexicana. Middle left: Halimeda cf. tuna forma platydisca. Middle right: Caulerpa prolifera. Bottom left: Penicillus dumentosus. Bottom middle: Caulerpa cupressoides. Bottom right: Caulerpa racemosa f. lamourouxii. doi:10.1371/journal.pone.0010677.g003 PLoS ONE www.plosone.org 5 May 2010 Volume 5 Issue 5 e10677

Figure 4. Selected species from Brown Town. The large region (. one hectare) of Saba Bank (depth 25 m) nicknamed Brown Town because of the domination by brown macroalgae (Phaeophyceae). Top left: Overview of Brown Town habitat with over 50% cover of Dictyota turf. Top right: Dictyota hamifera. Middle left: Stypopodium zonale. Middle right: mixture of Lobophora variegata and Dictyota humifusa. Bottom right: Dictyopteris justii. Bottom right: Sargassum hystrix. doi:10.1371/journal.pone.0010677.g004 PLoS ONE www.plosone.org 6 May 2010 Volume 5 Issue 5 e10677

Algal Diversity: Saba Bank Figure 5. Selected specimens from Seaweed City. Specimens dominating the stony pavement area (30 m deep) termed Seaweed City, dominated by red algae (Rhodophyta). Top left: Wrightiella blodgettii. Top right: Hypoglossum hypoglossoides. Middle right: Gracilaria cylindrica. Bottom left: Jania capillacea. Bottom right: Tricleocarpa fragilis. doi:10.1371/journal.pone.0010677.g005 author, collector, collector number and precise location as a satellite map and longitude/latitude. Searching for a given parameter generates information associated with the specimens collected by the project under that parameter. Images taken of in situ living plants from the field are attached at the bottom of the label data. PLoS ONE www.plosone.org Discussion Prior to this survey, the two most diverse areas for algae reported in the Caribbean had been Diamond Rock, Martinique [10] and Pelican Cays, Belize [12], a mangrove, seagrass, and coral complex. Habitats on Saba Bank have far exceeded both of 7 May 2010 Volume 5 Issue 5 e10677

Figure 6. Selected specimens from Seaweed City. More Rhodophyta species characteristic of Seaweed City (Figure 5). Top left: Porolithon pachydermum. Top right: Scinaia halliae. Middle left: Dasya antillarum. Middle right: Meristiella schramii. Bottom left: Laurencia intricate. Bottom right: Chrysymenia dickieana. doi:10.1371/journal.pone.0010677.g006 these places for species diversity per unit collection effort. A major reason for this uniqueness and richness is the sheer size and habitat range of the seamount/atoll. The rim habitats range from windward pristine coral reefs to extensive leeward rhodolith (coralline algal spheres) beds (N 17u25.8329, W 63u40. 9629) containing a high diversity of small epiphytic algal taxa. The Relative Dominance Model [9] is useful for characterizing the health of any given coral reef. According to this model, healthy coral reefs are dominated by reef-building (hermatypic) corals, crustose coralline algae, and high populations PLoS ONE www.plosone.org 8 May 2010 Volume 5 Issue 5 e10677

Figure 7. Selected specimens from potential new species. Some examples of potential new species of brown algae (Phaeophyceae) from Saba Bank (35 45 m deep). Top four: Sargassum spp. Bottom right and left: Dictyota spp. doi:10.1371/journal.pone.0010677.g007 of herbivorous fishes all characteristic of Saba Bank s windward eastern rim and fore-reef slope (Figure 8). Vast sedimentary environments with some interspersed bedrock create relatively unstructured interior plains behind the rim communities, where seagrass beds would normally abound. However, seagrasses are absent (presumably due to excessive depths and insufficient light). Here vast plains of various groups of large and robust algal forms provide the three-dimensional structural heteroge- PLoS ONE www.plosone.org 9 May 2010 Volume 5 Issue 5 e10677

Algal Diversity: Saba Bank Figure 8. Windward fore-reef slope. Coral-dominated community characteristic of the windward (east) fore-reef slope of Saba Bank. doi:10.1371/journal.pone.0010677.g008 neity. These are many of the rhizophytic (i.e., rooted) Bryopsidales forms typical of healthy seagrass beds in the sedimentary habitats. The seagrass model [13] indicates that these sand plains of robust large epiphyte-free green algae, as in Field of Greens (Figure 3), indicate pristine oligotrophic conditions. The same can be said in the cases of Brown Town (Figure 4) and Seaweed City (Figures 5 and 6), where especially clean robust macroalgal forms predominate on hard bottom. Few filamentous and thin sheet forms indicative of stressed or physically disturbed environments were observed. expedition and the three dive sites with highest algal diversity is available online: http://www.littlersworks.net/. Collections for pressing were taken by hand and preserved in the field and processed upon returning to the Smithsonian Institution. Nearly all specimens were photographed in situ and the same plants were placed in individual numbered plastic bags at the time of collection. These were transferred to polycarbonate scintillation vials, fixed in 5% formalin, finally preserved in 70% ethanol, and later examined microscopically. Additionally, identical specimens for molecular analyses were dried in frozen silica gel, placed in hermetically sealed vials, and stored in a freezer. All macroalgal/seaweed specimens were deposited in the Algal Collection of the US National Herbarium, Smithsonian Institution. All Saba Bank projects have collecting permits through CITES (where necessary) and the Saba Conservation Foundation (where CITES is not required). Materials and Methods During 2-16 January 2006, we accompanied a multi-disciplinary team of sixteen other scientists and managers of marine protected areas to conduct a detailed biological assessment and sampling program of Saba Bank. The survey focused on the comprehensive survey of fishes, mollusks, crustaceans, macroalgae, and sponges. The team was supported by three vessels, two marine park patrol boats and a fishing vessel that operated together. Dives were made primarily in representative areas of interest at depths from 12 to 50 m and included both biological sampling and photographic documentation. A photographic overview of this Author Contributions Conceived and designed the experiments: MML DSL BLB. Performed the experiments: MML DSL BLB. Analyzed the data: BLB. Contributed reagents/materials/analysis tools: BLB. Wrote the paper: MML DSL. References 2. Spencer JW (1904) The windward islands of the West Indies. Transactions of the Canadian Institute 7: 351 370. Available: http://books.google.com/books? id=om0vaaaayaaj via the Internet. Accessed 28 Apr 2009. 3. Vaughan TW (1919) Fossil corals from Central America, Cuba, and Puerto Rico, with an account of the American Tertiary, Pleistocene, and recent coral reefs. 1. Meesters EH, Nijkamp H, Bijvoet L (1996) Towards sustainable management of the Saba Bank. A report for the Department of Public Health and Environment (VOMIL) Curac ao, Netherlands Antilles. KNAP Project 96-03: 42. Available: http://www.mina.vomil.an/pubs/meestersknap96-03-sababank.pdf via the Internet. Accessed 28 Apr 2009. PLoS ONE www.plosone.org 10 May 2010 Volume 5 Issue 5 e10677

Smithsonian Institution, United States National Museum, Bulletin 103: 189-524+I- XIV. Available: http://books.google.com/books?id=_tgaaaaayaaj via the Internet. Accessed 28 Apr 2009. 4. Davis WM (1926) The Lesser Antilles. American Geographic Society, Map of Hispanic America, Publication 2: 212. 5. Van der Land J (1977) The Saba Bank, a large atoll in the northeastern Caribbean FAO Fisheries Reports 200: 469 481. Available: http://www.nacri. org/greylit/vanderlandj_sababankatoll1977.pdf via the Internet. Accessed 28 Apr 2009. 6. MacIntyre IG, Kinsman DJJ, German RC (1975) Geological reconnaissance survey of Saba Bank, Caribbean Sea. Caribbean Journal of Science 15: 11 20. Available: http://academic.uprm.edu/publications/cjs/vol15a/p011-020. PDF via the Internet. Accessed 28 Apr 2009. 7. Klomp KD, Kooistra DJ (2003) A post-hurricane, rapid assessment of reefs in the Windward Netherlands Antilles (stony corals, algae, and fishes). Atoll Research Bulletin 496: 404 437. Available: http://hdl.handle.net/10088/4800 via the Internet. Accessed 28 Apr 2009. 8. Colwell RK (2006) EstimateS: Statistical estimation of species richness and shared species from samples. Version 8.0, November 12, 2006. User s Guide and application. Available: http://purl.oclc.org/estimates via the Internet. Accessed 28 Apr 2009. 9. Littler MM, Littler DS (2007) Assessment of coral reefs using herbivory/nutrient assays and indicator groups of benthic primary producers: a critical synthesis, proposed protocols, and critique of management strategies. Aquatic Conservation: Marine and Freshwater Ecosystems 17: 195 215. Available: http://hdl. handle.net/10088/2619 via the Internet. Accessed 28 Apr 2009. 10. Littler MM, Littler DS, Lapointe BE (1993) Modification of tropical reef community structure due to cultural eutrophication: the southwest coast of Martinique. Proceedings of the 7th International Coral Reefs Symposium, Guam, 1992 1: 335 343. Available: http://hdl.handle.net/10088/2570 via the Internet. Accessed 28 Apr 2009. 11. Littler DS, Littler MM, Brooks BL (2007) Marine Algae of Saba Bank. In: Mori SA, Buck WR, Gracie C, eds. Plants and Lichens of Saba, Virtual Herbarium. Available: http://sweetgum.nybg.org/saba/algae.html via the Internet. Accessed 28 Apr 2009. 12. Littler MM, Littler DS (1997) An illustrated marine flora of the Pelican Cays, Belize. Bulletin of the Biological Society of Washington 9: 149. 13. Littler MM, Littler DS (2005) Application of a seagrass management model. In: Krupnick GA, Kress WJ, eds. Plant conservation: a natural history approach. Chicago & London: University of Chicago Press. pp. 270-285. Available: http:// hdl.handle.net/10088/2611 via the Internet. Accessed 28 Apr 2009. PLoS ONE www.plosone.org 11 May 2010 Volume 5 Issue 5 e10677