Predicting patterns of coral spawning at multiple scales: the closer you look the harder it gets

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Predicting patterns of coral spawning at multiple scales: the closer you look the harder it gets Dr Andrew H Baird Senior Research Associate ARC Centre of Excellence for Coral Reef Studies andrew.baird@jcu.edu.au 40

Abstract Understanding the reproductive biology of organism is of fundamental interest to scientist and resource managers. Early theoretical studies predicted that the reproductive season of widespread organisms should be more extended near the equator than at high latitudes because conditions favourable for gametogenesis persist year round. Similarly, it was believed that synchrony among both populations and species would be lower because there are fewer good cues in the tropics where annual fluctuations in environmental variables are reduced. Subsequent work from numerous locations within the Indo- Pacific indicates that multi-specific synchronous spawning is a characteristic feature of all Acropora assemblages. At large spatial scales spawning periods are highly predictable. In the central Indo- Pacific, for example, the majority of reproductive output is concentrated in brief spawning periods following full moons at the beginning and end of the monsoon. The spawning peak in Western Australia, Manado, Singapore, northern New Guinea, southern Japan and Aceh is in Mar/Apr, whereas in Bali, Padang, Makassar, the Solomon Islands, New Caledonia and on the GBR the peak is in Oct/Nov. While the comparative intensity of these peaks varies between locations, it appears to be consistent among years. Above approximately 28-30 degrees latitude, and possibly at some sites in the cental Pacific, such as Guam, this pattern breaks down and the spawning peak is progressively one month later in the season for every 2-400 km further from the equator. At smaller spatial scales the patterns are far less regular. For example, in the central GBR peak spawning on inshore reefs occurs one month before offshore reefs, however, Acropora spawning occurs following every full moon between Oct and Feb at most reefs. Some species spawn predominantly early in the season, such as the classic mass spawners A. millepora and A. hyacinthus, some spawn throughout the season, eg A. humilis, and some species spawn predominantly later in the season eg A. verweyi. Peak spawning within populations of a single species can vary dramatically over very small scales. For example, consider 4 mid-shelf reefs in the Central GBR separated by less than 20 km: on 2 reefs fecund colonies of A. monticulosa were observed only in Dec, at a 3 rd reef, fecund colonies were only observed in Nov, while at the 4 th reef, fecund coral were observed in both Nov & Dec. In conclusion, while large scale patterns in coral spawning may be relatively predictable, detailed studies at the local scale will rarely be avoidable. 41

Questions to address How synchronised is coral spawning? One month or several? Is there geographic variation in the timing of spawning? Are there consistent inshore-offshore differences? Are there species which spawn more than once? Are there species which are not synchronous? What proportion of the population might typically spawn in a single event? 42

spawn slick Coral life history fertilisation embryogenesis spawning 2. motile larvae Settlement and metamorphosis 1. Sessile adult gametogenesis juvenile 43

Mature eggs in an Acropora colony Photo: James Guest Photograph reproduced with kind permission of Springer Science and Business Media. Guest JR, Chou LM, Baird AH, Goh BPL (2002) Multispecific, synchronous coral spawning in Singapore. Coral Reefs 21: 422-423 44

Acropora colony setting just prior to spawning Photo: James Guest Photograph reproduced with kind permission of Springer Science and Business Media. Guest JR, Chou LM, Baird AH, Goh BPL (2002) Multispecific, synchronous coral spawning in Singapore. Coral Reefs 21: 422-423 45

Close up of an egg-sperm bundle Photo: Masanori Nonaka Photograph reproduced with kind permission of Springer Science and Business Media. Nonaka M, Yamamoto HH, Baird AH, Kamiki T (2003) Reseeding the reefs of Okinawa with the larvae of captive-bred corals. Coral Reefs 22: 34-34 46

Bundle release: Platygyra sp. Photo: James Guest 47

Coral spawn slick 48

Embryogenesis 12 to 36 hours depending on the species Photo: Andrew Heyward 49

Coral planula larva 50

Coral recruit: 2 months old 51

Coral sexuality Hermaphrodites Individual colonies produce both eggs and sperm Gonochores Individual colonies either male or female 52

Coral reproductive mode Brooders Spawners Internal fertilisation Larvae are competent to settle on release Colonies breed more than once per year External fertilisation Larvae not competent to settle on release Colonies breed once per year 53

Patterns in coral reproductive biology Reproductive mode Sexuality Brooding Spawning Sum Gonochorism 19 (5.8) 80 (24.3) 99 (30.1) Hermaphroditism 23 (7.0) 207 (62.9) 230 (69.9) Sum 42 (12.8) 287 (87.2) 349 Kerr & Baird unpublished data 54

Coral reproductive biology: a brief history Prior to 1984 most corals were believed to be brooders, reproductively active year all year resulting in: a uniform pool of larvae; and settlement through out the year 55

Coral spawning on the Great Barrier Reef: in the central GBR over 130 species spawn in the week following a full moon in late spring (Harrison et al. 1984) > 30 species spawn within hours on the same night at a single location (Willis et al. 1985; Babcock et al. 1986) 56

The mass spawning period: GBR Orpheus Island, GBR November 1984 Willis et al. 1985 Number of species 25 20 15 10 5 0 Pectinia Agaricidae Favia Acropora Montipora 1 2 3 4 5 6 7 8 9 10 Days after full moon 57

Coral spawning: global patterns 1990 s view Synchronous spawning [occurs] on the Great Barrier Reef, while asynchrony among and within species has been observed in the Red Sea, Caribbean, Central Pacific, Hawaii, and southern Japan (Richmond & Hunter 1990) 58

Geographic variation in spawning synchrony: global patterns 28 of 41 Acropora species sampled had mature colonies A multi-specific spawning event close to the equator in contradiction to the dogma Baird, A.H., & Sadler, C. (2001) Synchronous spawning of Acropora in the Solomon Islands. Coral Reefs. 19: 286. 59

Spawning synchrony: study sites 60

Why the Acropora? Abundant on most reefs Ecologically significant Easy to sample Generally a good indicator of spawning behaviour of other hermaphroditic species 61

Gametogenesis: the typical Acropora on the GBR egg diameter (mm) 0.6 0.5 0.4 0.3 0.2 0.1 spawn invisible white pigmented 0 Mar Apr May Jun Jul Aug Sept Oct Nov 62

Reproductive condition of Acropora colonies 1. mature pigmented eggs; spawning following next full moon 2. immature white eggs; spawning in 2-3 months Photo: James Guest Broken branch of A. intermedia 3. empty - eggs too small to see or absent; recently spawned, or spawning unlikely to spawn in the near future. 63

Spawning synchrony: Central Indo-Pacific 64

The proportion of Acropora colonies breeding In the central Indo-Pacific, for example, the majority of reproductive output is concentrated in brief spawning periods following full moons at the beginning and end of the monsoon. The spawning peak in Manado, Singapore, northern New Guinea, southern Japan and Aceh is in Mar/Apr, whereas in Bali, Padang, Makassar, the Solomon Islands, New Caledonia and on the GBR the peak is in Oct/Nov. While the comparative intensity of these peaks varies between locations, the timing appears to be consistent among years. 65

Spawning synchrony: Acropora in Singapore 80 Proportion of colonies mature (%) 60 40 20 0 Mar '02 (n=113) Apr (n=74) May (n=79) Jul (n=72) Sep (n=83) Oct (n=97) Nov (n=78) Dec (n=76) Jan '03 (n=81) Feb (n=101) Mar (n=100) Apr (n=98) May (n=79) Guest JR, Baird AH, Goh BPL & Chou LM (2004) Coral Reefs in press 66

Geographic variation in the time of spawning: central Indo-Pacific In the central Indo-Pacific the majority of spawning is concentrated in brief periods following full moons at the beginning and end of the monsoon 67

Spawning synchrony: High latitude reefs 68

Geographic variation in the timing of spawning: other studies Guest et al., (2005) 69

Geographic variation in the timing of spawning: high latitude reefs Above approximately 28-30 degrees latitude, the spawning peak is progressively one month later in the season for every 2-400 km from the equator 70

Spawning synchrony: cross shelf patterns GBR 71

Spawning synchrony in Acropora assemblages: Cross shelf patterns in the central GBR At smaller spatial scales the patterns are far less regular. For example, in the Central GBR peak spawning on inshore reefs occurs one month before offshore reefs. However, Acropora spawning occurs following every full moon between October and February at most reefs. 72

Inshore-offshore differences Peak spawning is typically one month earlier on inshore reefs at least on the GBR; almost certainly driven by temperature Similar pattern in the Gulf of Thailand, with inshore northern reefs spawning a month earlier than open ocean reefs in the south 73

Spawning synchrony: species which spawn more than once per year Some species spawn predominantly early in the season, such as the classic mass spawners, A. millepora and A. hyacinthus. Some spawn throughout the season eg. A. humilis. Some species spawn predominantly later in the season eg. A. verweyi. 74

Spawning synchrony: reef scale spatial variation in Acropora valida Peak spawning within populations of a single species can vary dramatically over very small scales. For example, consider 4 mid-shelf reefs in the Central GBR separated by less than 20 km: On 2 reefs fecund colonies of A. monticulosa were observed only in December, at a 3rd reef, fecund colonies were only observed in November, while at the 4th reef, fecund coral were observed in both November and December. 75

Are there species which spawn more than once per year? Most colonies of most spawning species have only one gametogenic cycle per year i.e. each colony spawns only once Very high synchrony within populations is the exception rather than the rule. Spawning is typically split over 2-3 months in most species at most locations 76

Are there species which are not synchronous? Brooders are less synchronous than spawners, particularly on low latitude reefs A small number of spawning species release gametes outside the main mass spawning periods eg A. veryweyi; A. longicyathus 77

What proportion of the population might typically spawn in a single event? Generally between 20-80 % Very rarely 100 % 78

How synchronised is coral spawning? Multi-specific synchronous spawning is a feature of all specious coral assemblages Discrete mass spawning periods, similar to that on the GBR, concentrated at changes of season within 28 degrees of the equator Highly predictable at large scale; less so a smaller scales eg. reefs with region 79

How synchronised is coral spawning? Caveats Always exceptions eg Gulf of Thailand the northern reefs spawn in February; Guam in May/June Some sites remain a mystery despite intensive sampling eg. Sth PNG Exact day of spawning often varies between years How will spawning synchrony be affected by climate change Detailed studies at local scale are necessary 80

How synchronised is coral spawning? Knowledge gaps Environmental cues for coral spawning remain unknown: temperature, solar irradiance or other cues? Data on reproductive biology is available for less than 50 % of scleractinian species In particular, gonochoric species poorly known 81

Question time Question Simpson- A previous explanation of why corals spawn in Spring on the East Australian Coast and Autumn on the Western Australian coast proposed that this was a genetic polymorphism with larvae distributed either way by prevailing currents. Responses Baird there may be a genetic basis to the Spring-Autumn split in some species but we are not sure. Kabay- What is the significance of the full moon in predicting spawning? Baird- Corals can detect moonlight and may focus in on the moon phase or it may be other factors associated with moon phase Simpson- the tide is critically associated with the moon and the 7d post full moon periodicity may be aligning with neap tides. Ward- How local is the scale of variation in the percentages of coral populations that are reproductively synchronised? Could this patchiness be used for management? Baird Differences in fecundity are associated spatially within reefs or between reef patches. Some patches of Acropora individuals may be almost all gravid while others a few km away may be all non-gravid. It is not clear what environmental differences cause this patchiness. Simpson- This may relate to specific individuals we have seen corals which will spawn at the same time year after year. Metaxis Is some of the apparent variation in the timing of spawning within a species due to taxonomic confusion? Stoddart You show sites which have a major and a minor spawning peak in Spring or Autumn. Are the site-specific differences constant between years? Forde Acropora species are fast growing. Might your variation in fecundity be related to immature individuals? Baird With some groups the differences have been identified as relating to cryptic species but others seem to vary within a single readily identified species. Baird We only have multi-year data for a few sites, but the ratio is constant over those years at those sites. Baird Unlikely as we target individuals which are generally of a reproductive size. 82